2018
DOI: 10.1016/j.dsr.2018.08.006
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Natural spatial variability of depositional conditions, biogeochemical processes and element fluxes in sediments of the eastern Clarion-Clipperton Zone, Pacific Ocean

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Cited by 98 publications
(178 citation statements)
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“…To conclude, our study supports the assumptions behind the creation of nine large APEIs, namely that gradients of sea surface primary productivity determine large-scale patterns and that nodule densities determine local-scale patterns in community structure, species composition and functioning (Wedding et al, 2013). However, among exploration contract areas, there is a shift in community composition and trophic structure between BGR, IOM, and GSR on the one hand and Ifremer on the other hand, suggesting that these two groups do not belong to the same subregion, as hypothesized by Wedding et al (2013). Environmental conditions at the APEI no.…”
Section: Major Forces Driving Local-and Regional-scale Patterns In Cosupporting
confidence: 78%
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“…To conclude, our study supports the assumptions behind the creation of nine large APEIs, namely that gradients of sea surface primary productivity determine large-scale patterns and that nodule densities determine local-scale patterns in community structure, species composition and functioning (Wedding et al, 2013). However, among exploration contract areas, there is a shift in community composition and trophic structure between BGR, IOM, and GSR on the one hand and Ifremer on the other hand, suggesting that these two groups do not belong to the same subregion, as hypothesized by Wedding et al (2013). Environmental conditions at the APEI no.…”
Section: Major Forces Driving Local-and Regional-scale Patterns In Cosupporting
confidence: 78%
“…Considering the large environmental footprint of nodule mining disturbances on the seafloor, as well as the diversity and vulnerability of the abyssal fauna, the need for marine spatial planning to preserve species, habitats and functions in the CCFZ has emerged, concomitant to a renewed interest for deep-sea mineral resources (Wedding et al, 2013). Due to the paucity of biological data in the CCFZ, the recommendations issued by Wedding et al (2013) for the design of a network of protected areas were mainly based on nitrogen flux at 100 m depth (a proxy for trophic inputs to the seafloor), modeled nodule densities, the distribution of large seamounts and the dispersal distances of shallow water taxa. One of the main assumptions underlying the management plan is that longitudinal and latitudinal productivity-driven gradients shape the community structure and species distribution of abyssal communities.…”
Section: Introductionmentioning
confidence: 99%
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