巴伦支海现代孔隙水盐组成及生物成因元素分析(1997-2019)

THE BARENTS SEA SYSTEM Pub Date : 2021-09-09 DOI:10.29006/978-5-6045110-0-8/(28)

A. Lein, M. Kravchishina, G. A. Pavlova, A. Chultsova, A. Novigatsky, A. Klyuvitkin, A. Savvichev

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摘要

本文讨论了21世纪北极地区与北冰洋“大西洋化”有关的最大变暖时期巴伦支海和挪威海孔隙水盐组成、悬浮颗粒物、蓬松层和表层(0-30 cm)的同位素有机碳组成(Cl-、SO42-、Ca2+ Alk和生物源元素)。

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Salt composition and biogenic elements in modern pore waters of the Barents Sea (1997–2019)

The data (Cl-, SO42-, Ca2+ Alk and biogenic elements) on the salt composition of pore water and the isotopic organic carbon composition of suspended particulate matter, fluffy layer and surface layers (0–30 cm) of bottom sediments in the Barents and Norwegian seas are discussed during the period of the supposed maximum warming in the Arctic region in the 21st century associated with the “atlantification” of the Arctic Ocean.

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THE BARENTS SEA SYSTEM

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