2015
DOI: 10.1016/j.dsr.2015.02.009
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Long-term (1993–2013) changes in macrozooplankton off the Western Antarctic Peninsula

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Cited by 153 publications
(199 citation statements)
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“…The Western Antarctic Peninsula (WAP) is one of the most rapidly warming areas on Earth41, and krill is the most abundant species in the coastal areas of this region23; predators such as fish, seabirds, penguins, seals and whales rely on this single resource. The presence of numerous krill-feeding whales in fjords, such as Potter Cove and others along the WAP, as well as the presence of the dominant benthic fish species Notothenia coriiceps , which feeds primarily on krill20, underscore the importance of krill for these regions.…”
Section: Discussionmentioning
confidence: 99%
“…The Western Antarctic Peninsula (WAP) is one of the most rapidly warming areas on Earth41, and krill is the most abundant species in the coastal areas of this region23; predators such as fish, seabirds, penguins, seals and whales rely on this single resource. The presence of numerous krill-feeding whales in fjords, such as Potter Cove and others along the WAP, as well as the presence of the dominant benthic fish species Notothenia coriiceps , which feeds primarily on krill20, underscore the importance of krill for these regions.…”
Section: Discussionmentioning
confidence: 99%
“…Larger krill may find maintaining position against a current to be less of a metabolic burden than age 1+ krill, and may choose to stay in an area with fewer predators than the coastal fjords. The observed abundance of age 1+ krill could also be related to multiyear patterns in krill recruitment, as 2013 was a particularly high recruitment year for krill in the WAP region (Steinberg et al 2015), although the lack of a strong age 2+ year class within the fjords suggests recruitment variability is not the full explanation for the observed length distributions as 2012 was also a strong krill recruitment year (Steinberg et al 2015).…”
Section: Minimizing Advective Lossesmentioning
confidence: 99%
“…Even though macronutrient concentrations in the water column during this period were low and uptake by phytoplankton was likely hampered, nutrients could still have been available through high bacterial remineralization, sloppy grazing, and/or viral lysis which peaks after the end of the bloom (Ducklow et al, 2012b;Brum et al, 2015). Additionally, the build-up of phytoplankton biomass could also have been ended by strong grazing, as is often observed at the sea ice edge, an attribute not covered in the RaTS program (Ross et al, 2008;Saba et al, 2014;Steinberg et al, 2015).…”
Section: Influence Of Presence/absence Of Sea Ice On Phytoplankton Dymentioning
confidence: 99%