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- W4308149819 abstract "Abstract Based on the analysis of fish otolith assemblages from surface sediments of the Lomonosov Ridge (Arctic Ocean), we demonstrate that the very low Holocene sedimentation rates and winnowing of fine sediments result in the mixing of the whole Holocene populations at the sediment surface. Specimens from the Marine Isotope Stage (MIS) 3 or older could even be recovered in the surface due to a sedimentary hiatus at some locations in the central Arctic during the last glacial maximum. Two examples illustrate that 14 C‐stratigraphies from planktic foraminifers in underlying cored sediments reflect the mixing between Holocene and MIS 3 or older populations, thus invalidating continuous age‐depth inferences based on 14 C ages. Hence, much caution is required when attempting to set paleoceanographic reconstructions based on 14 C chronologies in a low sediment accumulation rate environment such as the central Arctic Ocean. Already published paleoceanographic reconstructions from this area might thus require some revisions." @default.
- W4308149819 created "2022-11-08" @default.
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- W4308149819 date "2022-11-02" @default.
- W4308149819 modified "2023-10-14" @default.
- W4308149819 title "Challenging Radiocarbon Chronostratigraphies in Central Arctic Ocean Sediment" @default.
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- W4308149819 doi "https://doi.org/10.1029/2022gl100446" @default.
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