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揭示弗拉姆海峡(北冰洋)中与生物碳泵相关的远洋-底栖耦合关系。

Unveiling pelagic-benthic coupling associated with the biological carbon pump in the Fram Strait (Arctic Ocean).

作者信息

Ramondenc Simon, Eveillard Damien, Metfies Katja, Iversen Morten H, Nöthig Eva-Maria, Piepenburg Dieter, Hasemann Christiane, Soltwedel Thomas

机构信息

Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany.

MARUM, Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany.

出版信息

Nat Commun. 2025 Jan 20;16(1):840. doi: 10.1038/s41467-024-55221-x.

DOI:10.1038/s41467-024-55221-x
PMID:39833152
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC11747630/
Abstract

Settling aggregates transport organic matter from the ocean surface to the deep sea and seafloor. Though plankton communities impact carbon export, how specific organisms and their interactions affect export efficiency is unknown. Looking at 15 years of eDNA sequences (18S-V4) from settling and sedimented organic matter in the Fram Strait, here we observe that most phylogenetic groups were transferred from pelagic to benthic ecosystems. Chaetoceros socialis, sea-ice diatoms, Radiolaria, and Chaetognatha are critical components of vertical carbon flux to 200 m depth. In contrast, the diatom C. socialis alone is essential for the amount of organic carbon reaching the seafloor. Spatiotemporal changes in community composition show decreasing diatom abundance during warm anomalies, which would reduce the efficiency of a diatom-driven biological carbon pump. Interestingly, several parasites are also tightly associated with carbon flux and show a strong vertical connectivity, suggesting a potential role in sedimentation processes involving their hosts, especially through interactions with resting spores, which could have implications for pelagic-benthic coupling and overall ecosystem functioning.

摘要

沉降聚集体将有机物从海洋表层输送到深海和海底。虽然浮游生物群落会影响碳输出,但具体的生物及其相互作用如何影响输出效率尚不清楚。通过研究弗拉姆海峡沉降和沉积有机物中15年的环境DNA序列(18S-V4),我们发现大多数系统发育类群从浮游生态系统转移到了底栖生态系统。群居角毛藻、海冰硅藻、放射虫和毛颚动物是垂直碳通量至200米深度的关键组成部分。相比之下,仅群居角毛藻对于到达海底的有机碳量至关重要。群落组成的时空变化表明,在暖异常期间硅藻丰度下降,这将降低硅藻驱动的生物碳泵的效率。有趣的是,几种寄生虫也与碳通量紧密相关,并表现出很强的垂直连通性,这表明它们在涉及宿主的沉降过程中可能发挥作用,特别是通过与休眠孢子的相互作用,这可能对浮游-底栖耦合和整体生态系统功能产生影响。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/d42e/11747630/1d3556e5e102/41467_2024_55221_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/d42e/11747630/c4d2521ff766/41467_2024_55221_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/d42e/11747630/271598e0f6ad/41467_2024_55221_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/d42e/11747630/2abd8aee8bfa/41467_2024_55221_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/d42e/11747630/10e0fe837844/41467_2024_55221_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/d42e/11747630/1d3556e5e102/41467_2024_55221_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/d42e/11747630/c4d2521ff766/41467_2024_55221_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/d42e/11747630/271598e0f6ad/41467_2024_55221_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/d42e/11747630/2abd8aee8bfa/41467_2024_55221_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/d42e/11747630/10e0fe837844/41467_2024_55221_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/d42e/11747630/1d3556e5e102/41467_2024_55221_Fig5_HTML.jpg

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本文引用的文献

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ISME Commun. 2024 Jan 23;4(1):ycae014. doi: 10.1093/ismeco/ycae014. eCollection 2024 Jan.
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The polar night shift: seasonal dynamics and drivers of Arctic Ocean microbiomes revealed by autonomous sampling.极夜轮班:通过自主采样揭示北冰洋微生物群落的季节动态和驱动因素
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Fungal parasitism on diatoms alters formation and bio-physical properties of sinking aggregates.
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Sea ice presence is linked to higher carbon export and vertical microbial connectivity in the Eurasian Arctic Ocean.海冰的存在与欧亚北极海洋更高的碳输出和垂直微生物连通性有关。
Commun Biol. 2021 Nov 3;4(1):1255. doi: 10.1038/s42003-021-02776-w.
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