Global Change Abstracts The Swiss Contribution - SCNAT
Global Change Abstracts The Swiss Contribution - SCNAT
Global Change Abstracts The Swiss Contribution - SCNAT
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138 <strong>Global</strong> <strong>Change</strong> <strong>Abstracts</strong> – <strong>The</strong> <strong>Swiss</strong> <strong>Contribution</strong> | Oceans and Fresh Water Systems<br />
Large river floodplains potentially include the<br />
full range of freshwater ecosystems from permanently<br />
flowing channels to temporary pools and<br />
springs. Attempts to restore such complex systems<br />
require tools adapted to assess restoration success.<br />
In an analysis of invertebrate assemblages in the<br />
Rhone River floodplain (France), taxonomic-based<br />
indices (rarefied richness and assemblage composition)<br />
were compared with functional metrics<br />
using trait-based ratios as surrogates of ecosystem<br />
processes. <strong>The</strong>ir ability to respond to a gradient<br />
of hydrological connectivity was assessed in 7<br />
cut-off channels. <strong>The</strong> sampling design included<br />
2 sites/channel (upstream and downstream), 4<br />
randomly chosen sampling points (0.5 x 0.5-m<br />
quadrats) /site, and 2 sampling seasons (spring<br />
and summer). Water physicochemical and habitat<br />
variables were recorded when invertebrates were<br />
sampled. Environmental variables, including water<br />
conductance, (NH 3-N), submerged vegetation<br />
cover, diversity of sediment grain size, and organic<br />
matter content of the sediment, were used to<br />
construct a synthetic variable describing the hydrological<br />
connectivity of each site with the main<br />
river channel. A quadratic regression of rarefied<br />
taxonomic richness and the connectivity gradient<br />
was not quite significant, but assemblage composition<br />
was strongly related to the gradient. Four<br />
of 8 trait-based metrics; were correlated with the<br />
connectivity gradient. Values of metrics that are<br />
surrogates for top-down control of assemblage<br />
structure and habitat stability (based on functional<br />
feeding groups) declined along the gradient<br />
from disconnected sites to more connected sites.<br />
Values of metrics that are surrogates for voltinism<br />
and food supply for water- column-feeding fish increased<br />
with connectivity. Top-down control and<br />
voltinism surrogates suggested a decline in predator-prey<br />
relationships and lower habitat stability,<br />
respectively, in the more connected sites. Assemblage<br />
composition and some of the trait-based<br />
metrics were sensitive to a flood that occurred before<br />
one of the sampling dates. Some of the traitbased<br />
metrics showed potential for explaining<br />
floodplain invertebrate assemblages and for monitoring<br />
postrestoration conditions in floodplain<br />
water bodies. However, the metrics were developed<br />
initially for studies of lotic systems and their<br />
use in heterogeneous floodplain water bodies will<br />
require further investigation, e.g., delineation of<br />
reference conditions for trait-based metrics.<br />
Journal of the North American Benthological Society,<br />
2007, V26, N4, DEC, pp 779-796.<br />
08.1-266<br />
Bipolar gene flow in deep-sea benthic foraminifera<br />
Pawlowski J, Fahrni J, Lecroq B, Longet D, Cornelius<br />
N, Excoffier L, Cedhagen T, Gooday A J<br />
Switzerland, England, Denmark<br />
Biodiversity , Ecology , Marine & Freshwater Biology<br />
Despite its often featureless appearance, the deepocean<br />
floor includes some of the most diverse<br />
habitats on Earth. However, the accurate assessment<br />
of global deep-sea diversity is impeded by<br />
a paucity of data on the geographical ranges of<br />
bottom-dwelling species, particularly at the genetic<br />
level. Here, we present molecular evidence<br />
for exceptionally wide distribution of benthic<br />
foraminifera, which constitute the major part of<br />
deep-sea meiofauna. Our analyses of nuclear ribosomal<br />
RNA genes revealed high genetic similarity<br />
between Arctic and Antarctic populations of three<br />
common deep-sea foraminiferal species (Epistominella<br />
exigua, Cibicides wuellerstorfi and Oridorsalis<br />
umbonatus), separated by distances of up to<br />
17 000 km. Our results contrast with the substantial<br />
level of cryptic diversity usually revealed by<br />
molecular studies, of shallow- water benthic and<br />
planktonic marine organisms. <strong>The</strong> very broad<br />
ranges of the deep-sea foraminifera that we examined<br />
support the hypothesis of global distribution<br />
of small eukaryotes and suggest that deep-sea<br />
biodiversity may be more modest at global scales<br />
than present estimates suggest.<br />
Molecular Ecology, 2007, V16, N19, OCT, pp<br />
4089-4096.<br />
08.1-267<br />
Earlier onset of the spring phytoplankton<br />
bloom in lakes of the temperate zone in a<br />
warmer climate<br />
Peeters F, Straile D, Lorke A, Livingstone D M<br />
Germany, Switzerland<br />
Marine & Freshwater Biology , Meteorology &<br />
Atmospheric Sciences , Oceanography , Biodiversity<br />
Ecology<br />
<strong>The</strong> decoupling of trophic interactions is potentially<br />
one of the most severe consequences of climate<br />
warming. In lakes and oceans the timing<br />
of phytoplankton blooms affects competition<br />
within the plankton community as well as foodweb<br />
interactions with zooplankton and fish. Using<br />
Upper Lake Constance as an example, we present<br />
a model-based analysis that predicts that in<br />
a future warmer climate, the onset of the spring<br />
phytoplankton bloom will occur earlier in the<br />
year than it does at present. This is a result of the<br />
earlier occurrence of the transition from strong<br />
to weak vertical mixing in spring, and of the as-