Accumulation of organic carbon in the Laptev Sea

Fuente: PANGAEA
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Autores principales: Stein, Ruediger, Fahl, Kirsten
Formato: Dataset Open Access
Lenguaje:en
Publicado: PANGAEA 2000
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author Stein, Ruediger
Fahl, Kirsten
author_facet Stein, Ruediger
Fahl, Kirsten
collection Datos científicos de ciencias marinas y ambientales
contents Composition and accumulation rates of organic carbon in Holocene sediments provided data to calculate an organic carbon budget for the Laptev Sea continental margin. Mean Holocene accumulation rates in the inner Laptev Sea vary between 0.14 and 2.7 g C cm**2/ky; maximum values occur close to the Lena River delta. Seawards, the mean accumulation rates decrease from 0.43 to 0.02 g C cm**2/ky. The organic matter is predominantly of terrigenous origin. About 0.9*10**6 t/year of organic carbon are buried in the Laptev Sea, and 0.25*10**6 t/year on the continental slope. Between about 8.5 and 9 ka, major changes in supply of terrigenous and marine organic carbon occur, related to changes in coastal erosion, Siberian river discharge, and/or Atlantic water inflow along the Eurasian continental margin.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_711774
institution PANGAEA
language en
publishDate 2000
publisher PANGAEA
record_format pangaea
spellingShingle Accumulation of organic carbon in the Laptev Sea
Stein, Ruediger
Fahl, Kirsten
Amundsen Basin; Arctic Ocean; ARK-IX/4; ARK-VIII/2; ARK-VIII/3; ARK-XI/1; AWI_Paleo; Barents Sea; BC; Box corer; C-11; C-37; C-4; C-7; C-8; Gakkel Ridge, Arctic Ocean; Giant box corer; GKG; Gravity corer (Kiel type); Gravity corer (Russian type); KAL; KAL_R; Kara Sea/St. Anna Trough; Kasten corer; Kasten corer RUS; Laptev Sea; MUC; MultiCorer; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; PL-1994; PL94-07; PL94-08; PL94-60; PL94-64; PL94-67; Polarstern; Professor Logachev; PS19/112; PS19/157; PS19/165; PS19/228; PS19 ARCTIC91; PS19 EPOS II; PS2138-1; PS2163-1; PS2170-4; PS2206-4; PS2445-4; PS2446-4; PS2447-4; PS2458-4; PS2471-4; PS2474-3; PS2476-4; PS2485-2; PS27; PS27/019; PS27/020; PS27/024; PS27/038; PS27/054; PS27/059; PS27/062; PS27/072; PS2725-5; PS2741-1; PS2742-5; PS2757-8; PS2761-10; PS2763-7; PS2778-2; PS2782-1; PS36; PS36/009; PS36/028; PS36/030; PS36/052; PS36/057; PS36/060; PS36/082; PS36/086; Quaternary Environment of the Eurasian North; QUEEN; RGC; Siberian River Run-Off; SIRRO; SL; Svalbard; Vilkitsky Strait
Composition and accumulation rates of organic carbon in Holocene sediments provided data to calculate an organic carbon budget for the Laptev Sea continental margin. Mean Holocene accumulation rates in the inner Laptev Sea vary between 0.14 and 2.7 g C cm**2/ky; maximum values occur close to the Lena River delta. Seawards, the mean accumulation rates decrease from 0.43 to 0.02 g C cm**2/ky. The organic matter is predominantly of terrigenous origin. About 0.9*10**6 t/year of organic carbon are buried in the Laptev Sea, and 0.25*10**6 t/year on the continental slope. Between about 8.5 and 9 ka, major changes in supply of terrigenous and marine organic carbon occur, related to changes in coastal erosion, Siberian river discharge, and/or Atlantic water inflow along the Eurasian continental margin.
title Accumulation of organic carbon in the Laptev Sea
topic Amundsen Basin; Arctic Ocean; ARK-IX/4; ARK-VIII/2; ARK-VIII/3; ARK-XI/1; AWI_Paleo; Barents Sea; BC; Box corer; C-11; C-37; C-4; C-7; C-8; Gakkel Ridge, Arctic Ocean; Giant box corer; GKG; Gravity corer (Kiel type); Gravity corer (Russian type); KAL; KAL_R; Kara Sea/St. Anna Trough; Kasten corer; Kasten corer RUS; Laptev Sea; MUC; MultiCorer; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; PL-1994; PL94-07; PL94-08; PL94-60; PL94-64; PL94-67; Polarstern; Professor Logachev; PS19/112; PS19/157; PS19/165; PS19/228; PS19 ARCTIC91; PS19 EPOS II; PS2138-1; PS2163-1; PS2170-4; PS2206-4; PS2445-4; PS2446-4; PS2447-4; PS2458-4; PS2471-4; PS2474-3; PS2476-4; PS2485-2; PS27; PS27/019; PS27/020; PS27/024; PS27/038; PS27/054; PS27/059; PS27/062; PS27/072; PS2725-5; PS2741-1; PS2742-5; PS2757-8; PS2761-10; PS2763-7; PS2778-2; PS2782-1; PS36; PS36/009; PS36/028; PS36/030; PS36/052; PS36/057; PS36/060; PS36/082; PS36/086; Quaternary Environment of the Eurasian North; QUEEN; RGC; Siberian River Run-Off; SIRRO; SL; Svalbard; Vilkitsky Strait
url https://doi.org/10.1594/PANGAEA.711774