Sediment properties and geochemical proxies of gravity cores obtained on the continental slope and rise at the eastern side of Hillary Canyon in the Ross Sea since Last Glacial Maximum

For the reconstruction of paleoenvironment, 14C ages, magnetic susceptibility, number of gravel, granulometry, biogenic opal, total organic carbon, d13C, total nitrogen, d15N, total organic carbon-total nitrogen ratio, CaCO3 were measured. Druing the PNRA-Rosslope II Expedition 2014, gravity cores(R...

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Bibliographic Details
Main Authors: Ha, Sangbeom, Colizza, E, Torricella, Fiorenza, Langone, Leonardo, Giglio, Federico, Kuhn, Gerhard, Macrì, Patrizia, Khim, Boo-Keun
Format: Dataset
Language:English
Published: PANGAEA 2022
Subjects:
Continental Margin
Ice Sheet
paleoproductivity
Ross Sea
Sea ice
sediment core
Hillary Canyon
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.943782
https://doi.org/10.1594/PANGAEA.943782
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Summary:For the reconstruction of paleoenvironment, 14C ages, magnetic susceptibility, number of gravel, granulometry, biogenic opal, total organic carbon, d13C, total nitrogen, d15N, total organic carbon-total nitrogen ratio, CaCO3 were measured. Druing the PNRA-Rosslope II Expedition 2014, gravity cores(RS14-GC1, GC2, and GC3) on the continental slope and rise at the eastern side of Hillary Canyon in the Ross Sea since Last Glacial Maximum.

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