2005
DOI: 10.3354/meps300003
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Persistence of labile organic matter and microbial biomass in Antarctic shelf sediments: evidence of a sediment ‘food bank’

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Cited by 167 publications
(130 citation statements)
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“…Additionally, cold Southern Ocean deep-sea conditions can result in the persistence of organic matter in sediments and act as a year round food supply to deposit feeding fauna, dampening the effects of strong seasonal pulses of food (Mincks et al, 2005;Glover et al, 2008). When compared to the similarly sized deep-sea protobranch Ledella pustulosa (Gage, 1994), the Antarctic species have lower overall growth performances, although this is not expected to be related to food availability.…”
Section: Discussionmentioning
confidence: 99%
“…Additionally, cold Southern Ocean deep-sea conditions can result in the persistence of organic matter in sediments and act as a year round food supply to deposit feeding fauna, dampening the effects of strong seasonal pulses of food (Mincks et al, 2005;Glover et al, 2008). When compared to the similarly sized deep-sea protobranch Ledella pustulosa (Gage, 1994), the Antarctic species have lower overall growth performances, although this is not expected to be related to food availability.…”
Section: Discussionmentioning
confidence: 99%
“…The Antarctic Peninsula shelf undergoes seasonal deposition of high amounts of phytodetritus coming from fast-sinking sea ice algae aggregates (Riebesell et al 1991) and from post-sea ice retreat summer phytoplankton blooms ). This material accumulates in sediments, where it constitute persistent ''food banks'' that are available to benthic consumers all year round (Mincks et al 2005. Here, data from stations sampled during the PS81 cruise accordingly suggested that over the 2008-2012 period, both average sea ice cover and surface primary productivity were higher in Weddell Sea than in the other areas Dorschel et al 2015; Table 1).…”
mentioning
confidence: 86%
“…The Antarctic Peninsula is indeed one of the most quickly warming regions of the world, and as a result, sea ice cover in this area shows an important decrease (Turner et al 2005;Parkinson and Cavalieri 2012). These changes will undoubtedly in turn modify sea urchin trophic environment, and warmer temperatures notably cause a decrease in the amount of material available to benthic consumers in ''food banks'' (Mincks et al 2005). While sea urchin responses to such changes are difficult to predict, our results suggest that differences in adaptive strategies could lead to different effects on each of the studied families' feeding habits, biology and, ultimately, distribution in the Southern Ocean.…”
mentioning
confidence: 99%
“…However, minor increases in temperature will also increase overall metabolic rates of benthic and pelagic communities. In Antarctic regions, one of the key processes that is thought to govern the deepwater soft sediment communities is captured in the FOODBANCS hypothesis (Smith and DeMaster, 2008), according to which concentrated summer food pulses and slow microbial enzymatic activity caused by the cold temperatures provide a long-lasting food bank that supports benthic metazoan communities (Mincks et al, 2005). With increasing temperatures, bacterial recycling will be enhanced, potentially leading to a non-linear increase in the overall metabolism of the benthic community and increased food limitation in deeper seas ( Figure 4A).…”
Section: The Polar Deep Seasmentioning
confidence: 99%