Carbonate compensation depth drives abyssal biogeography in the northeast Pacific.
Carbonate compensation depth drives abyssal biogeography in the northeast Pacific.
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DOI:
10.1038/s41559-023-02122-9
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发表时间:
2023-09
影响因子:
16.8
通讯作者:
中科院分区:
文献类型:
--
作者:
Abyssal seafloor communities cover more than 60% of Earth’s surface. Despite their great size, abyssal plains extend across modest environmental gradients compared to other marine ecosystems. However, little is known about the patterns and processes regulating biodiversity or potentially delimiting biogeographical boundaries at regional scales in the abyss. Improved macroecological understanding of remote abyssal environments is urgent as threats of widespread anthropogenic disturbance grow in the deep ocean. Here, we use a new, basin-scale dataset to show the existence of clear regional zonation in abyssal communities across the 5,000 km span of the Clarion–Clipperton Zone (northeast Pacific), an area targeted for deep-sea mining. We found two pronounced biogeographic provinces, deep and shallow-abyssal, separated by a transition zone between 4,300 and 4,800 m depth. Surprisingly, species richness was maintained across this boundary by phylum-level taxonomic replacements. These regional transitions are probably related to calcium carbonate saturation boundaries as taxa dependent on calcium carbonate structures, such as shelled molluscs, appear restricted to the shallower province. Our results suggest geochemical and climatic forcing on distributions of abyssal populations over large spatial scales and provide a potential paradigm for deep-sea macroecology, opening a new basis for regional-scale biodiversity research and conservation strategies in Earth’s largest biome. Analysing seabed imagery data spanning 5,000 km and >50,000 megafaunal specimens across the Clarion–Clipperton Zone abyssal plain in the northeast Pacific, the authors identify two distinct biogeographical provinces in which taxa that are dependent on calcium carbonate structures are restricted to depths above 4,300–4,880 m.
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影响因子:
1.3
作者:
Amon DJ;Ziegler AF;Drazen JC;Grischenko AV;Leitner AB;Lindsay DJ;Voight JR;Wicksten MK;Young CM;Smith CR
通讯作者:
Smith CR
影响因子:
1.3
作者:
Bribiesca-Contreras G;Dahlgren TG;Amon DJ;Cairns S;Drennan R;Durden JM;Eléaume MP;Hosie AM;Kremenetskaia A;McQuaid K;O'Hara TD;Rabone M;Simon-Lledó E;Smith CR;Watling L;Wiklund H;Glover AG
通讯作者:
Glover AG
影响因子:
2.9
作者:
Harris, P. T.;Macmillan-Lawler, M.;Baker, E. K.
通讯作者:
Baker, E. K.
DOI:
10.1029/jc081i015p02617
发表时间:
1976-01-01
期刊:
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS AND ATMOSPHERES
影响因子:
--
作者:
BERGER, WH;ADELSECK, CG;MAYER, LA
通讯作者:
MAYER, LA
影响因子:
4.6
作者:
Aleynik D;Inall ME;Dale A;Vink A
通讯作者:
Vink A