12.07.2015 Views

the humboldt current system of northern and central chile - figema

the humboldt current system of northern and central chile - figema

the humboldt current system of northern and central chile - figema

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

THE HUMBOLDT CURRENT SYSTEM OF NORTHERN AND CENTRAL CHILEworld have demonstrated that self-funding (e.g., through tourism business) is not feasible (Balmfordet al. 2004).Outlook, long-term research vision <strong>and</strong> future research frontiersAn outlook <strong>of</strong> <strong>the</strong> pressing scientific questions <strong>and</strong> tasks to be addressed in <strong>the</strong> short/mid-termfuture (during <strong>the</strong> next decade) within <strong>the</strong> HCS <strong>of</strong> nor<strong>the</strong>rn <strong>and</strong> <strong>central</strong> Chile should, as a minimum,include (1) studies <strong>of</strong> ocean–atmosphere interactions <strong>and</strong> <strong>of</strong>fshore oceanography, (2) research ininshore <strong>and</strong> <strong>of</strong>fshore oxygen-minimum eco<strong>system</strong>s, (3) research on inner inshore coastal oceanography<strong>and</strong> benthic-pelagic linkages, (4) development <strong>of</strong> an eco<strong>system</strong>-based adaptive resourcemanagement approach to fisheries that integrates socioeconomic aspects, (5) implementation <strong>of</strong> acoastal overarching network <strong>system</strong> for marine conservation-management, (6) novel approaches incoastal mariculture, (7) studies <strong>of</strong> marine non-indigenous species (NIS), (8) marine molecularbiology, particularly on genomics, <strong>and</strong> (9) training <strong>of</strong> Chilean marine taxonomists.A long-term HCS vision (during <strong>the</strong> coming two decades) should also, as a minimum, include(1) intensification <strong>of</strong> precautionary <strong>and</strong> integrative eco<strong>system</strong> management; (2) implementation <strong>of</strong>a high-sea conservation policy; (3) intensification <strong>of</strong> research on <strong>the</strong> continental slope, deep-sea<strong>and</strong> abyssal eco<strong>system</strong>s; (4) scientific <strong>and</strong> technological research on deep-sea gas (methane)hydrates; <strong>and</strong> (5) evaluations <strong>of</strong> <strong>the</strong> effects <strong>of</strong> future climate change.Short/mid-term scientific outlookResearch on ocean–atmosphere interactions <strong>and</strong> <strong>of</strong>fshore oceanographyThe HCS <strong>of</strong>fers unique opportunities for <strong>of</strong>fshore oceanographic studies (e.g., Strub et al. 1998)<strong>and</strong> considered as a whole, Chile <strong>and</strong> Peru represent between 15% <strong>and</strong> 20% <strong>of</strong> <strong>the</strong> world’s fisheryl<strong>and</strong>ings. Large-scale fluctuations in ocean climate (ENSO <strong>and</strong> <strong>the</strong> PDO) dominate interannual <strong>and</strong>interdecadal variability in <strong>the</strong> ocean, which in turn are linked to upwelling <strong>and</strong> climate changes(Chavez et al. 2003) <strong>and</strong> are considered key elements in <strong>the</strong> HCS functioning. Upwelling <strong>system</strong>spresently are experiencing ‘anomalous changes’ such as pr<strong>of</strong>ound changes in <strong>the</strong> physical <strong>and</strong>biogeochemical properties in <strong>the</strong> California Current Systems (Freel<strong>and</strong> et al. 2003, Grantham et al.2004), massive nitrogen loss in <strong>the</strong> Benguela upwelling <strong>system</strong> (Kuypers et al. 2005), <strong>and</strong> hydrogensulphide eruptions in <strong>the</strong> Atlantic Ocean <strong>of</strong>f sou<strong>the</strong>rn Africa <strong>and</strong> linked abrupt degradation <strong>of</strong>upwelling <strong>system</strong>s (Bakun & Weeks 2004, Weeks et al. 2004, Arntz et al. 2006). Such interannual<strong>and</strong> decadal variability <strong>and</strong> anomalous changes may intensify due to global climate changes, whichwill also affect <strong>the</strong> HCS, causing important changes in productivity, biogeochemical cycling <strong>and</strong>fisheries. Research on <strong>the</strong>se <strong>and</strong> related oceanographic topics is urgently needed for <strong>the</strong> HCS.Research on inshore <strong>and</strong> <strong>of</strong>fshore oxygen-minimum eco<strong>system</strong>sOxygen-minimum zones (OMZs) in <strong>the</strong> ocean generally form along <strong>the</strong> EBCs. The decomposition<strong>of</strong> upwelling-derived biomass in combination with sluggish circulation <strong>of</strong> mid-water massesstrongly enhance <strong>the</strong> hypoxia conditions, as is <strong>the</strong> case in <strong>the</strong> HCS (Levin & Gage 1998, Moraleset al. 1999, Levin 2002, Helly & Levin 2004, Ulloa & De Pol 2004). The HCS is characterised by<strong>the</strong> relative shallowness <strong>of</strong> <strong>the</strong> oxygen-minimum layer. The OMZ produces peculiar environmentswith organisms highly resistant to low oxygen concentrations (Levin et al. 2001, Gallardo et al.2004). These environments are unique in <strong>the</strong> HCS <strong>and</strong> quite different from those <strong>of</strong>f California(Arntz et al. 2006). They <strong>of</strong>fer diverse opportunities to develop frontier research, ranging from299

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!