ISSN Approved Journal No: 2250-1770 | Impact factor: 8.17 | ESTD Year: 2011
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Paper Title: DOWNCORE VARIATION OF ORGANIC CARBON IN MARINE SEDIMENT CORE FROM OFF MAHARASHTRA, EASTERN ARABIAN SEA
Author Name(s): V. Yoganandan
Published Paper ID: - IJCSP21A1001
Register Paper ID - 211838
Publisher Journal Name: IJPUBLICATION, IJCSPUB
DOI Member ID: 10.6084/m9.doi.one.IJCSP21A1001 and DOI : http://doi.one/10.1729/Journal.29296
Author Country : Indian Author, India, - , -, - , | Research Area: Science and Technology Published Paper URL: viewfull.php?&p_id=IJCSP21A1001 Published Paper PDF: download.php?file=IJCSP21A1001 Published Paper PDF: http://www.ijcspub.org/papers/IJCSP21A1001.pdf
Title: DOWNCORE VARIATION OF ORGANIC CARBON IN MARINE SEDIMENT CORE FROM OFF MAHARASHTRA, EASTERN ARABIAN SEA
DOI (Digital Object Identifier) : http://doi.one/10.1729/Journal.29296
Pubished in Volume: 11 | Issue: 1 | Year: January 2021
Publisher Name : IJCSPUB | www.ijcspub.org | ISSN : 2250-1770
Subject Area: Science and Technology
Author type: Indian Author
Pubished in Volume: 11
Issue: 1
Pages: 1-4
Year: January 2021
Downloads: 87
E-ISSN Number: 2320-2882
Organic carbon OC in marine sediments is a critical component of the global carbon cycle, and its degradation influences a wide range of phenomena, including the magnitude of carbon sequestration over geologic timescales, the recycling of inorganic carbon and nutrients, the dissolution and precipitation of carbonates, the production of methane and the nature of the seafloor biosphere. Although much has been learned about the factors that promote and hinder rates of organic carbon degradation in natural systems, the controls on the distribution of organic carbon in modern and ancient sediments are still not fully understood. The result shows that higher OC content (>1.2 to 4.4%) is present in the top 2 m and lower content (<1 to 0.3 %) is present in the rest of the core with minor fluctuation. The low OC content in the early Holocene sediments may be due to the low productivity. High OC content during the late Holocene was due to the higher productivity in the study area.
Licence: creative commons attribution 4.0
Organic Carbon, Eastern Arabian Sea, Paleoproductivity, Marine Sediments.