A. Lein, M. Kravchishina, G. A. Pavlova, A. Chultsova, A. Novigatsky, A. Klyuvitkin, A. Savvichev
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引用次数: 0
Abstract
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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