Phoenix Islands Protected Area 2009 ... - Science-to-Action
Phoenix Islands Protected Area 2009 ... - Science-to-Action
Phoenix Islands Protected Area 2009 ... - Science-to-Action
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<strong>Phoenix</strong> <strong>Islands</strong> <strong>Protected</strong> <strong>Area</strong> Assessment <strong>2009</strong><br />
Preliminary Expedition Report<br />
Page 1 of 35<br />
Oc<strong>to</strong>ber 1, <strong>2009</strong><br />
Republic of Kiribati
<strong>Phoenix</strong> <strong>Islands</strong> <strong>Protected</strong> <strong>Area</strong> Expedition <strong>2009</strong> – Assessment Report<br />
Senior Edi<strong>to</strong>rs: Gregory S<strong>to</strong>ne, Expedition Leader, David Obura, Chief Scientist for Coral Reef<br />
Assessment and Randi Rotjan.<br />
Contributing Authors: Rob Barrel, Craig Cook, Alan Dynner, Les Kaufman, Kate Madin, Larry<br />
Madin, Stuart Sandin, Brian Skerry, Tuake Teema, Tukabu Terooko, and Jeff Wildermuth.<br />
Page 2 of 35
Table of Contents<br />
Summary Results...................................................................................................................................................4<br />
Introduction and Acknowledgments..............................................................................................................6<br />
Expedition members and affiliation details ................................................................................................6<br />
Expedition Details .................................................................................................................................................7<br />
Objective 1a: Blue water zooplank<strong>to</strong>n assessment........................................................................................................8<br />
Objective 1b: Deep Water ROV assessments...................................................................................................................11<br />
Objective 1c: Coral reef assessments i. Corals and benthic structure.................................................................12<br />
Objective 1c: Coral reef assessments ii. Corallivory (fishcoral trophic interactions)................................20<br />
Objective 1c: Coral reef assessments iii. Fish diversity, abundance, and biomass assessments .............23<br />
Objective 1d: Onshore (landbased) Assessment ........................................................................................................25<br />
Objective 1e: Kiribati Fisheries Assessments..................................................................................................................27<br />
Objective 1f: Collaborative efforts.......................................................................................................................................29<br />
Objective 2: Medical objectives.............................................................................................................................................31<br />
Objective 3: Media objectives ................................................................................................................................................32<br />
Appendix I, Memo on PIPA Tourism Potential......................................................................................... 33<br />
Appendix II, PIPA Research Permit .......................................................................................................35<br />
Page 3 of 35
Summary Results<br />
This is the fourth scientific expedition mounted by the New England Aquarium <strong>to</strong> the <strong>Phoenix</strong> <strong>Islands</strong>, Republic of<br />
Kiribati in the South Pacific, and the first since the <strong>Phoenix</strong> <strong>Islands</strong> <strong>Protected</strong> <strong>Area</strong> was formally gazetted in 2006,<br />
and extended in 2008 <strong>to</strong> become the largest MPA in the world, with a surface area of 408,250 km 2 . The expedition<br />
team of 14 people spent 11 days in PIPA from September 13‐23, completing over 400 SCUBA dives. Six islands<br />
were visited; in order: Nikamororo (2 days), McKean (1 day), Kan<strong>to</strong>n (3 days), Enderbury (1 day), Rawaki (1 day),<br />
and Orona (2 days). Initial expectations for the trip were <strong>to</strong> conduct research on deep sea and seamount<br />
ecosystems, two of the most extensive and valuable of PIPA’s assets, but the lack of suitable vessels made this<br />
impossible. Nevertheless, preliminary work on pelagic invertebrates and with a deep water ROV was conducted,<br />
while the main efforts focused on coral reef assessments, initiating a broader range of research projects on coral<br />
reef biota and terrestrial assessments with a management focus. Video footage was collected for further<br />
development of educational and promotional videos on PIPA, and a National Geographic Magazine pho<strong>to</strong>grapher<br />
collected material for a future article on PIPA in the magazine. Timing of the expedition coincides with PIPA’s<br />
application for listing as a World Heritage Site, and the research expedition had as an additional goal <strong>to</strong> inform this<br />
process and support the application.<br />
The pelagic invertebrate collections and deep water ROV confirmed that PIPA waters are typical of oligotrophic<br />
ocean conditions, with low biomass in the water column, many cosmopolitan species of gelatinous plank<strong>to</strong>n that<br />
probably fit in<strong>to</strong> the food web here much as they do in other locales, and very clear waters. Future plank<strong>to</strong>n<br />
studies at PIPA should expand the collections started here, and include quantitative, stratified sampling both<br />
upstream and downstream of the islands, and in the lagoons on different tidal cycles <strong>to</strong> estimate the input of<br />
zooplank<strong>to</strong>n <strong>to</strong> the fringing reefs and lagoon communities.<br />
The coral reef assessments found a rapid recovery in coral cover, returning 50% of the cover lost in the 2002‐3<br />
bleaching event and an overall cover of 26%. Coralline algae, which is critical in promoting regrowth of corals and<br />
strengthening the reef framework increased from 2002 <strong>to</strong> 2005 <strong>to</strong> <strong>2009</strong>. Algal turf, which competes with corals<br />
decreased from 2005 <strong>to</strong> <strong>2009</strong>, after an increase due <strong>to</strong> the coral mortality in 2002; intact fish herbivore<br />
populations were likely instrumental in preventing algal domination and facilitating regrowth of coralline algae and<br />
corals. Taken <strong>to</strong>gether, these 3 indica<strong>to</strong>rs are a strong indication of very robust and healthy reef recovery which<br />
will continue in coming years. The best reefs were on the leeward sides of Enderbury and Rawaki islands, and had<br />
recovered all the cover lost, returning <strong>to</strong> about 80% cover of corals. Nevertheless, many species were not yet<br />
present as large colonies and more time will be needed for re‐colonization of some lost species and res<strong>to</strong>ration of<br />
the large sizes found before the bleaching event. In contrast with this best‐case scenario for reef recovery from<br />
mass mortality, which occurred in ideal conditions on the leeward reefs of small islands (less heating of water by<br />
the island, no lagoon effect that retards coral recovery, minimal breakage by waves), were clear examples of how<br />
local fac<strong>to</strong>rs can slow reef recovery. The discreteness and isolation of the islands helped distinguish these different<br />
fac<strong>to</strong>rs, which is often not possible on larger island/continental systems where many threats act <strong>to</strong>gether and<br />
mask each others’ signal.<br />
• Heavy wave energy on windward slopes causes repeated coral breakage, which slows recovery (windward<br />
sides of most islands);<br />
• Lagoon waters are hotter and more rich in nutrients and sediment than open reef waters, and this favours<br />
fleshy and turf algal growth over corals, making it harder for new corals <strong>to</strong> settle and survive (leeward<br />
sides of Kan<strong>to</strong>n and Nikumaroro affected by lagoon waters, especially north of the channels);<br />
• The presence of a shipwreck causes iron enrichment of waters locally. At very high levels, this causes the<br />
reef <strong>to</strong> degrade. At lower levels of iron, that adult corals may be able <strong>to</strong> <strong>to</strong>lerate, the settlement and<br />
survival of small corals is compromised, and recovery from major coral mortality is retarded (major<br />
shipwrecks especially on leeward reefs have an effect, on Nikumaroro, Kan<strong>to</strong>n and Orona). Similarly,<br />
guano and excess nutrient enrichment may have the same effect (McKean).<br />
Page 4 of 35
• Low connectivity and high mortality can combine such that with very low larval flow between islands and<br />
very low surviving adult coral populations that may fail <strong>to</strong> reproduce successfully, recruitment failure<br />
results in very slow recovery (McKean windward side).<br />
The fish assemblage of the <strong>Phoenix</strong> <strong>Islands</strong> had high abundance and biomass (5.55 fish m ‐2 and 259.6 g m ‐2 ,<br />
respectively). This is similar <strong>to</strong> that of the Northwestern Hawaiian <strong>Islands</strong> (Papahanaumokuakea National Marine<br />
Monument with 243 g m ‐2 on average) and Palmyra a<strong>to</strong>ll in the Line <strong>Islands</strong> (270 g m ‐2 ). The biomass of fish was<br />
dominated by large‐bodied and massive preda<strong>to</strong>ry species including snappers, groupers, and, on some islands,<br />
sharks. However shark populations have clearly suffered from fishing in the past, which has been documented <strong>to</strong><br />
have occurred in 2001, 2005, 2006 and 2007, illustrating the urgent need <strong>to</strong> enforce fishing restrictions. Large<br />
numbers of small sharks were noted at some locations, suggesting recovery may be underway. The persistence of<br />
high fish biomass following the 2002 mass‐bleaching event, particularly within guilds that feed upon algae and<br />
benthic invertebrates, has very likely been a key fac<strong>to</strong>r in the impressive regeneration of hard coral communities<br />
on PIPA reefs. Observations of fishery resources confirm their robustness in the absence of exploitation, including<br />
species targeted in the aquarium trade, live reef food fish trade and food fish resources, making PIPA a valuable<br />
reference site for understanding the impact of these fisheries elsewhere.<br />
Additional studies on coral reef dynamics were conducted <strong>to</strong> build a broader science base emanating from PIPA.<br />
With an intact fish fauna, observations of coral‐fish interactions, in particular corallivory, found very high rates of<br />
predation on corals as well as high selectivity of which coral genera are targeted. This contrasts with results from<br />
other locations where fishing impacts on the fish fauna result in much lower abundances and therefore also of<br />
predation on corals. No damaging invertebrate corallivores were found, and only one clear case of an unknown<br />
coral disease was noted. Integration of results from PIPA surveys will be done with a number of programmes,<br />
including the IUCN Climate Change and Coral Reefs reef resilience assessment programme, and various<br />
components of the Marine Management <strong>Area</strong> <strong>Science</strong> programme of Conservation International (particularly the<br />
Community Health Index that works on reef resilience, the Coral Whisperer programme on gene expression in<br />
stressed corals, and initial surveys of using coral fluorescence as a field indica<strong>to</strong>r).<br />
Coral and invertebrate samples were made on behalf of 8 colleagues working in population genetics, coral<br />
physiology and systematics, <strong>to</strong>talling 500 samples from a variety of coral genera and a small number of other taxa<br />
(soft corals, corallimorphs, holothurians, vermetid worms and serpulid worms). These samples will be delivered <strong>to</strong><br />
the respective researchers, and their findings documented separately.<br />
Land surveys were conducted on all islands, with the following observations made:<br />
• Nikumaroro: only one coconut crab was seen, and rocks were found suggesting an old Polynesian marae.<br />
• McKean: no evidence of rats or other rodents was seen and bait stations were observed everywhere,<br />
suggesting successful eradication.<br />
• Kan<strong>to</strong>n: The air strip was inspected and appears <strong>to</strong> be in excellent condition, without signs of degradation. A<br />
survey was conducted around the old hotel and Pan Am airbase, and Rob Barrel of the Nai’a prepared a memo<br />
detailing a vision for using the site as a PIPA <strong>to</strong>urism base.<br />
• Enderbury: The island was overrun with rats and bird populations appeared low.<br />
• <strong>Phoenix</strong> (Rawaki): There was no evidence of rats or rabbits on this island. Bird populations appeared robust.<br />
• Orona: one small island in the northern area was surveyed, and appeared in good condition. Observed<br />
abundant giant clams and seabirds<br />
The findings of the expedition will contribute important information <strong>to</strong> management of PIPA, as well as<br />
fundamental contributions <strong>to</strong> science. Rapid reporting of the coral bleaching and fish herbivore results will be<br />
prioritized, as these are extremely relevant <strong>to</strong> understanding the vulnerability of coral reefs <strong>to</strong> combined climate<br />
change and local threats. The findings confirm the importance of PIPA as a potential reference or observa<strong>to</strong>ry<br />
site, which will also be true for the other principal ecosystems – the deep sea, seamounts, pelagic and<br />
terrestrial. We therefore recommend strengthening all efforts <strong>to</strong> operationalize PIPA, including raising funds <strong>to</strong><br />
Page 5 of 35
capitalize the endowment and successful completion of the World Heritage application. The expedition also<br />
found increased benefits from broadening the science and research interests in PIPA, and encourage further<br />
development of a more comprehensive research agenda and building capacity, particularly on Kan<strong>to</strong>n, <strong>to</strong><br />
support this.<br />
Introduction and Acknowledgments<br />
This is a preliminary report on a scientific expedition <strong>to</strong> the <strong>Phoenix</strong> <strong>Islands</strong>, Republic of Kiribati in the South<br />
Pacific. The <strong>Phoenix</strong> <strong>Islands</strong> <strong>Protected</strong> <strong>Area</strong> was formally gazetted in 2006, and extended in 2008 <strong>to</strong> become the<br />
largest Marine <strong>Protected</strong> <strong>Area</strong> (MPA) in the world, with a surface area of 408,000 km2.<br />
We thank the government of Kiribati for the permission <strong>to</strong> conduct this survey and <strong>to</strong> the sponsors including the<br />
Oak foundation, The Akiko Shiraki Dynner Fund for Exploration and Conservation at the New England Aquarium,<br />
the Marine Management <strong>Area</strong> <strong>Science</strong> Program at Conservation International, Mr. James Stringer, Wendy<br />
Benchley, and Dr. Craig Cook. Thanks <strong>to</strong> Randi Rotjan for assembling the bits and pieces of this report while being<br />
<strong>to</strong>ssed up, down and sideways during the five day boat crossing back <strong>to</strong> Fiji from the <strong>Phoenix</strong> <strong>Islands</strong>. We also<br />
thank Elyse Antrim, Edward Lohnes, Lydia Bergen and Heather Tausig for essential help with planning and<br />
execution of this expedition, even though they were not with us on the cruise.<br />
Expedition members and affiliation details (alphabetical order)<br />
Rob Barrel: NAI’A<br />
Craig Cook: Undersea Medical Consultants<br />
Alan Dynner: New England Aquarium<br />
Les Kaufman: Bos<strong>to</strong>n University, Conservation International, New England Aquarium<br />
Kate Madin: Woods Hole Oceanographic Institution<br />
Larry Madin: Woods Hole Oceanographic Institution<br />
David Obura: CORDIO and New England Aquarium<br />
Randi Rotjan: New England Aquarium and Harvard University<br />
Stuart Sandin: Center for Marine Biodiversity and Conservation, Scripps Institution of Oceanography<br />
Brian Skerry: National Geographic and New England Aquarium<br />
Gregory S<strong>to</strong>ne: Conservation International and New England Aquarium<br />
Jim Stringer: Retired; Pho<strong>to</strong>grapher<br />
Tuake Teema: Ministry of Fisheries & Mineral Resources Development Kiribati<br />
Tukabu Teroroko: Direc<strong>to</strong>r of the <strong>Phoenix</strong> <strong>Islands</strong> <strong>Protected</strong> <strong>Area</strong><br />
Jeff Wildermuth: National Geographic<br />
Page 6 of 35
Expedition Details<br />
For this trip, the expedition team chartered the Nai’a, based out of Fiji. The Nai’a is 120 feet long, by 30 feet in<br />
beam, by 11 feet draft; 240 <strong>to</strong>ns. She is a Dutch‐built mo<strong>to</strong>r sailor, built in Amsterdam in 1979 and re‐built by Rob<br />
Barrel in Fiji in 1992. The expedition team of 14 people spent 11 days on‐site from September 13‐23, completing<br />
over 400 SCUBA dives. Six islands were visited; in order: Nikumororo (2 days), McKean (1 day), Kan<strong>to</strong>n (3 days),<br />
Enderbury (1 day), Rawaki (1 day), and Orona (2 days), with transit time between. Transit time <strong>to</strong> and from PIPA<br />
was approximately 5.5 days each way. This was the first expedition <strong>to</strong> the <strong>Phoenix</strong> <strong>Islands</strong> following the<br />
designation as PIPA: the world’s largest marine reserve. There were several trip objectives, and this report is<br />
organized around them as follows:<br />
1) Scientific objectives<br />
a) Blue water zooplank<strong>to</strong>n assessment<br />
b) Deep Water ROV assessments<br />
c) Coral reef assessments<br />
i. Corals and benthic structure<br />
ii. Corallivory (fish‐coral trophic interactions)<br />
iii. Fish diversity, abundance, and biomass assessments<br />
d) On‐shore (land‐based) Assessment<br />
e) Kiribati Fisheries Assessments<br />
f) Collaborative efforts<br />
2) Medical objectives<br />
3) Media objectives<br />
Page 7 of 35
Objective 1a: Blue water zooplank<strong>to</strong>n assessment<br />
Larry and Kate Madin<br />
Introduction<br />
PIPA is the world’s largest marine protected area, established largely <strong>to</strong> protect the nearly undisturbed<br />
environments of its islands, a<strong>to</strong>lls, submerged banks and seamounts. Of its 408,250 square kilometers of area, only<br />
25 square kilometers are land area – 0.006% of the protected area. All else is open ocean over deep‐sea floor. The<br />
water column of PIPA is the largest habitat by far within the region, and its importance as home <strong>to</strong> large fishes,<br />
turtles and marine mammals is protected by the prohibition of high‐seas fishing within PIPA. The protected ocean<br />
waters surrounding the 8 <strong>Phoenix</strong> <strong>Islands</strong> provide the large scale physical, chemical and biological context. This<br />
includes some of the food resources – plank<strong>to</strong>n, larvae and pelagic fishes ‐‐ that are part of the larger ecology of<br />
the reefs.<br />
Part of the open‐ocean environment has yet <strong>to</strong> be surveyed – the invertebrate organisms and larval forms that<br />
make up the zooplank<strong>to</strong>n. While the primary creation of food from sunlight is the role of phy<strong>to</strong>plank<strong>to</strong>n and other<br />
pho<strong>to</strong>synthetic micro‐organisms, the zooplank<strong>to</strong>n that consume these cells are essential links <strong>to</strong> larger animals,<br />
including eventually the larger fish and whales. Zooplank<strong>to</strong>n are also an important food resource for coral and<br />
planktivorous fishes on the reefs. We have almost no information about the biodiversity or abundance of the<br />
zooplank<strong>to</strong>n in PIPA waters. They are likely <strong>to</strong> be similar <strong>to</strong> other tropical regions, but given the remoteness of the<br />
<strong>Phoenix</strong> <strong>Islands</strong>, could include species that are rare or unknown elsewhere.<br />
During the <strong>2009</strong> expedition, we made a preliminary survey of the zooplank<strong>to</strong>n community around the islands. For<br />
small organisms, we made two plank<strong>to</strong>n <strong>to</strong>ws, and for larger and more fragile gelatinous made four ‘blue‐water’<br />
SCUBA dives <strong>to</strong> observe and collect specimens in individual jars. These specimens may be the first from this remote<br />
part of the Western Pacific Ocean.<br />
Summary of Results<br />
Date, time and locations of the 4 Blue‐water dives are given in Table 1. In all cases, dives were conducted<br />
approximately 1 km seaward of the anchorage point of Nai’a at each of the islands. Dives typically lasted about 45<br />
minutes, and divers worked at various depths between the surface and the maximum listed in the table.<br />
The two plank<strong>to</strong>n <strong>to</strong>ws were made with a 50 cm diameter plank<strong>to</strong>n net, with 150 µm mesh, <strong>to</strong>wed behind the dive<br />
skiff just below the surface for 8‐10 minutes. The <strong>to</strong>ws were not quantitative, but meant only <strong>to</strong> provide a sample<br />
of the diversity of smaller organisms. Both <strong>to</strong>w samples contained large amounts of flocculent phy<strong>to</strong>plank<strong>to</strong>n and<br />
smaller numbers of zooplank<strong>to</strong>n. Samples were preserved in 70% ethanol for later analysis. (Formalin was<br />
unavailable).<br />
Table 1.<br />
Dive 1 Dive 2 Dive 3 Dive 4<br />
Date 9/14/09 9/17/09 9/20/09 9/22/09<br />
Time 1500 1430 1430 1045<br />
Location Nikumaroro Kan<strong>to</strong>n Ender bury Orona<br />
Depth 78 ft 51 ft 88 ft 80 ft<br />
Temperature 85 F 85 F 83 F 84 F<br />
Divers L.Madin, K.Madin L.Madin, K.Madin L.Madin, K.Madin L.Madin, K.Madin<br />
S<strong>to</strong>ne, Dynner S<strong>to</strong>ne, Cook S<strong>to</strong>ne, Skerry S<strong>to</strong>ne, Rotjan<br />
Campbell Wildermuth Stringer<br />
The water column observed during the dives was typical of the oligotrophic open ocean, with very clear blue water<br />
and sparse plank<strong>to</strong>nic organisms. Divers both collected organisms in jars and recorded organisms that were seen<br />
Page 8 of 35
ut not collected. Most animals seen were familiar and specimens were not preserved once their presence was<br />
recorded. Diving observations are only qualitative, and it is always possible that species were overlooked by the<br />
divers. The zooplank<strong>to</strong>n species collected are summarized in Table 2. Numbers of animals seen or collected are<br />
given for each dive. The + after the number indicates that additional individuals were seen but not collected; a + by<br />
itself indicates seen only.<br />
Table 2.<br />
Taxon Dive 1 Dive 2 Dive 3 Dive 4 Total<br />
Radiolarian colonies 2+ 4+ 1+ 1+ 8+<br />
Plank<strong>to</strong>nic forams 1 1<br />
Coral larvae 14+ 2+ 2+ 18+<br />
Medusae<br />
Pelagia noctiluca 1 1 1 3<br />
Aequorea globosa 1 1<br />
Unid. cubomedusa 1 1<br />
Siphonophores<br />
Forskalia sp. 4+ 4+<br />
Unid. calycophoran 1 1<br />
Ctenophores<br />
Cestum veneris 2+ 1+ 1 4+<br />
Leucothea multicornis 1 1<br />
Pteropods<br />
Cavolinia sp. 1 1 2<br />
Corolla sp. 1 1+ 2+<br />
Unid. Pteropod 2+ 2+<br />
Salps<br />
Cyclosalpa affinis (a) 1 1<br />
Weelia cylindrica (a & s) 7+ 7+<br />
Larvaceans<br />
Megalocercus sp 1+ 1+<br />
Crustaceans<br />
Sapphirina sp. + + +<br />
Unid. Crustacean larvae 2 2<br />
Grey reef sharks were seen on two dives, briefly at the beginning of Dive 2, when it had <strong>to</strong> be discouraged by the<br />
safety diver using a shark stick, and on Dive 4 when a 2 m shark came by two or three times <strong>to</strong> look at the divers,<br />
but didn’t approach. These were both larger than most of the sharks seen around the reefs. On most dives, two or<br />
three juvenile fish hung around the divers much of the time.<br />
Discussion<br />
The gelatinous plank<strong>to</strong>n collected was typical of oligotrophic ocean conditions. All of the species seen in PIPA have<br />
also been recorded from the Celebes Sea (Madin, unpubl.) and from the Sargasso Sea, with the possible exception<br />
of the cubomedusa, which has not yet been identified. All are adapted <strong>to</strong> the low nutrient, low food resource<br />
environment. Colonial radiolarians are typical of the oligotrophic tropics, as the colonies include algal cells that<br />
provide nutrition <strong>to</strong> their pro<strong>to</strong>zoan hosts. The pteropods and salps are particle feeders that use different methods<br />
<strong>to</strong> filter small particles of all types from the water column. The siphonophores and ctenophores found are<br />
preda<strong>to</strong>rs that specialize in capturing very small crustacean and other zooplank<strong>to</strong>n, either with fine stinging<br />
tentacles (siphonophores) or sticky body surfaces (ctenophores). Such small prey were visible in the guts of the<br />
ctenophore Cestum veneris. Pelagia is an omnivorous preda<strong>to</strong>r that consumes gelatinous animals as well as<br />
crustaceans. Cubomedusae are often fish preda<strong>to</strong>rs, and it is a bit surprising <strong>to</strong> find one in such a sparse<br />
Page 9 of 35
environment, but it may have drifted out from closer <strong>to</strong> the island. The copepod Sapphirina, seen on two dives, is<br />
associated with salps, and suggests their presence even when they were not seen by the divers.<br />
The four dive sites differed in the animals seen. Dive 1 at Nikumaroro had the largest abundance of coral larvae. At<br />
Kan<strong>to</strong>n none were seen, but there was the largest diversity of medusae and siphonophores. No salps were found<br />
on the first two dives, but Weelia cylindrica was abundant on the dive 4 at Orona. However, given the limited<br />
sampling time at each site it would be premature <strong>to</strong> conclude that these observations represent distinct patterns<br />
of distribution. It is more likely that these species, and others, occur patchily throughout the waters of PIPA.<br />
This survey was limited in scope and sampling methodology, but does suggest that the waters of PIPA are typical of<br />
the tropical open ocean, with many cosmopolitan species of gelatinous plank<strong>to</strong>n that probably fit in<strong>to</strong> the food<br />
web here much as they do in other locales. The survey was not adequate <strong>to</strong> map the abundance of small<br />
zooplank<strong>to</strong>n around the islands that might be food resources for the reef community. There are clearly many<br />
planktivorous fishes, as well as the corals themselves, that depend on zooplank<strong>to</strong>n for much of their diet. Our<br />
sampling capability was insufficient <strong>to</strong> determine how much of this zooplank<strong>to</strong>n came from offshore waters and<br />
how much was meroplank<strong>to</strong>n or demersal plank<strong>to</strong>n local <strong>to</strong> the lagoon and reef itself. Future plank<strong>to</strong>n studies at<br />
PIPA should include quantitative, stratified sampling both upstream and downstream of the islands, and in the<br />
lagoons on different tidal cycles <strong>to</strong> estimate the input of zooplank<strong>to</strong>n <strong>to</strong> the fringing reefs and lagoon<br />
communities. This would ideally require use of an oceanographic ship and opening‐closing nets. Additional diving<br />
collections would help fill out the catalog of gelatinous animals, and could be conducted from a live‐aboard vessel.<br />
Page 10 of 35
Objective 1b: Deep Water ROV assessments<br />
Greg S<strong>to</strong>ne<br />
A Video Ray Remotely Operated Vehicle (model PRO 3 XE GTO) was used <strong>to</strong> survey beyond SCUBA depths at three<br />
islands. Those results are recorded on video tape and summarized below:<br />
Date Location Depth Observations<br />
09/13/09 McKean <strong>Islands</strong> 250 feet Healthy, low diversity coral cover (Platyseris spp.)<br />
<strong>to</strong> 250 feet in‐between sand patches<br />
9/18/09 Endurbury Island 325 feet Healthy, low diversity coral cover <strong>to</strong> 325 feet, 10<br />
sharks (gray reef and black tip) seen.<br />
9/21/09 Orona 200 feet Sharks<br />
Page 11 of 35
Objective 1c: Coral reef assessments i. Corals and benthic structure<br />
David Obura and Randi Rotjan<br />
Introduction<br />
The <strong>Phoenix</strong> <strong>Islands</strong> long term moni<strong>to</strong>ring programme for coral reefs has been conducted in 2000, 2002 and 2005,<br />
and a principal goal of this expedition was <strong>to</strong> provide the fourth time point, in <strong>2009</strong>. Most significantly, this is the<br />
second sample point after mass bleaching and mortality of corals that occurred after the sampling done in 2002,<br />
that was likely the most severe temperature anomaly for coral reefs in recorded his<strong>to</strong>ry. This survey will give the<br />
first strong indication of recovery potential six years after the mortality event. Methods applied were selected for<br />
consistency with past moni<strong>to</strong>ring efforts, but also <strong>to</strong> upgrade the accuracy and precision of measurements <strong>to</strong> be<br />
consistent with other assessment programmes in the region and globally. We conducted a variety of both<br />
qualitative and quantitative assessments, including visual estimates, pho<strong>to</strong>quadrats <strong>to</strong> assess percent live coral<br />
cover, and genera‐level diversity and abundance measurements over line transects. Importantly, we also assessed<br />
size‐class information on corals, which yield insight in<strong>to</strong> the recovery dynamics of corals and resilience of the coral<br />
community. Coral mortality between 2002 and 2005 was estimated at 60% on average, though varied between 80<br />
and 40% on an island‐wide scale, and from 100% <strong>to</strong> about 20% on a site‐specific scale.<br />
Methods – coral/benthic assessment<br />
Methods are adapted from the IUCN Resilience Assessment pro<strong>to</strong>col (Obura and Grimsditch <strong>2009</strong>), and simplified<br />
for application on the expedition. Four datasets were collected on corals:<br />
1. Benthic cover/pho<strong>to</strong>quadrats<br />
2. Coral genus composition<br />
3. Coral genus size class distributions<br />
4. Reef resilience indica<strong>to</strong>rs<br />
Benthic Cover/Pho<strong>to</strong>quadrats<br />
Digital still pho<strong>to</strong>graphs of the reef substrate are taken from a height of approximately 0.6‐0.75 meters above the<br />
substrate using natural light and setting the white balance at the survey depth <strong>to</strong> enhance reds and help<br />
distinguish classes such as coralline algae. Pho<strong>to</strong>graphs were taken haphazardly<br />
over the study site, following the line of the coral belt transects. 40‐44 images were<br />
collected per site, from which images for analysis will be randomly selected.<br />
Pho<strong>to</strong>graphs are downloaded on<strong>to</strong> a computer, and analysed for benthic<br />
composition using dedicated software such as Coral Point Count (Kohler and Gill<br />
2006 (http://www.nova.edu/ocean/cpce/index.html) or Pho<strong>to</strong>Grid. Provisionally,<br />
25 points will be used for recording data from each pho<strong>to</strong>graph, and the results for<br />
4 images will be combined <strong>to</strong>gether <strong>to</strong> form one sample, or ‘transect’, of 100<br />
points. Not less than six of these transects (i.e. 24 images) are needed <strong>to</strong> calculate<br />
the mean and standard deviation of cover types, and preferably 10 ‘transects’ (40<br />
images) should be scored for each site.<br />
Coral genus composition<br />
Proportional abundance of all genera at a site was estimated on a five‐point scale. This is done <strong>to</strong>wards the end of<br />
the dive when an overall impression of the sampling site has been made, and the relative abundance of genera can<br />
be estimated.<br />
Codes Class Explanation Numerical (approximate)<br />
D 5 Dominant Dominate the coral community<br />
and/ or structure of the site<br />
>30% of coral cover<br />
A 4 Abundant Visually abundant and seen in large 10‐30% coral population by number or area<br />
Page 12 of 35<br />
Sample pho<strong>to</strong> quadrat. Pho<strong>to</strong>s of<br />
the benthos were taken at each<br />
site for later area measurements<br />
of various benthic structures.
numbers. Co‐dominate the site and/or large number of colonies (>100)<br />
seen/inferred in the immediate area of the site<br />
(2500 m 2 )<br />
C 3 Common Easily found/seen on site, but not<br />
dominant in any way<br />
U/O 2 Uncommo<br />
n/<br />
Occasional<br />
Not easily found, but several<br />
individuals seen or can be found by<br />
dedicated searching.<br />
R 1 Rare Found by chance occurrence or<br />
only 1 or 2 found by dedicated<br />
searching.<br />
>1% of coral population by number or area<br />
and/or >20 colonies seen/inferred in the<br />
immediate area of the site (2500 m 2 )<br />
Sites<br />
Data were collected on 9 days at 26 sites on 6 of the islands, as summarized in the table below. Of these, 17 were<br />
leeward sites, 7 were windward and 2 were lagoon sites. We attempted <strong>to</strong> sample a windward site on each island,<br />
but this was not always possible due <strong>to</strong> conditions and time available.<br />
Date Island Code Site Name Longitude (W) Latitude (S) Exposure<br />
13/9/09 Nikumaroro N4 Naia Point 174o32.697' 4o39.335' lee<br />
13/9/09 N3 Landing 174o32.616' 4o40.477' lee<br />
13/9/09 N6 Norwich City 174o32.847' 4o39.652' lee<br />
14/9/09 N8 Turtle Nest Beach 174o30.905' 4o40.008' wind<br />
14/9/09 N11 Windward Wing wind<br />
14/9/09 N10 Southwest Corner 174o32.41' 4o40.87' lee<br />
15/9/09 McKean Mc1 Guano Hut 174o7.65' 3o35.52' lee<br />
15/9/09 Mc3 Windward wreck 174o7.61' 3o35.66' wind<br />
15/9/09 Mc2 Rush Hour 174o7.69' 3o35.86' lee<br />
17/9/09 Kan<strong>to</strong>n K24 Oasis 171o41.149' 2o50.098' wind<br />
17/9/09 K22 Satelliite Beach 171o43.51' 2o46.802' lee<br />
17/9/09 K21 Crash Landing 171 o 43.407 2 o 45.795 lee<br />
18/9/09 K20 Six Sticks 171o43.24' 2o48.337' lee<br />
18/9/09 K25 Steep To 171o42.511' 2o49.986' lee<br />
18/9/09 K19 Weird Eddy lee<br />
19/9/09 K8 Coral Castles 171o41.743' 2o48.814' lag<br />
20/9/09 Enderbury E3 Lone Palm 171o5.564' 3o7.06' lee<br />
20/9/09 E5 Southern Ocean 171o4.761' 3o8.855' wind<br />
20/9/09 E2 Observation Spot 171o5.549' 3o8.539' lee<br />
21/9/09 Rawaki R1 Deepwater 170o43.054' 3o43.222' lee<br />
21/9/09 R2 Stillwater 170o43.017' 3o43.26' lee<br />
22/9/09 Orona O11 Aerials 172o12.953' 4o31.961' wind<br />
22/9/09 O7 Algae Corner 172o13.616' 4o31.112' lee<br />
22/9/09 O8 Dolphin Ledge 172o10.932' 4o29.487' lee<br />
23/9/09 O3 Lagoon 3 172o10.509' 4o30.341' lag<br />
23/9/09 O13 Farside 172o8.241' 4o29.468' wind<br />
Preliminary Results<br />
Coral genera<br />
Thirty coral genera were recorded overall, with 24 being the maximum recorded at any one site, at Satellite Beach,<br />
Kan<strong>to</strong>n. Favia was the dominant and most widespread genus, followed by Porites, Montipora and Pavona. Favia,<br />
Porites and Montipora were the dominant genera recovering on many of the leeward and windward fore reefs,<br />
while Acropora and Pavona were dominent in the lagoons.<br />
These genera compared <strong>to</strong> a list of 34 genera recorded in 2000, 2002 and 2005. Genera not recorded during this<br />
survey included Stylocoeniella, Cycloseris, Echinophyllia and Stylophora. The absence of Stylophora is notable as<br />
this is among the most susceptible genera <strong>to</strong> bleaching, and its absence is indicative of decline as a result of the<br />
bleaching event of 2002‐3. The other genera are small and generally not dominant, and may have been present<br />
but missed during surveys.<br />
The principal coral communities noted in <strong>2009</strong> were:<br />
• Reef slopes – sites with the best growth and recovery were dominated by Favia, Montipora or Porites,<br />
with some regrowth of Pocillopora, which was co‐dominant with these other genera before bleaching.<br />
Page 14 of 35
Recovery by Acropora was as yet absent. The most highly impacted leeward reefs had these dominant<br />
genera but at lower densities, and few other genera.<br />
• Lagoon patch reefs – these were very different from each other, with Kan<strong>to</strong>n reefs showing heavy<br />
mortality of Acropora, but with regrowth by Acropora tables and foliaceous Pavona. In Orona lagoon,<br />
lagoon sites were dominated by small Goniastrea colonies along with other faviids, and high densities of<br />
small Tridacna clams up <strong>to</strong> 20 cm.<br />
Table A. Relative abundance of coral genera at study sites in the <strong>Phoenix</strong> <strong>Islands</strong>. Coding is by number of ‘x’s as<br />
follows: 5 – Dominant, 4 – Abundant, 3 – Common, 2 – Uncommon, 1 – Rare. Also shown are the number of<br />
genera per site and the number of sites sampled.<br />
Satelliite Beach<br />
Oasis<br />
Deepwater<br />
Aerials<br />
Six Sticks<br />
Steep To<br />
Observation Spot<br />
Algae Corner<br />
Crash Landing<br />
Coral Castles<br />
Palm Lone<br />
Site<br />
Sitenum E3 K22 K24 R1 O11 K20 K25 E2 O8 K21 K8 N10 O13 E5 N3 N8 R2 K19 Mc2 O7 Mc1 Mc3 O1 N11<br />
# genera 21 24 22 21 21 22 22 18 19 19 19 18 18 18 18 19 18 20 14 14 13 11 10 11<br />
Coral genus code<br />
Favia fav xxxxx xxxx xxxx xxxx xxxx xxxx xxxx xxxxx xx xxxx xx xxx xxx xxxxx xx xxxx xxxx xxx xxx xx xx xxxx xxx xxx 24<br />
Porites por xxxx xxxx xxxx xxxxx xxxxx xxxx xxxx xxxx xxxx xxx xxxx xxxx xxx xxxxx xxx xx xx xxxx x xxx xxx xxx 22<br />
Montipora mtp xxxxx xx xxx xxxx xxxx xxx xxx xxx xxxx xxx xxx xxx xxxx xxx xx xxx xxx xx xx xx xxx xx xx xx 24<br />
Pavona pav xxxx xxxx xxxx xxxx xxxx xxx xxx xxxx xxx xxx xxxxx xx xxx xxx xxx x xxx xxx xx x xx xx x 23<br />
Pocillopora poc xxx xxx xx xx xxx xxx xxx xxx xxx xxx xx xxx xxx xxx xxx xxx xx xx xxx xxx xxx xxx xxx 23<br />
Fungia fun xxxx xxx xxx xx xx xxx xxx xx xxx xxx xxx xxx xx xxx xxx x xx xx xxx xx x xx xxx xx 24<br />
Hydnopohora hyd xxxx xxxx xxxx xx xx xxxx xxxx xx xxxx xxx xx xxx xx xx xx xx xxx xx xx 19<br />
Leptastrea lep xxx xxx xxx xxx xxx xx xx xxx xxx xx xx xx x xx xx xx xx xx xx xxxx xx xx 22<br />
Psammocora psa xxx xx xx xx xx xxx xxx xxx xx xx xx xxx xxx xx xxx xx xx xx xx x xx xx xx 23<br />
Halomitra hal xxxx xxx xx xx x xxx xx xx xx xx xx xxx xx xxx xxx x x xx xxx xx xxx x 22<br />
Lep<strong>to</strong>seris les xxx xxx xx xxx xxx xx xx xxx xxx xxx xx xx xx xx xx xx xx x xx xx xx x 22<br />
Cyphastrea cyp xx xx xx xxx xxx xx x xxxx xx xx xxx xx xx xx x xx xxxx 17<br />
Favites fts xx xx xxx xx xxx xx xx xx xx xx xx x xx xx xx xx xx x x xx 20<br />
Platygyra pla xxx xxx xx xxx xx xx xx xx xxx xx xx xx xx xx xx x xx 17<br />
Acropora acr xxx xx xx xx x x xxxxx xx x xxx x xxx xx xx 14<br />
Herpolitha her xxx xx xx xx xx xx xx xx xx xx xx xx xxx xx 14<br />
Sandalolitha san xxx xx xx x xx xx x xx x x xxx xx x x xx xx 16<br />
Montastrea mon xxx xx xx x xx xx xx xxx xx xx xx xx x x 14<br />
Lobophyllia lob xx xx xx x xx x xx x x x xxx xxx xx xxx x 15<br />
Oxypora oxy xxx x xxx xx x xx x xx xx xx x 11<br />
Goniastrea gon xx xx xx x x xx xx xx x x x xxx 12<br />
Coscinaraea cos xx xx xx x xxx xx 6<br />
Turbinaria tur x xx xx xxx xx 5<br />
Plerogyra plg x x xx xxx 4<br />
Podabacea pod xx x x xxx 4<br />
Lep<strong>to</strong>ria leo xx xx x xx 4<br />
Pachyseris pac xx x x x xx 5<br />
Tubastrea tub xxx xx 2<br />
Gardineroseris gar x x 2<br />
Table B. Description of the principal coral communities and their state of recovery in <strong>2009</strong><br />
Fore reef,<br />
leeward<br />
sites with<br />
good<br />
recovery<br />
Fore reef,<br />
leeward<br />
sites with<br />
poor<br />
recovery<br />
Page 15 of 35<br />
Southwest Corner<br />
Recovery dominated by corals that survived the bleaching event, and re‐growth of<br />
these fragments – Montipora, and a Favia species, F. stelligera. Coral cover is up <strong>to</strong><br />
40‐80% at these reefs, and coralline algal cover is very high. Missing from these reefs<br />
are abundant branching corals of Pocillopora and Acropora<br />
Recovery is low on leeward sites that receive high levels of lagoon influence, on<br />
Kan<strong>to</strong>n and Nikumaroro. Lagoon waters have high temperatures, nutrients and<br />
sediment load, which all promote algal growth and suppress the survival of small<br />
corals. This influence is clear as it is maximum at the main point of lagoon outflow,<br />
and decreases away from this point depending on the principal current directions.<br />
Additionally, the presence of a shipwreck, which causes enrichment of iron in the<br />
otherwise iron‐poor oceanic waters, results in low coral health and promotion of a<br />
form of thick black algal turf. In some cases, the wrecks caused mass mortality of<br />
Farside<br />
Southern Ocean<br />
Landing<br />
Turtle Nest Beach<br />
Stillwater<br />
Weird Eddy<br />
Rush Hour<br />
Algae Corner<br />
Guano Hut<br />
Windward wreck<br />
Lagoon 1/channel<br />
Windward Wing<br />
Number of sites
Fore reef,<br />
windward<br />
sites with<br />
good<br />
recovery<br />
Fore reef,<br />
windward<br />
sites with<br />
poor<br />
recovery<br />
Lagoon<br />
sites<br />
corals before the bleaching (e.g. Norwich City on Nikumaroro, Algae Corner on<br />
Orona), and in others their influence clearly suppresses regrowth of corals (Kan<strong>to</strong>n).<br />
Windward reefs were a patchwork of robust coral growth and areas of rubble from<br />
wave energy before the bleaching. Now, regrowth of corals is evident at many sites<br />
(Porites, Montipora, Favia), though regrowth of fast growing species is absent<br />
(Acropora) <strong>to</strong> slow (Pocillopora). Where regrowth is dominated by Porites, a more<br />
diverse coral community is recovering due <strong>to</strong> the space provided by the massive<br />
Porites colonies.<br />
Due <strong>to</strong> high wave energy, recovery of windward reefs is slowed down as recovery<br />
corals suffer continual breakage and abrasion from mobile rubble. Where mortality<br />
was very high and coral cover very low, some windward reefs are showing little<br />
recovery. In the case of McKean, the presence of a new shipwreck may be retarding<br />
recovery, but more importantly, its isolation and the low coral cover following<br />
bleaching may mean that local reproduction of corals is very low, and very limited<br />
connectivity with other islands results in almost no recruitment of new corals.<br />
The shallowest coral communities suffered very high coral mortality (< 10 m in<br />
Kan<strong>to</strong>n, < 3 m in Orona), and recovery in these areas is still very limited. However<br />
deeper communities even of very sensitive Acropora in Kan<strong>to</strong>n survived quite well,<br />
and Acropora tables > 2 m diameter were common at 12‐3 m. Leafy Pavona species<br />
were common in some shallow sites and the deeper Acropora communities. In<br />
Orona, small faviids dominate the deeper coral communities, and these are at high<br />
abundance.<br />
Rapid assessment of benthic cover<br />
Coral mortality from 2002‐5 was estimated at<br />
60%, with coral cover declining from 37% <strong>to</strong> 15%<br />
in 2005 (fig. A). In <strong>2009</strong>, significant recovery was<br />
recorded, returning 50% of the cover lost,<br />
increasing <strong>to</strong> 26%. Coralline algae (CCA) continued<br />
<strong>to</strong> increase from 2005‐<strong>2009</strong> as reef recovery was<br />
proceeding. CCA cements the reef framework,<br />
which is important where so much mortality<br />
results in higher levels of coral rubble, so this<br />
cover of CCA will at least partially be converted <strong>to</strong><br />
coral cover in the near future. Conversely, the<br />
initial increase in algal turf from 2002‐2005 was<br />
reversed, as it declined in <strong>2009</strong> as coralline algal<br />
cover increased. Rubble from dead coral skele<strong>to</strong>ns<br />
was high in 2005 and <strong>2009</strong>, reflecting the ongoing<br />
processes of breakdown of the reef following coral mortality, with much of the rubble being covered by CCA and<br />
will eventually be fixed in<strong>to</strong> the reef framework or washed by waves in<strong>to</strong> deeper water.<br />
The condition of the reefs varied by exposure (windward, leeward and lagoon) and depth (fig. B). In general,<br />
leeward reefs had higher coral cover at al depth than windward reefs, with 20‐30% cover from 10 <strong>to</strong> 30 m depth,<br />
while coral cover at depth on the windward reefs was lower, due <strong>to</strong> wave energy and breakup of the reef<br />
framework causing high cover of rubble. Coral cover on patch reefs in the lagoons was high, at nearly 40%, though<br />
these are spread out among large areas of sand.<br />
Page 16 of 35<br />
Fig. A. Benthic covery of coral, coralline algae (CCA), algal turf and rubble in<br />
the <strong>Phoenix</strong> <strong>Islands</strong>, from 2000 <strong>to</strong> <strong>2009</strong>.
Fig. B. Variation in benthic cover by exposure (leeward, windward and lagoon) and depths zones in the <strong>Phoenix</strong> <strong>Islands</strong>, <strong>2009</strong>.<br />
Fig. C. Variation in hard coral cover among islands and by exposure (mean and standard error).<br />
Comparing among islands (fig. C), Enderbury and Rawaki had the best coral communities, particularly on the<br />
leeward reefs. The coral communities had recovered <strong>to</strong> nearly pre‐bleaching levels, with maxima of 80% cover<br />
from 10 <strong>to</strong> 30 m depth. Leeward reefs on other islands still showed high impacts of bleaching and mortality: on<br />
Kan<strong>to</strong>n and Nikumaroro and Orona, some lagoon effects were visible as a result of lower water quality, higher<br />
nutrients and sedimentation, causing slower recovery; on McKean, Kan<strong>to</strong>n and Orona, significant effects of<br />
shipwrecks on the leeward reefs were also clear, retarding coral recovery. Recovery on windward reefs was slower<br />
as a result of wave energy and breakage.<br />
Coral size class distributions<br />
Biomass of coral communities in the <strong>Phoenix</strong> <strong>Islands</strong> is dominated by corals in the size ranges 21‐40 and 41‐80 cm,<br />
while the abundance of corals is dominated by 6‐10 cm juveniles corals (fig. D). The number of smallest corals < 5<br />
cm is relatively low indicating low levels of recruitment and the isolation and low reproductive populations of<br />
Page 17 of 35
corals following the mass mortality in 2002‐3.<br />
Consequently, the main recovery appears <strong>to</strong> be from<br />
regrowth of coral fragments, which have now regrown<br />
in<strong>to</strong> the dominant 21‐80 cm sizes.<br />
Among genera (fig. E), Montipora and Favia were<br />
dominant in the size class distribution dataset,<br />
followed by Porites, Echinopora and Pavona. A large<br />
gap is then found <strong>to</strong> the less common genera from<br />
Cyphastrea and onwards down the x axis. Montipora is<br />
a fast‐growing genus, able <strong>to</strong> reproduce asexually from<br />
fragmentation, and was the dominant coral on some<br />
leeward sites on Enderbury and several windward<br />
sites. The high frequency of 6‐10 cm colonies in<br />
Montipora (fig. F) is largely from breakage of existing<br />
plates, while dominance of area is due <strong>to</strong> the large<br />
colonies up <strong>to</strong> 1.6 and 3.2 m, made<br />
up of many plates and leaves often<br />
from different initiating colonies.<br />
Favia is a slower‐growing genus and<br />
with greater <strong>to</strong>lerance of bleaching,<br />
and the key species, F. stelligera,<br />
forms submassive/columnar colonies<br />
that frequently break up in<strong>to</strong> smaller<br />
nubbins and columns, with regrowth<br />
spreading out from surviving<br />
fragments. Regrowth from fragments<br />
is illustrated by numerical dominance<br />
of the 11‐20 cm size class, and area<br />
dominance by the large area under<br />
21‐40 and 41‐80 cm colonies that<br />
contribute <strong>to</strong> the overall distribution<br />
in fig. D.<br />
Fig. F. Size class distributions of the dominant coral genera from size class transects, by number of colonies (left) and area (right). Low levels of<br />
recruitment and sexual reproduction are indicated by the low numbers of < 5 cm corals in all the dominant genera.<br />
Across sites, Lone Palm (E3, Enderbury) had the highest cover of corals, due <strong>to</strong> large Montipora and Favia colonies,<br />
while Orona lagoon (O3) had the highest number of colonies, due <strong>to</strong> many small colonies of Goniastrea,<br />
Cyphastrea, Fungia and Echinopora. The <strong>to</strong>p sites were well‐spread among islands – including in addition <strong>to</strong> the<br />
Page 18 of 35<br />
Fig. D. Size class distributions of all corals in the <strong>Phoenix</strong> <strong>Islands</strong>,<br />
by number and area of colonies.<br />
Fig. E. Relative abundance of coral genera by size class (number of colonies and area).<br />
Genera are ordered by <strong>to</strong>tal area from left <strong>to</strong> right.
above two, Deepwater (R1, Rawaki), Crash<br />
Landing (K21, Kan<strong>to</strong>n), Stillwater (R2), Aerials<br />
(O11, Orona) and Turtle Nest Beach (N8,<br />
Nikumaroro). Interestingly, the two <strong>to</strong>p sites by<br />
area both had very low numbers of small corals,<br />
emphasizing the importance of regrowth from<br />
surviving corals over recruitment for recovery <strong>to</strong><br />
date.<br />
Fig. H. Size class distributions of best sites from size class transects, by number of colonies (left) and area (right).<br />
Page 19 of 35<br />
Fig. G. Ranking of sites by size class distributions of corals.
Objective 1c: Coral reef assessments ii. Corallivory (fish‐coral trophic interactions)<br />
Randi Rotjan, David Obura, Stuart Sandin, and Les Kaufman<br />
Introduction<br />
It is well known that herbivores have numerous and diverse impacts on plant and algal fitness, community<br />
structure and ecosystem function. The importance of corallivory as a selective force, however, has been<br />
underestimated. Corallivores, or consumers of live coral tissue, employ a wide variety of feeding strategies and can<br />
be obligate or facultative coral feeders. A complex array of corallivores exists across the globe, represented by 11<br />
families of fishes and 5 invertebrate phyla and <strong>to</strong>taling over<br />
160 species known <strong>to</strong> consume scleractinian corals<br />
worldwide. Importantly, although these corallivores span a<br />
wide taxonomic range, they have been reported <strong>to</strong> feed on<br />
relatively few genera of hard corals, specifically, on only 28<br />
scleractinian genera worldwide. Damage by corallivores<br />
ranges from minor <strong>to</strong> lethal, but there is a growing body of<br />
evidence <strong>to</strong> support that even limited removal of tissue or<br />
skeletal structures has growth and/or fitness consequences<br />
for a scleractinian coral colony. The <strong>Phoenix</strong> <strong>Islands</strong> <strong>Protected</strong><br />
<strong>Area</strong> has provided an opportunity <strong>to</strong> examine corallivory in a<br />
recovering ecosystem, in the absence of local stressors. With<br />
Figure 1. Examples of spot biting (<strong>to</strong>p left Porites, bot<strong>to</strong>m right<br />
Pavona), focused biting (bot<strong>to</strong>m left Favia), and tip biting (<strong>to</strong>p<br />
right Pocillopora) in the <strong>Phoenix</strong> <strong>Islands</strong>. All pho<strong>to</strong>s by R. Rotjan.<br />
a relatively intact fish population and various levels of coral<br />
cover and diversity at various locales, PIPA provides an ideal<br />
situation <strong>to</strong> examine a gradient of corallivory in a remote<br />
location. Especially given that increasing reef stressors are<br />
increasingly diminishing global coral populations, examining the role of corallivores in reef trophodynamics is<br />
important <strong>to</strong> understand how fish‐coral interactions change with changing environmental conditions.<br />
Methods<br />
Corallivores differ in their feeding strategies, with different consequences for coral prey. ‘Mucus‐feeders’ consume<br />
only coral mucus without removing any other live coral tissue or underlying skele<strong>to</strong>n. Corallivores that remove<br />
coral tissue without damaging the underlying calcium carbonate skele<strong>to</strong>n are known as ‘browsers’. Bellwood &<br />
Choat (1990) distinguished two feeding modes for parrotfish that we apply<br />
here <strong>to</strong> all corallivores: ‘excava<strong>to</strong>rs’, which feed by removing live coral tissue<br />
with major portions of the underlying skele<strong>to</strong>n, and ‘scrapers’ , which<br />
remove live coral tissue while taking only little of the accompanying skele<strong>to</strong>n.<br />
These four categories can be used <strong>to</strong> classify the feeding strategies used by a<br />
wide variety of invertebrates and fish corallivores.<br />
Here, we investigated the corallivorous activity of scrapers and excava<strong>to</strong>rs on<br />
<strong>Phoenix</strong> <strong>Islands</strong> Reefs by coupling benthic reef assessments (Objective 1c i)<br />
with fish diversity, abundance, and biomass assessments (Objective 1c iii),<br />
and adding estimates of grazing incidence (percentage of colonies grazed) for<br />
each of the coral colony (identified <strong>to</strong> genus) in each transect. Colonies were<br />
classified as grazed if they showed at least six distinct spot‐biting scars (3<br />
pairs), or one large excavation scar (Figure 1). Intact colonies lacked such<br />
scars. Both freshly made and recovering grazing scars were counted. In this<br />
case, grazing incidence only reflects corallivory by scrapers and excava<strong>to</strong>rs;<br />
polyps removed by browsing corallivores (such as Chae<strong>to</strong>don spp.), or scars<br />
made by invertebrate corallivores (such as Drupella or Culcita) were not<br />
included.<br />
Page 20 of 35<br />
Figure 2. The incidence of corallivory across<br />
windward versus leeward sites located on 6<br />
of the 8 <strong>Phoenix</strong> <strong>Islands</strong> (Kiribati) in<br />
September <strong>2009</strong>. Bars represent means ± 1<br />
SEM. No difference (ND) was observed<br />
between windward versus leeward sites<br />
(unpaired t = 0.5224, df = 17, p = 0.6081).
Summary of Results<br />
Corallivory was present in all windward and leeward habitats, but was absent from the two lagoons sampled<br />
(Kan<strong>to</strong>n Island and Orona Island). We observed grazing on several coral genera that have not been previously<br />
reported in the literature: Hydnophora, Cyphastrea, Echinopora, Favites, Platygyra, and Halomitra. Grazing on<br />
these genera is likely not limited <strong>to</strong> the <strong>Phoenix</strong> <strong>Islands</strong>, but has been overlooked either due <strong>to</strong> an incomplete<br />
complement of fishes at other sites, or because there is a paucity of comprehensive corallivory studies worldwide.<br />
There was no difference between windward and leeward sites (Figure 2), and corallivory incidence ranged from 3‐<br />
24% across all sites (Figure 3). Across all sites, corallivory averaged around 9%, suggesting that an ecologically<br />
relevant portion of colonies regularly experience <strong>to</strong>tal or partial mortality, energy loss due <strong>to</strong> regeneration, or loss<br />
of reproductive effort due <strong>to</strong> fish grazing. However, it is apparent that many large colonies persist despite high<br />
levels of corallivory, suggesting some level of corallivory <strong>to</strong>lerance. Future studies might investigate the<br />
susceptibility or <strong>to</strong>lerance <strong>to</strong> corallivory.<br />
Corallivory was highest on Faviid corals (Figure 4). Taxonomic grazing patterns in PIPA resemble patterns in the<br />
Caribbean and elsewhere, with focused efforts on the following coral families: Faviidae, Poritidae, Pocilloporidae,<br />
Acroporidae, and Agaricidae (Figure 4). A <strong>to</strong>tal of 16 genera were found <strong>to</strong> be grazed across all sites. Although 25<br />
coral transects were completed, only 23 sites were completed for corallivory measures. Since there was no<br />
corallivory noted in lagoon habitats, only 21 sites contribute <strong>to</strong> the corallivory incidence compiled in Figure 4.<br />
Of the corallivorous fishes observed this trip,<br />
there were 20 scraper/excava<strong>to</strong>r species, and<br />
17 browser species (Table 1). Notably, no<br />
crown‐of‐thorns seastars (Acanthaster planci)<br />
were observed at any site, suggesting either<br />
that they are cryptic and present only in<br />
extremely low numbers, or that they are<br />
absent al<strong>to</strong>gether. Other invertebrate<br />
corallivores were present in low densities,<br />
including Drupella spp., Coralliophilla spp.,<br />
Culcita spp., Linckia laevigata, and several<br />
urchins and nudibranchs. However, no<br />
infestation of invertebrate corallivores was<br />
observed, suggesting that invertebrate<br />
corallivory is not a pressing issue for PIPA<br />
reefs at this time. Mucus‐feeders were also<br />
observed in low density, including Trapezia<br />
spp. and Tetralia spp. crabs.<br />
Page 21 of 35<br />
Table 1. Corallivores observed in PIPA, September <strong>2009</strong>. Only<br />
scrapers/excava<strong>to</strong>rs were included in grazing incidence calculations.<br />
Scrapers/Excava<strong>to</strong>rs:<br />
Browsers:<br />
Balistidae (4)<br />
Balistapus undulatus<br />
Balis<strong>to</strong>ides viridescens<br />
Melichthys niger<br />
Rhinecanthus aculeatus<br />
Labridae (3)<br />
Coris aygula<br />
Labropsis xanthonota<br />
Thalasomma lunare<br />
Monacanthidae (2)<br />
Amanses scopas<br />
Cantherhines dumerilii<br />
Pomacentridae (2)<br />
Plectroglyphidodon dickii<br />
P. johns<strong>to</strong>nianus<br />
Scaridae (6)<br />
Bolbome<strong>to</strong>pon muricatum<br />
Calo<strong>to</strong>mus carolinus<br />
Chlororus microrhinos<br />
C. sordidus<br />
Scarus frenatus<br />
S. ghobban<br />
Tetraodontidae (2)<br />
Arothron meleagris<br />
Canthigaster solandri<br />
Zanclidae (1)<br />
Zanclus cornutus<br />
Chae<strong>to</strong>dontidae (17)<br />
C. auriga<br />
C. bennetti<br />
C. ephippium<br />
C. kleinii<br />
C. lineolatus<br />
C. lunulatus<br />
C. meyeri<br />
C. ornatissimus<br />
C. pelewensis<br />
C. quadrimaculatus<br />
C. reticulatus<br />
C. trifascialis<br />
C. unimaculatus<br />
C. vagabundus<br />
Forcipiger flavissimus<br />
F. longisrostris<br />
Heniochus chrysos<strong>to</strong>mus<br />
H. varius
Page 22 of 35<br />
Figure 2. The incidence of corallivory, organized by coral taxonomic group, measured from 23 sites on<br />
the <strong>Phoenix</strong> <strong>Islands</strong> (Kiribati) in September <strong>2009</strong>.<br />
Figure 3. The incidence of corallivory across sites located on 6 of the 8 <strong>Phoenix</strong> <strong>Islands</strong> (Kiribati) in<br />
September <strong>2009</strong>.
Objective 1c: Coral reef assessments iii. Fish diversity, abundance, and biomass assessments<br />
Stuart Sandin and Les Kaufman<br />
Introduction<br />
Coral reefs are among the most diverse and productive marine ecosystems, but are also among the most<br />
threatened by human activities. At the local scale, fishing and pollution can directly alter the structure of reef<br />
communities, and at the global scale, the effects of climate change impose episodic stress <strong>to</strong> even the most<br />
remote reefs. Despite knowledge of the types of changes that can result from human impacts, the generality of<br />
these changes is far from certain. It also is not known <strong>to</strong> what extent local human impacts must be ameliorated <strong>to</strong><br />
enable coral reefs <strong>to</strong> rebound from acute disturbances of a more regional or global nature, such as bleaching,<br />
typhoons, or earthquakes. Furthermore, changes in community structure can be associated with dramatic<br />
alterations of ecological functioning, including changes in the rate of fisheries productivity and the rate of coral<br />
recovery following major disturbances (i.e., ecological resilience). To most effectively implement ecosystem<br />
approaches in the management of coral reefs, it is critical <strong>to</strong> understand the pathway by which reef ‘health’ is<br />
degraded, the functional consequences of these changes, and their implications for ecosystem services and in<br />
particular service res<strong>to</strong>ration following acute insults.<br />
The coral reefs of <strong>Phoenix</strong> <strong>Islands</strong> provide a unique setting <strong>to</strong> study the fundamental associations among reef<br />
organisms, in particular between reef fishes and the benthic organisms (namely, the corals and algae). To this end,<br />
we investigated the structure of the fish assemblage across the archipelago, providing quantitative insights in<strong>to</strong><br />
the patterns of abundance, biomass, and diversity of this taxon. Given the protection from fishing afforded by the<br />
regulations of the <strong>Phoenix</strong> <strong>Islands</strong> <strong>Protected</strong> <strong>Area</strong>, the reefs of the region should provide a clear baseline of the<br />
condition expected of little‐exploited reef ecosystems.<br />
Methods<br />
Surveys were conducted by one team of divers (Sandin and Kaufman). Stations were spaced haphazardly across<br />
the islands, with effort determined by available ship time and island itinerary. At each station, the team of tandem‐<br />
paired divers tallied all fishes as they were encountered within fixed‐length (25‐m) strip transects whose widths<br />
differed depending on direction of swim. Transect bearings were determined haphazardly along isobaths (between<br />
10 and 12m depth). Each diver was responsible for one‐half of the areas surveyed, as follows: large‐bodied vagile<br />
fishes ≥ 20 cm <strong>to</strong>tal length (TL) were tallied within an 8‐m wide strip (two 4‐m wide swaths separated by 1 m)<br />
surveyed on an initial “swim‐out” as the transect line was laid. This swim was completed within a 3‐5 minute<br />
window. Small‐bodied, less vagile and more site‐attached fish < 20 cm TL were tallied within a 4‐m wide strip<br />
surveyed on the return swim back along the laid transect line. Fishes were recorded by species or lowest<br />
recognizable taxon. Tallies were binned by 5‐cm TL class. Two transects were surveyed at each station. Thus, at<br />
each station, the densities of large‐bodied fishes were estimated within a 400 m 2 (2 × 25 × 8 m) area, and the<br />
densities of small fishes within a 200 m 2 (2 × 25 × 4 m) area. Additional species richness data were recorded <strong>to</strong><br />
complement those recorded on transects. Species presence was tallied within 1,000 m 2 (50‐m long by 20‐m wide)<br />
areas searched by 1‐way zigzag swims centered on the transect lines. Additional species observed outside of set<br />
areas were recorded <strong>to</strong> augment island‐by‐island taxonomic summaries.<br />
Transects provided the input <strong>to</strong> estimates of species‐ and size‐specific numerical densities. Various published,<br />
unpublished, and web‐based sources provided the length‐weight regression parameters necessary for converting<br />
numbers <strong>to</strong> biomass. Density and biomass were standardized <strong>to</strong> one square meter.<br />
Summary of Results<br />
The coral reefs of the <strong>Phoenix</strong> <strong>Islands</strong> support over 500 species of fishes, with representatives from the central,<br />
western, and eastern Pacific fish fauna (G. Allen, in review). Because of the remoteness of the islands and their<br />
situation in the equa<strong>to</strong>rial currents, there are a number of endemic fish species found only in the <strong>Phoenix</strong> <strong>Islands</strong><br />
and a few other central Pacific a<strong>to</strong>lls.<br />
Page 23 of 35
Ecologically, the fish assemblage of the<br />
<strong>Phoenix</strong> <strong>Islands</strong> had relatively high abundance<br />
and biomass, with domination by large‐bodies<br />
species including large preda<strong>to</strong>rs. Across 23<br />
sites in the forereef habitat (standardized <strong>to</strong><br />
depths of 10‐12m), we found an average<br />
abundance of 5.55 fish m ‐2 and average<br />
biomass of 259.6 g m ‐2 for the reef fish fauna.<br />
The abundance of fishes was dominated by<br />
small‐bodied planktivores (including anthias<br />
species and schooling damselfishes; Figure 1).<br />
The biomass of fish was dominated by large‐<br />
bodied and massive preda<strong>to</strong>ry species<br />
(including snappers, groupers, and, on some<br />
islands, sharks; Figure 2). The variability of<br />
biomass within the <strong>to</strong>p preda<strong>to</strong>r trophic<br />
group was largely due <strong>to</strong> extreme variation in<br />
Figure 1. Abundance of fish across six of the <strong>Phoenix</strong> <strong>Islands</strong>. Density is separated by trophic level.<br />
shark densities, with apparent evidence of<br />
shark harvest from some of the <strong>Phoenix</strong><br />
<strong>Islands</strong>. This is consistent with evidence of shark finning operations in the region in recent years.<br />
In sum, the reef fish assemblages of the <strong>Phoenix</strong> <strong>Islands</strong> are large and healthy, showing great similarity <strong>to</strong> other<br />
little‐fished coral reef ecosystems in the central Pacific. For example, the average fish biomass of the <strong>Phoenix</strong><br />
<strong>Islands</strong> is similar <strong>to</strong> that of the Northwestern Hawaiian <strong>Islands</strong> (Papahanaumokuakea National Marine Monument<br />
with 243 g m ‐2 on average) and Palmyra a<strong>to</strong>ll in the Line <strong>Islands</strong> (270 g m ‐2 ). These results demonstrate the unique<br />
characteristics of the reefs in the <strong>Phoenix</strong> <strong>Islands</strong>, where remoteness and local protection has prevented the<br />
reduction of reef fishes from his<strong>to</strong>rical, baseline states. The only deviation from this baseline condition is the<br />
seeming reduction of reef shark abundances, which should be viewed as an important fact in need of management<br />
attention under the auspices of the <strong>Phoenix</strong> <strong>Islands</strong> <strong>Protected</strong> <strong>Area</strong>. Abundant evidence in the scientific literature<br />
attests <strong>to</strong> the likely importance of an intact fish community <strong>to</strong> coral reef resilience. Our observations on this<br />
expedition suggest that the persistence of high fish biomass following the 2002 mass‐bleaching event, particularly<br />
within guilds that feed upon algae and benthic invertebrates, has been a key fac<strong>to</strong>r in the impressive regeneration<br />
of hard coral communities on PIPA reefs.<br />
Figure 2. Total biomass of fish across six of the <strong>Phoenix</strong> <strong>Islands</strong>. Biomass density<br />
is separated by trophic level.<br />
Page 24 of 35
Objective 1d: On‐shore (land‐based) Assessment<br />
Greg S<strong>to</strong>ne and Tukabu Teroroko<br />
Land Surveys and Activities<br />
Surveys were conducted on land at all islands by Tukabu Teroroko and Greg S<strong>to</strong>ne. Plastic, rope and metal debris<br />
was abundant on the windward beaches of all islands. Other notable observations are below:<br />
• Nikumaroro: we walked the beach form the landing <strong>to</strong> the lagoon and saw one coconut crab and no sign<br />
of the wheel rim seen by G. S<strong>to</strong>ne in 2002. We walked through old village and found what Tukabu thought<br />
was an old marae.<br />
• McKean: No evidence of rats or other rodents was seen and bait stations were observed everywhere. Bait<br />
stations on the windward side near the ship wreck still contained dry bait. Other stations on the leeward<br />
sides still had bait, but were wet inside (pho<strong>to</strong>, below right). The <strong>Islands</strong> was transected through the<br />
center. The shipwreck was inspected and continues <strong>to</strong> breakup and rust (pho<strong>to</strong>, below left).<br />
• Kan<strong>to</strong>n: The sir strip was inspected and appears <strong>to</strong> be in excellent condition. There are no holes, rough<br />
spots of any degradation. A box of educational materials was delivered <strong>to</strong> the school. The 30 villagers on<br />
Kan<strong>to</strong>n were low on food as the supply ferry was late in servicing the island. NAI’A left all excess food for<br />
the village including 30 kg rice, 20kg flour, 20 kg sugar, 2 cases of milk, 4 packs powdered milk, 500 tea<br />
bags. Of note at Kan<strong>to</strong>n were frequent sightings of 5‐12 bottlenose dolphins near the entrance <strong>to</strong> the<br />
lagoon. We walked around the old hotel and Pan Am airbase (see pho<strong>to</strong>s below). Rob Barrel of NAI’A<br />
prepared a memo detailing a vision for using the site as a PIPA <strong>to</strong>urism base that was submitted <strong>to</strong> PIPA<br />
management committee (appendix I).<br />
Page 25 of 35
• Enderbury: The island was overrun with rats and bird populations appeared low. We killed one rat and<br />
pho<strong>to</strong>graphed it:<br />
• <strong>Phoenix</strong> (Rawaki): There was no evidence of rats or rabbits on this island. Bird populations appeared<br />
robust.<br />
• Orona: We entered the lagoon by skiff and landed on one island in the northern area. Observed abundant<br />
giant clams and seabirds. Had <strong>to</strong> leave soon because of a rising tide, so observations were limited.<br />
Page 26 of 35
Objective 1e: Kiribati Fisheries Assessments<br />
Tuake Teema<br />
Background information<br />
This expedition’s purpose was <strong>to</strong> assist Kiribati in the event of conducting continuous studies on status of<br />
fisheries/coral in this PIPA Region.<br />
2000:‐ general fisheries studies by NEAq, WWF & NG<br />
2002:‐ coral moni<strong>to</strong>ring relating <strong>to</strong> Climate Change<br />
2007:‐ coral moni<strong>to</strong>ring relating <strong>to</strong> Climate Change<br />
<strong>2009</strong>:‐ general fisheries studies by NEAq, CI, WHOI, NG<br />
These ongoing studies represent a comprehensive evaluation process <strong>to</strong> move Kiribati <strong>to</strong> become a world heritage<br />
nation (PIPA Region). The documentation of this scientific expedition is handled by National Geographic, and we<br />
are working <strong>to</strong> build up a biological inven<strong>to</strong>ry about these islands. Biological & ecological parameters are useful<br />
<strong>to</strong>ols for fisheries management & conservation, and collection of comprehensive fisheries data & other relevant<br />
information within the <strong>Phoenix</strong> <strong>Islands</strong> is surely a biological inven<strong>to</strong>ry. These studies will help us <strong>to</strong> understand the<br />
effects of global warming on coral reefs, and will also help <strong>to</strong> identify endemic species.<br />
One of the most important outcomes of this trip is the effort <strong>to</strong> track the level of fishing activities in this<br />
designated PIPA region. Drastic decline of the shark fishery is observed in this <strong>2009</strong> trip, perhaps illegal fishing<br />
might be going on here. The threat of illegal fishing heightens the importance for Kiribati <strong>to</strong> meet its ICUN<br />
obligation <strong>to</strong> qualify for world heritage position in order <strong>to</strong> help protect PIPA. This qualification must be based on<br />
scientific facts.<br />
Methods<br />
Fish count is done by underwater visual census using a line transect of 25m by 8m. Coral count is also done by Line<br />
transect on point count. Pelagic species collection is done by dragging plank<strong>to</strong>n net at the stern of the boat. Coral<br />
sampling was undertaken for proper labora<strong>to</strong>ry works. Jellyfish and other gelatinous species were also preserved<br />
for lab observation, and also Kiribati target fishes.<br />
Summary of Results<br />
Pet fish for the aquarium trade is very much healthy here in the <strong>Phoenix</strong> <strong>Islands</strong>, since there has not been any<br />
fishing for those species in this area. The live‐fish trade is also very much healthy as we encountered several sizes<br />
of Napoleon Wrasses, indicating <strong>to</strong> us that they are still reproducing quite well. For food fish purposes, high<br />
abundance was observed all throughout the <strong>Phoenix</strong> Group, but ciguatera needs <strong>to</strong> be further investigated in this<br />
area. The need <strong>to</strong> study ciguatera is quite valuable <strong>to</strong> be able <strong>to</strong> advise people settling there for <strong>to</strong>urism purposes.<br />
Proper anchoring places are necessary <strong>to</strong> reduce threat <strong>to</strong> coral reefs, especially when <strong>to</strong>urism will be carried out<br />
in the future. So far, we have good data on coral‐associated fisheries but lack information on the deep bot<strong>to</strong>m<br />
species, Kiribati Fisheries Division should go ahead on this. There is also a demand <strong>to</strong> confirm whether tuna<br />
actually spawn at the <strong>Phoenix</strong> <strong>Islands</strong>; if they do, this would further demonstrate its solemn importance <strong>to</strong> be<br />
designated as a World Heritage Site. Further translocation of mangroves in Kan<strong>to</strong>n and the rest of these islands<br />
should be discussed <strong>to</strong> be able <strong>to</strong> provide more marine habitats for the marine lives. Enhancement program <strong>to</strong> get<br />
giant clams, arkshell and sea cucumbers <strong>to</strong> spawn at Kan<strong>to</strong>n should be considered; these programs may impact<br />
other islands. Giant clams and sea cucumbers are heavily fished throughout Gilbert Group and this enhancement<br />
program will help <strong>to</strong> res<strong>to</strong>re them where few or less people disturbed and interacted with these identified animals.<br />
Fisheries hatcheries may be installed in Kan<strong>to</strong>n with a wet labora<strong>to</strong>ry where people can do their work. What we<br />
observed at Kan<strong>to</strong>n recently during this trip is very much a sad s<strong>to</strong>ry <strong>to</strong> tell: residents were running out of food<br />
stuffs because the ships never drop there <strong>to</strong> despatch new food cargoes for them. The question we should ask<br />
ourselves, then, is how much we prepare <strong>to</strong> arrange ourselves <strong>to</strong> overcome all these difficulties if we are <strong>to</strong> get<br />
<strong>to</strong>urism in action?<br />
Page 27 of 35
Other issues that need <strong>to</strong> be carefully examined before eco<strong>to</strong>urism comes in<strong>to</strong> reality is the strict means of<br />
regulating polluting activities <strong>to</strong> safeguard marine organisms, wildlife and forestry in this group of islands. Kiribati<br />
is blessed and pleased <strong>to</strong> have a continuous support from the US Government through New England Aquarium<br />
(NEAq) and Conservation International (CI) <strong>to</strong> allocate highly academic scientists <strong>to</strong> conduct fisheries surveys for us<br />
in the <strong>Phoenix</strong> <strong>Islands</strong>, and for provision of funds for this overall <strong>2009</strong> survey. Scientific data like these will very<br />
much support our endeavour in protecting and managing what we have on these islands for the future of our<br />
young generations.<br />
Page 28 of 35
Objective 1f: Collaborative efforts<br />
MMAS (Marine Management <strong>Area</strong> <strong>Science</strong>) Contributions and Collaborations<br />
One of the scientific objectives of MMAS was <strong>to</strong> develop a means of assessing the ecological health (including<br />
resilience), beginning with coral reefs, applicable <strong>to</strong> all the world’s tropical nations with marine coastlines. This<br />
index of marine ecosystem health is called “CHI”, for “community health index”; it is also a transliteration of the<br />
Chinese concept of life force. MMAS needed CHI <strong>to</strong> create a common ecological context and baseline for its<br />
intensive studies of management effectiveness at various locations around the world. CHI was developed through<br />
support <strong>to</strong> work the Line <strong>Islands</strong> led by Scripps University, and this initial phase of work is being completed through<br />
inclusion of data from PIPA. The CHI project is a collaborative effort among CI, Scripps, BU, USD, and National<br />
Geographic; the principle scientists are Enric Sala, Stuart Sandin, David Obura, Forest Rohwer, and Les Kaufman.<br />
The <strong>2009</strong> PIPA expedition contributed <strong>to</strong> CHI through the fish and benthic transects, and through field trials of a<br />
microbial assay device developed for MMAS by Forest Rohwer, and tested at PIPA by Stuart Sandin. The work on<br />
CHI will benefit especially from the team’s discovery of aggressive regeneration of the coral communities in PIPA<br />
following the 2002 mass bleaching event. Our data from PIPA provide a baseline for a system subjected <strong>to</strong> very<br />
little local human impact, and still capable of mounting successional return <strong>to</strong> a coral‐dominated benthic<br />
ecosystem following a major disturbance.<br />
Coral Whisperer<br />
“Coral Whisperer” is a project under the Marine Management <strong>Area</strong> <strong>Science</strong> Program for Conservation<br />
International. The basic idea is <strong>to</strong> use patterns of gene expression in important reef‐building corals as a way of<br />
determining the nature and intensity of anthropogenic and other kinds of stress that the corals in any place are<br />
experiencing. The goal is the creation of a molecular diagnostic <strong>to</strong>ol for reef‐building corals that makes it easier <strong>to</strong><br />
know if management actions are having the desired effect in improving coral reef health. Two of the three model<br />
coral systems for CW occur (or did occur) in abundance in PIPA: a tabulate (table‐<strong>to</strong>p) coral found in a variety of<br />
situations but especially on the fore‐reef and well‐flushed regions in lagoons (Acropora hyacinthus), and lace coral,<br />
which reaches high abundance in some lagoonal environments in PIPA, and is a reef‐builder elsewhere in the<br />
Pacific (Pocillopora damicornis). The importance of getting samples from PIPA is that it can serve as a reference<br />
site representing very low local human impact on the coral transcrip<strong>to</strong>me. It is also an important site from a<br />
biogeographical perspective, <strong>to</strong> better understand coral systematics. On this trip, we collected 10 specimens of<br />
the former for genetic studies by Steve Palumbi at Stanford Marine Lab and 5 specimens of the latter species for<br />
work at Bos<strong>to</strong>n University by Les Kaufman, John Finnerty, and Nikki Traylor‐Knowles.<br />
Coral Fluorescence<br />
On this expedition we conducted our first field test for MMAS of the use of induced fluorescence of corals as a<br />
diagnostic for coral resilience at the colony and population level. Our system is based on a Nikon D2X in a Subal<br />
housing mated <strong>to</strong> a Nikon SB‐104 and Sea and Sea YS110 strobe system plus underwater exciter and band‐pass<br />
fluorescence filters purchased from NightSea, Inc. The goal on this trip was <strong>to</strong> work with a still camera and filter<br />
system <strong>to</strong> document patterns of coral fluorescence in broad daylight. The test was successful, revealing intense<br />
fluorescent activity in the epitheca (growing margins) of some coral species, and in the s<strong>to</strong>ma (mouth) of others.<br />
The next step is <strong>to</strong> apply it <strong>to</strong> coral recruits.<br />
Other Coral Collaborative Studies<br />
Several other coral researchers were invited <strong>to</strong> add mission objectives <strong>to</strong> the <strong>2009</strong> PIPA research cruise because<br />
these were supportive or complementary <strong>to</strong> our principle goals.<br />
Anne Cohen, Woods Hole Oceanographic Institute, studies the effects of ocean acidification on coral growth and<br />
development. This work is closely related <strong>to</strong> the MMAS objective of developing a multiple‐insult (acidification,<br />
bleaching, overfishing, pollution) assay for a coral colony’s ability <strong>to</strong> conduct routine repair of its skele<strong>to</strong>n as it is<br />
damaged on a daily basis by coral preda<strong>to</strong>rs, competi<strong>to</strong>rs, and disease, as well as <strong>to</strong> understand the regenerative<br />
process through labora<strong>to</strong>ry and field experiments. For Anne, a single core of a large colony of Porites lobata was<br />
Page 29 of 35
obtained <strong>to</strong> provide baseline growth rates and skeletal structure through time from a relatively pristine site that<br />
can be compared with similar data from elsewhere in this important reef‐building coral’s extremely broad range.<br />
Iliana Baums, Penn State University, is studying the population genetics of Porites lobata and Montipora capitata.<br />
As such, we have collected 25 samples of the former and 1 sample of the latter (the only colony we found). On a<br />
similar theme, Mikhail Matz (University of Texas‐Austin) is conducting a full scale Micronesia connectivity study<br />
using Acroporid corals. We have therefore collected 19 specimens of A. hyacinthus and 25 samples of A. cytherea<br />
for his genetic studies by Mikhail Matz. We have collected samples of Porites and Pocillopora for Konrad Hughens,<br />
Woods Hole Oceanographic Institution, who is examining coral stress indica<strong>to</strong>rs on a global scale.<br />
Both Andrew Baker (University of Miami) and Todd Lajeunesse (Penn State University) are studying invertebrate‐<br />
dinoflagellate symbioses, specifically, coral‐zooxanthellae relationships. To conduct their studies of symbiont<br />
population genetics and population dynamics, we have collected a broad range of host‐symbiont samples for both<br />
(detailed in the sample appendix). Similarly, we collected a broad range of hosts for Allen Chen (Academia Sinica),<br />
who is examining zooxanthellae diversity.<br />
Tim Werner (New England Aquarium and Bos<strong>to</strong>n University) is studying the systematics, population biology, and<br />
conservation of holothurids (sea cucumbers). We have collected 7 samples from the Orona Lagoon for his<br />
examination. Craig OSenberg is studying the dynamics of host‐macroborer interactions on Pacific reefs; we have<br />
thus collected 4 serpulid polychaetes (Christmas tree worms) and 2 vermetid mollusks on his behalf.<br />
Samples Collected (all less than 5 cm 2 ):<br />
Corals:<br />
7 Echinopora spp.<br />
31 Acropora hyacinthis<br />
8 Pocillopora spp.<br />
12 Psammocora spp.<br />
25 Porites lobata<br />
5 Lep<strong>to</strong>seris spp.<br />
4 Leptastrea spp.<br />
25 Acropora cytherea<br />
3 Coscinaria spp.<br />
194 various (all < 2 cm 2 ) – see appendix 1<br />
Page 30 of 35<br />
Other invertebrates:<br />
4 serpulids, 2 vermetids<br />
7 holothurid (sea cucumber) samples<br />
1 Porites lobata skeletal core
Objective 2: Medical objectives<br />
Craig Cook<br />
Conducting dive operations in remote locations requires special considerations and safety equipment <strong>to</strong> provide<br />
the lowest risk <strong>to</strong> those involved. Considerations included treatment of decompression illness and location and<br />
recovery of the lost diver in addition <strong>to</strong> the usual medical issues inherent in a large remote expedition.<br />
The <strong>Phoenix</strong> Island Protective <strong>Area</strong> Expedition <strong>2009</strong> (PIPA <strong>2009</strong>) implemented several unique pro<strong>to</strong>cols and dive<br />
plans dealing with the following:<br />
Decompression Illness:<br />
While rare, any dive below two atmospheres absolute (ATA) caries a risk of decompression illness directly related<br />
<strong>to</strong> time and depth. During the course of the expedition over five‐hundred hours of diving operations were<br />
conducted by the twelve member team without event. In the case of decompression illness, a portable<br />
recompression chamber was present onboard. The chamber was a Hyperlite monoplace capable of providing a US<br />
Navy Table 6 treatment table. The chamber insured that a diver could be treated within minutes of surfacing and<br />
symp<strong>to</strong>m onset. Without an onboard chamber, medical evacuation would require air ambulance service with a<br />
possibility of delay up <strong>to</strong> 24 hours. Operation of the chamber was undertaken by the Diving Medical Officer on<br />
site.<br />
The portable recompression chamber that was taken on the expedition.<br />
Diver Location Aides:<br />
Diving operations were undertaken over a 24 dive sites and six islands under both windward and leeward<br />
conditions. The <strong>Phoenix</strong> <strong>Islands</strong> while under the Kiribatti administration have no search and rescue (SAR) capability<br />
in the event of a diver who becomes separated from the diving team. To maximize prompt diver recovery, each<br />
dive team member carried a surface location aide in the form of a safety sausage. In the rare circumstance that a<br />
diver would be out of visual range, each buddy pair carried either a VHF radio tuned <strong>to</strong> the ship moni<strong>to</strong>ring<br />
frequency or a Personal Loca<strong>to</strong>r Beacon (PLB) in a pressure proof canister. Arrangements were made with the<br />
USCG Rescue Coordination Center Honolulu (RCC Honolulu) <strong>to</strong> provide the satellite latitude and longitude via SAT<br />
phone communication in the case of PLB activation. This would provide immediate positioning data <strong>to</strong> the ship<br />
without having <strong>to</strong> mobilize SAR rescue resources from the USCG. In addition a four element yagi direction finding<br />
antennae capable of homing <strong>to</strong> a 121.5 MHZ signal was available for PLB location.<br />
Medical Issues:<br />
The length and remoteness of the PIPA <strong>2009</strong> expedition placed an increased likelihood of a medical event<br />
becoming a possibility. Medical supplies were available as well as the presence of an onboard medical physician.<br />
While there were a number of minor medical issues, no major medical events were experienced.<br />
Page 31 of 35
Objective 3: Media objectives<br />
Brian Skerry and Jeff Wildermuth<br />
Videography<br />
Jeff Wildermuth documented the PIPA <strong>2009</strong> Expedition in High Definition Video for the New England Aquarium,<br />
Conservation International, and the National Geographic Society. Sam Campbell, Brigitte Dewhirst, and Rob Barrel<br />
(Nai’a owner), also contributed video footage for the sake of the expedition. S. Campbell worked primarily on a<br />
high definition Sony EX1 camera and a Gates housing, whereas R. Barrel shot footage with a Sony HDV camera.<br />
Together, they recorded close <strong>to</strong> 10 hours of video.<br />
Pho<strong>to</strong>graphy<br />
Brian Skerry came <strong>to</strong> the <strong>Phoenix</strong> <strong>Islands</strong> on assignment for National Geographic Magazine (NGM). He<br />
pho<strong>to</strong>graphed the animals and ecosystems underwater as well as a small portion of the terrestrial side for a s<strong>to</strong>ry<br />
that will be published in NGM. Brian’s focus was on the abundant fish life found here and the recovering coral<br />
reefs. Among the species he pho<strong>to</strong>graphed are snapper, grouper, wrasse, trevally and surgeon fishes. Brian’s<br />
images will also be published in the forthcoming book about PIPA, which will be authored by Greg s<strong>to</strong>ne. He was<br />
assisted by Jeff Wildermuth.<br />
Jim Stringer has a passion for pho<strong>to</strong>graphy, diving, and travel, and was a participant in the 2005 PIPA expedition.<br />
He joined this expedition team as an amateur pho<strong>to</strong>grapher, with expedition goals of (1) learning the extent of<br />
coral recovery post 2005 (2) diving in the wonderful <strong>Phoenix</strong> <strong>Islands</strong> <strong>Protected</strong> <strong>Area</strong>, recently established by<br />
Kiribati, and (3) <strong>to</strong> contribute pho<strong>to</strong>‐documentation of the reef and islands, as well as the scientific, medical, and<br />
media participants of the expedition.<br />
Page 32 of 35
Appendix I: Memo on PIPA Tourism Potential<br />
Page 33 of 35<br />
<strong>Phoenix</strong> <strong>Islands</strong> <strong>Protected</strong> <strong>Area</strong><br />
Tukabu Teroroko, Direc<strong>to</strong>r<br />
Dear Tukabu:<br />
25 September, <strong>2009</strong><br />
As our expedition <strong>to</strong> PIPA winds down, I wanted <strong>to</strong> confirm for your<br />
future reference our interest in helping Kiribati develop sustainable<br />
eco<strong>to</strong>urism in the <strong>Phoenix</strong> <strong>Islands</strong>.<br />
As you know, the Fiji‐based ship, NAI’A, is largely responsible for<br />
bringing the <strong>Phoenix</strong> <strong>Islands</strong> <strong>to</strong> the attention of the diving and ocean<br />
conservation world. We first dived at Nikumaroro in 1997 when NAI’A<br />
was chartered by the aircraft recovery group TIGHAR <strong>to</strong> search for the<br />
remains of flyer Amelia Earhart. We then organized a diving research<br />
expedition in 2000 that included scientists from the New England<br />
Aquarium. They were so impressed with the conservation value of the<br />
<strong>Phoenix</strong> <strong>Islands</strong> that they sponsored another expedition on NAI’A with<br />
National Geographic in 2002. NAI’A has completed four scientific<br />
expeditions throughout the <strong>Phoenix</strong> <strong>Islands</strong> in support of PIPA and<br />
four <strong>to</strong> Nikumaroro in support of TIGHAR.<br />
Now that the <strong>Phoenix</strong> <strong>Islands</strong> <strong>Protected</strong> <strong>Area</strong> has been established,<br />
there is a clear opportunity for the government of Kiribati <strong>to</strong> develop a<br />
sustainable eco‐<strong>to</strong>urism operation in the islands. Our company is well‐<br />
placed <strong>to</strong> provide development and management expertise. With<br />
seventeen years of experience running ocean based high‐end eco‐<br />
<strong>to</strong>urism in Fiji and Tonga and eight expeditions <strong>to</strong> the <strong>Phoenix</strong> <strong>Islands</strong>,<br />
we understand what clients want and how best <strong>to</strong> deliver it.<br />
Intimate ecological exploration of tropical islands and reefs should and<br />
inevitably does feature going underwater as scuba divers, snorkelers or<br />
via submarines. Diving, fishing, and U/W exploration are areas where<br />
we have the environmental knowledge, cultural understanding,<br />
logistical expertise and enthusiasm borne of experience in this<br />
exhilarating and beautiful, but complex world under the surface.
We believe the demographic <strong>to</strong> whom PIPA would appeal is not unlike our client‐base in Fiji and<br />
Tonga: high‐end, well educated and experienced travelers looking for quality and originality. These<br />
travelers do not require absolute luxury, but they are willing <strong>to</strong> pay well for a safe, educational and<br />
unique eco‐<strong>to</strong>urism experience.<br />
Air access <strong>to</strong> Kan<strong>to</strong>n is of paramount importance. It may be that charter flights in and out of the<br />
Kan<strong>to</strong>n landing strip are a sustainable long‐term option and this bears further research, but we feel<br />
that a better solution will be the purchase of a modern 12‐passenger seaplane such as the Dornier<br />
Seastar. This allows not only reliable visi<strong>to</strong>r and staff transfer in and out of Kan<strong>to</strong>n and small‐scale<br />
eco<strong>to</strong>urism development of Orona and Nikumaroro, but fisheries moni<strong>to</strong>ring capability as well.<br />
The ideal PIPA lodge would consist of a main lounge/library/theatre/dining room <strong>to</strong>gether with<br />
modern “safari tents” built on existing foundations at the Southside site of the former Pan Am hotel.<br />
It would be entirely self‐sufficient with modern design and construction minimizing the<br />
requirement for outside supplies. It should be scalable – built <strong>to</strong> support 20‐30 guests initially and<br />
then expanded as its success is broadcast <strong>to</strong> the world. The lodge would also support a rotating<br />
group of expert scientists who, in addition <strong>to</strong> carrying out ongoing research for PIPA, would interact<br />
with the guests and add value <strong>to</strong> their experience. Daily activities would include scuba diving,<br />
snorkeling in the lagoon, bird watching, sailing on traditional Kiribati canoes, and perhaps catch‐<br />
and‐release bonefish and big game fishing.<br />
Especially when used in conjunction with a modern seaplane, the former Pan Am base is a special<br />
location. It is isolated from the large‐scale rubbish left behind by the colonial powers on Northside, it<br />
has a strong and interesting his<strong>to</strong>ry that will appeal <strong>to</strong> visi<strong>to</strong>rs and, of course, it is ideally suited <strong>to</strong><br />
supporting seaplane operations.<br />
The seaplane, besides facilitating access <strong>to</strong> and from PIPA, could be a significant <strong>to</strong>urism draw.<br />
Groups of divers or sightseers could make day trips <strong>to</strong> Nikumaroro or Orona, or even Enderbury<br />
and Manra in calm weather. To really maximize the value of PIPA’s outlying lagoonal islands, both<br />
for biodiversity as well as eco‐<strong>to</strong>urism, existing shallow tidal channels should be deepened and<br />
widened <strong>to</strong> allow reliable small boat access. Then boats could be left at the islands for the use of<br />
scientists and <strong>to</strong>urists who make short visits with the seaplane.<br />
PIPA is unique from an eco<strong>to</strong>urism perspective: a probable World Heritage Site where, with the<br />
right infrastructure development, discerning <strong>to</strong>urists could relatively easily experience a pristine<br />
ocean environment that exists nowhere else.<br />
It is early days yet for eco‐<strong>to</strong>urism in the <strong>Phoenix</strong> <strong>Islands</strong>, but I ask that you remember NAI’A and<br />
consider our expertise in this area when it comes time <strong>to</strong> develop an eco‐<strong>to</strong>urism plan.<br />
Best wishes,<br />
Robert Barrel<br />
Founder and Managing Direc<strong>to</strong>r, NAI’A Fiji<br />
rob@naia.com.fj<br />
Page 34 of 35
Appendix II: PIPA Research Permit<br />
Page 35 of 35
New England Aquarium<br />
Deepwater Shelf Connectivity Study<br />
<strong>Phoenix</strong> <strong>Islands</strong> <strong>Protected</strong> <strong>Area</strong><br />
• How many islands and sites were visited and what was done there in terms of types of<br />
surveys.<br />
The 11-day scientific expedition visited 6 islands/a<strong>to</strong>lls: Nikumaroro (2 days), McKean (1 day),<br />
Kan<strong>to</strong>n (3 days), Enderbury (1 day), Rawaki (1 day), and Orona (2 days).<br />
At all sites, a series of transects were conducted including a) coral reef assessments, b) fish<br />
assemblage assessments, c) corallivory assessments, and d) sample collections. Land surveys<br />
were also conducted at each island. Findings are summarized on page 4 of the Preliminary<br />
Expedition Report.<br />
• The data has been collected but what is the state of its analysis? Preliminary results yet?<br />
What are the plans for dissemination of results and when might this take place?<br />
The findings of the expedition will contribute important information <strong>to</strong> management of PIPA, as<br />
well as fundamental contributions <strong>to</strong> science. Rapid reporting of the coral bleaching and fish<br />
herbivore results will be prioritized, as these are extremely relevant <strong>to</strong> understanding the<br />
vulnerability of coral reefs <strong>to</strong> combined climate change and local threats. The findings confirm<br />
the importance of PIPA as a potential reference or observa<strong>to</strong>ry site, which will also be true for<br />
the other principal ecosystems – the deep sea, seamounts, pelagic and terrestrial. The expedition<br />
also found increased benefits from broadening the science and research interests in PIPA, and<br />
encourage further development of a more comprehensive research agenda and building capacity,<br />
particularly on Kan<strong>to</strong>n, <strong>to</strong> support this.<br />
These findings have been preliminary analyzed and presented at the following venues:<br />
-The 2010 Benthic Ecology Meetings in Wilming<strong>to</strong>n, NC (R. Rotjan)<br />
-The 2010 New England <strong>Area</strong> Coral Reef <strong>Science</strong> Salon (L. Kaufman)<br />
-A New England Aquarium Lowell Lecture in the IMAX theatre (R. Rotjan)<br />
-An informal presentation <strong>to</strong> Woods Hole Oceanographic Institution (R. Rotjan)<br />
At least 8 scientific manuscripts are currently in preparation detailing the biodiversity, bleaching,<br />
recovery, and current status of the <strong>Phoenix</strong> <strong>Islands</strong>, as well as several manuscripts in preparation<br />
by our collabora<strong>to</strong>rs who received samples. The first of these is currently in review at Coral<br />
Reefs, submitted by Obura et al.