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Under the sea ice: Exploring the relationship between sea ice and the foraging behaviour of southern elephant seals in East Antarctica

机译:海冰下:探索南极东部海冰与南部象海豹觅食行为的关系

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摘要

Investigating ecological relationships between predators and their environment is essential to understand the response of marine ecosystems to climate variability and change. This is particularly true in polar regions, where sea ice (a sensitive climate variable) plays a crucial yet highly dynamic and variable role in how it influences the whole marine ecosystem, from phytoplankton to top predators. For mesopredators such as seals, sea ice both supports a rich (under-ice) food resource, access to which depends on local to regional coverage and conditions. Here, we investigate sex-specific relationships between the foraging strategies of southern elephant seals (Mirounga leonine) in winter and spatio-temporal variability in sea ice concentration (SIC) and coverage in East Antarctica. We satellite-tracked 46 individuals undertaking post-moult trips in winter from Kerguelen Islands to the peri-Antarctic shelf between 2004 and 2014. These data indicate distinct general patterns of sea ice usage: while females tended to follow the sea ice edge as it extended northward, the males remained on the continental shelf despite increasing sea ice. Seal hunting time, a proxy of foraging activity inferred from the diving behaviour, was longer for females in late autumn in the outer part of the pack ice, similar to 150-370 km south of the ice edge. Within persistent regions of compact sea ice, females had a longer foraging activity (1) in the highest sea ice concentration at their position, but (ii) their foraging activity was longer when there were more patches of low concentration sea ice around their position (either in time or in space; 30 days & 50 kin). The high spatio-temporal variability of sea ice around female positions is probably a key factor allowing them to exploit these concentrated patches. Despite lack of information on prey availability, females may exploit mesopelagic finfishes and squids that concentrate near the ice-water interface or within the water column (from diurnal vertical migration) in the pack ice region, likely attracted by an ice algal autumn bloom that sustains an under-ice ecosystem. In contrast, male foraging effort increased when they remained deep within the sea ice (420-960 km from the ice edge) over the shelf. Males had a longer foraging activity (i) in the lowest sea ice concentration at their position, and (ii) when there were more patches of low concentration sea ice around their position (either in time or in space; 30 days & 50 km) presumably in polynyas or flaw leads between land fast and pack ice. This provides access to zones of enhanced resources in autumn or in early spring such as polynyas, the Antarctic shelf and slope. Our results suggest that some seals utilized a highly sea ice covered environment, which is key for their foraging effort, sustaining or concentrating resources during winter. (C) 2017 Elsevier Ltd. All rights reserved.
机译:调查捕食者与其环境之间的生态关系对于了解海洋生态系统对气候变化和变化的响应至关重要。在极地地区尤为如此,在极地地区,海冰(一个敏感的气候变量)在其如何影响从浮游植物到顶级捕食者的整个海洋生态系统中起着至关重要但高度动态和可变的作用。对于海豹这样的中捕食者,海冰都支持丰富的(冰下)食物资源,能否获得取决于当地到区域的覆盖范围和条件。在这里,我们调查了冬季南象海豹(Mirounga leonine)的觅食策略与南极东部海冰浓度(SIC)和覆盖率的时空变化之间的性别特异性关系。我们用卫星跟踪了46个人在冬季从Kerguelen群岛到南极外围大陆架在2004年至2014年之间进行冬季换羽旅行。这些数据表明海冰的使用有明显不同的一般模式:而女性随着海冰边缘的扩展而趋向于跟随向北,尽管海冰增加,但雄性仍留在大陆架上。海豹狩猎时间是潜水行为推断的觅食活动的代名词,在深秋时分,女性在冰袋外围的觅食时间更长,类似于冰缘以南150-370公里。在致密海冰的持久区域内,雌性的觅食活动较长(1)在其位置处的最高海冰浓度下,但(ii)当其位置周围有更多的低浓度海冰块时,其觅食活动则较长(时间或空间; 30天50亲属)。女性位置周围海冰的高度时空变化可能是允许她们利用这些集中斑块的关键因素。尽管缺乏猎物可获得性的信息,但雌性仍可能利用浮游鱼类和鱿鱼,这些鱼类和鱿鱼集中在浮冰区冰水界面附近或水柱内(由于日间垂直迁移),可能被冰藻秋季开花所吸引冰底生态系统。相反,当雄性觅食力停留在架子上的海冰深处(距冰缘420-960公里)时,它们的觅食力增加。雄性的觅食活动更长(i)在其位置最低的海冰浓度下,以及(ii)当其位置周围有更多的低浓度海冰块时(在时间或空间上; 30天和50公里)大概是在polynyas或快速落冰和浮冰之间的瑕疵引线中。这提供了进入秋季或初春资源丰富的区域的通道,例如多年生植物,南极大陆架和斜坡。我们的结果表明,某些海豹利用了高度被海冰覆盖的环境,这对于冬季觅食,维持或集中资源至关重要。 (C)2017 Elsevier Ltd.保留所有权利。

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  • 来源
    《Progress in Oceanography》 |2017年第8期|17-40|共24页
  • 作者单位

    UPMC Univ, Sorbonne Univ, Paris 06, UMR CNRS IRD MNHN 7159,LOCEAN IPSL, F-75005 Paris, France|Univ Tasmania, Inst Marine & Antarctic Studies, Private Bag 129, Hobart, Tas 7001, Australia;

    UPMC Univ, Sorbonne Univ, Paris 06, UMR CNRS IRD MNHN 7159,LOCEAN IPSL, F-75005 Paris, France|British Antarctic Survey, Cambridge CB3 0ET, England;

    Hokkaido Univ, Inst Low Temp Sci, Kita Ku, N19 W8, Sapporo, Hokkaido 0600819, Japan|Univ Tasmania, Antarctic Climate & Ecosyst Cooperat Res Ctr, Private Bag 80, Hobart, Tas 7001, Australia;

    Univ Tasmania, Antarctic Climate & Ecosyst Cooperat Res Ctr, Private Bag 80, Hobart, Tas 7001, Australia|Australian Antarctic Div, Channel Highway, Kingston, Tas 7050, Australia;

    Ctr Australian Weather & Climate Res, Australian Bur Meteorol, Hobart, Tas 7001, Australia;

    Australian Antarctic Div, Channel Highway, Kingston, Tas 7050, Australia;

    Univ Rochelle, CNRS, UMR 7372, Ctr Etud Biol Chize, F-79360 Villiers En Bois, France;

    Macquarie Univ, Dept Biol Sci, Sydney, NSW 2109, Australia;

    Univ Tasmania, Inst Marine & Antarctic Studies, Private Bag 129, Hobart, Tas 7001, Australia|Macquarie Univ, Dept Biol Sci, Sydney, NSW 2109, Australia|Sydney Inst Marine Sci, 19 Chowder Bay Rd, Mosman, NSW 2088, Australia;

    South Australian Res & Dev Inst, 2 Hamra Ave, West Beach, SA 5024, Australia;

    Univ Tasmania, Inst Marine & Antarctic Studies, Private Bag 129, Hobart, Tas 7001, Australia|Univ Tasmania, Antarctic Climate & Ecosyst Cooperat Res Ctr, Private Bag 80, Hobart, Tas 7001, Australia;

    UPMC Univ, Sorbonne Univ, Paris 06, UMR CNRS IRD MNHN 7159,LOCEAN IPSL, F-75005 Paris, France;

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