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首页> 外文期刊>Paleoceanography >Holocene productivity changes off Adelie Land (East Antarctica)
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Holocene productivity changes off Adelie Land (East Antarctica)

机译:全新世生产力在Adelie Land(南极东部)改变

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[1] This study presents the first high-resolution multiproxy investigation of primary productivity (PP) duringthe Holocene from the Antarctic continental margins. Micropaleontological and geochemical data from thesediment core MD03-2601, associated to sea ice model outputs, give unprecedented insights into the biologicalpump of the Antarctic coastal area off Adelie Land in response to climatic changes. Plurimillennial andmillennial changes of PP are observed in the study area in response to changes in nutrient availability,stratification, and growing season duration, which are linked to sea ice, upwelling, wind, and glacier dynamics.The precessional cycle seems to be responsible in the PP long-term variations, while forcing factors involved atthe millennial timescale remain more enigmatic. Our results emphasize enhanced biological pump duringwarmer and windier Holocene phases because of a longer growing season and greater nutrient input. Antarcticcoastal and continental shelf zones may therefore represent a more intense carbon sink in the future.
机译:[1]这项研究提出了从南极大陆边缘全新世期间首次生产力(PP)的首次高分辨率多代理调查。来自这些沉积物核心MD03-2601的微古生物学和地球化学数据与海冰模型的输出相关联,对响应气候变化的阿德利陆地南极沿海地区的生物泵提供了前所未有的见识。在研究区内,PP的百年和千禧年变化是由于养分的可利用性,分层和生长期的变化而引起的,这些变化与海冰,上升流,风和冰川的动力学有关。 PP的长期变化,虽然迫使千禧年时间尺度中涉及的因素仍然更加令人费解。我们的研究结果强调,由于更长的生长季节和更多的养分输入,在较新的和较暖的全新世阶段生物泵的流量增加。因此,南极沿海和大陆架地区可能代表未来更强烈的碳汇。

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