Changes in Organic Carbon Delivery to the Yangtze River Delta Over the Last 2000 Years

Natural processes and anthropogenic activities are vital in dictating the amount and character of organic carbon (OC) input into large river deltas and adjacent shelves. Previous studies have indicated that sediment from the Huanghe River (HR) has significantly affected the formation of the northern...

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Main Authors: Liang Zhou, Yang Yang, Yong Shi, Xiaomei Xu, Ya Ping Wang, Jianjun Jia, Jian Hua Gao, Shu Gao
Format: Article
Language:English
Published: Frontiers Media S.A. 2022-05-01
Series:Frontiers in Marine Science
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/fmars.2022.867820/full
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author Liang Zhou
Liang Zhou
Yang Yang
Yong Shi
Xiaomei Xu
Ya Ping Wang
Jianjun Jia
Jian Hua Gao
Shu Gao
author_facet Liang Zhou
Liang Zhou
Yang Yang
Yong Shi
Xiaomei Xu
Ya Ping Wang
Jianjun Jia
Jian Hua Gao
Shu Gao
author_sort Liang Zhou
collection DOAJ
description Natural processes and anthropogenic activities are vital in dictating the amount and character of organic carbon (OC) input into large river deltas and adjacent shelves. Previous studies have indicated that sediment from the Huanghe River (HR) has significantly affected the formation of the northern Yangtze River subaqueous delta (YRD) over the past several hundred years. However, whether this process has changed sedimentary OC burial in the YRD remains unclear. A sediment core was collected from the YRD in 2018 CE for optically stimulated luminescence and 210Pb dating as well as grain size, total OC, total nitrogen, and stable-isotope analyses to investigate temporal changes in sedimentary OC over the past 2000 years. The results indicate that changes in terrestrial OC inputs to the YRD have been controlled mainly by the East Asian summer monsoon and anthropogenic influences in the past 2000 years. However, the decreased terrestrial OC inputs after 1385 CE, have been significantly affected by increased contribution of HR sediment to the YRD when the HR lower courses shifted to enter the southern Yellow Sea. This study demonstrates that sediment source changes should not be neglected in analyses of mechanisms and variations in OC burial in estuarine and coastal areas.
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spelling doaj.art-de57fee7f3c54e099ea8d448c3a44ae22022-12-22T00:40:40ZengFrontiers Media S.A.Frontiers in Marine Science2296-77452022-05-01910.3389/fmars.2022.867820867820Changes in Organic Carbon Delivery to the Yangtze River Delta Over the Last 2000 YearsLiang Zhou0Liang Zhou1Yang Yang2Yong Shi3Xiaomei Xu4Ya Ping Wang5Jianjun Jia6Jian Hua Gao7Shu Gao8School of Geography, Geomatics, and Planning, Jiangsu Normal University, Xuzhou, ChinaHainan Key Laboratory of Marine Geological Resources and Environment, Hainan Marine Geological Survey Bureau, Haikou, ChinaSchool of Marine Science and Engineering, Nanjing Normal University, Nanjing, ChinaMinistry of Education Key Laboratory for Coast and Island Development, Nanjing University, Nanjing, ChinaMinistry of Education Key Laboratory for Coast and Island Development, Nanjing University, Nanjing, ChinaState Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai, ChinaState Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai, ChinaMinistry of Education Key Laboratory for Coast and Island Development, Nanjing University, Nanjing, ChinaMinistry of Education Key Laboratory for Coast and Island Development, Nanjing University, Nanjing, ChinaNatural processes and anthropogenic activities are vital in dictating the amount and character of organic carbon (OC) input into large river deltas and adjacent shelves. Previous studies have indicated that sediment from the Huanghe River (HR) has significantly affected the formation of the northern Yangtze River subaqueous delta (YRD) over the past several hundred years. However, whether this process has changed sedimentary OC burial in the YRD remains unclear. A sediment core was collected from the YRD in 2018 CE for optically stimulated luminescence and 210Pb dating as well as grain size, total OC, total nitrogen, and stable-isotope analyses to investigate temporal changes in sedimentary OC over the past 2000 years. The results indicate that changes in terrestrial OC inputs to the YRD have been controlled mainly by the East Asian summer monsoon and anthropogenic influences in the past 2000 years. However, the decreased terrestrial OC inputs after 1385 CE, have been significantly affected by increased contribution of HR sediment to the YRD when the HR lower courses shifted to enter the southern Yellow Sea. This study demonstrates that sediment source changes should not be neglected in analyses of mechanisms and variations in OC burial in estuarine and coastal areas.https://www.frontiersin.org/articles/10.3389/fmars.2022.867820/fullsedimentary organic carbonsediment sourceOC burialHuanghe River sedimentYangtze River Delta
spellingShingle Liang Zhou
Liang Zhou
Yang Yang
Yong Shi
Xiaomei Xu
Ya Ping Wang
Jianjun Jia
Jian Hua Gao
Shu Gao
Changes in Organic Carbon Delivery to the Yangtze River Delta Over the Last 2000 Years
Frontiers in Marine Science
sedimentary organic carbon
sediment source
OC burial
Huanghe River sediment
Yangtze River Delta
title Changes in Organic Carbon Delivery to the Yangtze River Delta Over the Last 2000 Years
title_full Changes in Organic Carbon Delivery to the Yangtze River Delta Over the Last 2000 Years
title_fullStr Changes in Organic Carbon Delivery to the Yangtze River Delta Over the Last 2000 Years
title_full_unstemmed Changes in Organic Carbon Delivery to the Yangtze River Delta Over the Last 2000 Years
title_short Changes in Organic Carbon Delivery to the Yangtze River Delta Over the Last 2000 Years
title_sort changes in organic carbon delivery to the yangtze river delta over the last 2000 years
topic sedimentary organic carbon
sediment source
OC burial
Huanghe River sediment
Yangtze River Delta
url https://www.frontiersin.org/articles/10.3389/fmars.2022.867820/full
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