Loading…

Aquatic environmental changes and anthropogenic activities reflected by the sedimentary records of the Shima River, Southern China

Reconstructing historical sedimentary records is essential for better understanding the effects of anthropogenic activities on river environments. We used lead-210 to date riverine sediment core from the Shima River in China. We obtained a sedimentary history of 34 years (1982–2015) for core S2, whi...

Full description

Saved in:
Bibliographic Details
Published in:Environmental pollution (1987) 2017-05, Vol.224, p.70-81
Main Authors: Gao, Lei, Wang, Zhuowei, Shan, Jiju, Chen, Jianyao, Tang, Changyuan, Yi, Ming
Format: Article
Language:English
Subjects:
Citations: Items that this one cites
Items that cite this one
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
cited_by cdi_FETCH-LOGICAL-a451t-75cb60f678fec63138c865ddee333c5281a73cc0d8c01ec4c64b3e5aa23b4ab3
cites cdi_FETCH-LOGICAL-a451t-75cb60f678fec63138c865ddee333c5281a73cc0d8c01ec4c64b3e5aa23b4ab3
container_end_page 81
container_issue
container_start_page 70
container_title Environmental pollution (1987)
container_volume 224
creator Gao, Lei
Wang, Zhuowei
Shan, Jiju
Chen, Jianyao
Tang, Changyuan
Yi, Ming
description Reconstructing historical sedimentary records is essential for better understanding the effects of anthropogenic activities on river environments. We used lead-210 to date riverine sediment core from the Shima River in China. We obtained a sedimentary history of 34 years (1982–2015) for core S2, which had a length of 34 cm. The sedimentation rate of 0.304–2.04 cm y−1 was controlled by both flood events and anthropogenic activities. The conservative element content depth profiles remained relatively constant, suggestive of a relatively stable sediment provenance; therefore, the increase in the sedimentation rate over time was mainly the result of domestic and industrial wastewater effluent and the construction of a rubber dam at the middle and lower reach of the Shima River. From 1982 to 2015, the nutrient and trace metal depth profiles could be divided in three periods based on their trends. From 1982 to 1993, the vertical profiles of nutrients (organic carbon, total phosphorus, and total nitrogen) and three trace metals (nickel, zinc, and manganese) were relatively stable; however, the gradual decrease in copper and cadmium was likely associated with a reduction in agricultural chemical application. From 1993 to 2003, a population explosion and rapid industrialization were responsible for an increase in the input of pollutants into the Shima River, which was partly attenuated by water from the Dong River, leading to a gradual increase in nutrient and trace metal contents. Finally, from 2003 to 2015, the Shima River stopped being used as a source of water due to its deteriorating water quality. The relatively lower velocity of the water flow after the recovery of its flow direction and the reconstruction of the rubber dam in 2009 provided advantageous sedimentary conditions, promoting nutrient accumulation and significant trace metal enrichment. [Display omitted] •34-years record of sedimentation was reconstructed in an urbanizing watershed.•Economic transition in the PRD areas was reflected by sedimentary history.•Urbanization and industrialization were prevailing contamination sources.•Significant enrichment of heavy metals was observed during the last two decades.
doi_str_mv 10.1016/j.envpol.2016.12.056
format article
fullrecord <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_1876817424</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><els_id>S0269749116315913</els_id><sourcerecordid>1876817424</sourcerecordid><originalsourceid>FETCH-LOGICAL-a451t-75cb60f678fec63138c865ddee333c5281a73cc0d8c01ec4c64b3e5aa23b4ab3</originalsourceid><addsrcrecordid>eNp9kE9r3DAQxUVpaDZpv0EpOvZQO_pn2bkUwpImhUChyV3I8jjW4pU2kryw13zyTrJpjz0IoZk3b_R-hHzmrOaM64tNDWG_i3Mt8FVzUbNGvyMr3rWy0kqo92TFhL6sWnXJT8lZzhvGmJJSfiCnohOdapRckeerp8UW7yia-RTDFkKxM3WTDY-QqQ0DnjKluIuPEFBnXfF7Xzw2E4wzuAID7Q-0TEAzDP7VIB2w6WIaMo3ja-t-8ltLf_s9pG_0Pi5YS4GuJx_sR3Iy2jnDp7f7nDz8uH5Y31Z3v25-rq_uKqsaXqq2cb1mo267EZyWXHau080wAGAm14iO21Y6x4bOMQ5OOa16CY21QvbK9vKcfD3a7lJ8WiAXs_XZwTzbAHHJBsHpjrdIDqXqKHUp5owxzS7h99PBcGZe4JuNOcI3L_ANFwbh49iXtw1Lv4Xh39Bf2ij4fhQAxtx7SCY7D8EhNsRVzBD9_zf8AdIzmt4</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>1876817424</pqid></control><display><type>article</type><title>Aquatic environmental changes and anthropogenic activities reflected by the sedimentary records of the Shima River, Southern China</title><source>Elsevier</source><creator>Gao, Lei ; Wang, Zhuowei ; Shan, Jiju ; Chen, Jianyao ; Tang, Changyuan ; Yi, Ming</creator><creatorcontrib>Gao, Lei ; Wang, Zhuowei ; Shan, Jiju ; Chen, Jianyao ; Tang, Changyuan ; Yi, Ming</creatorcontrib><description>Reconstructing historical sedimentary records is essential for better understanding the effects of anthropogenic activities on river environments. We used lead-210 to date riverine sediment core from the Shima River in China. We obtained a sedimentary history of 34 years (1982–2015) for core S2, which had a length of 34 cm. The sedimentation rate of 0.304–2.04 cm y−1 was controlled by both flood events and anthropogenic activities. The conservative element content depth profiles remained relatively constant, suggestive of a relatively stable sediment provenance; therefore, the increase in the sedimentation rate over time was mainly the result of domestic and industrial wastewater effluent and the construction of a rubber dam at the middle and lower reach of the Shima River. From 1982 to 2015, the nutrient and trace metal depth profiles could be divided in three periods based on their trends. From 1982 to 1993, the vertical profiles of nutrients (organic carbon, total phosphorus, and total nitrogen) and three trace metals (nickel, zinc, and manganese) were relatively stable; however, the gradual decrease in copper and cadmium was likely associated with a reduction in agricultural chemical application. From 1993 to 2003, a population explosion and rapid industrialization were responsible for an increase in the input of pollutants into the Shima River, which was partly attenuated by water from the Dong River, leading to a gradual increase in nutrient and trace metal contents. Finally, from 2003 to 2015, the Shima River stopped being used as a source of water due to its deteriorating water quality. The relatively lower velocity of the water flow after the recovery of its flow direction and the reconstruction of the rubber dam in 2009 provided advantageous sedimentary conditions, promoting nutrient accumulation and significant trace metal enrichment. [Display omitted] •34-years record of sedimentation was reconstructed in an urbanizing watershed.•Economic transition in the PRD areas was reflected by sedimentary history.•Urbanization and industrialization were prevailing contamination sources.•Significant enrichment of heavy metals was observed during the last two decades.</description><identifier>ISSN: 0269-7491</identifier><identifier>EISSN: 1873-6424</identifier><identifier>DOI: 10.1016/j.envpol.2016.12.056</identifier><identifier>PMID: 28284543</identifier><language>eng</language><publisher>England: Elsevier Ltd</publisher><subject>Agriculture ; Anthropogenic activities ; Cadmium - analysis ; China ; Environmental changes ; Environmental Monitoring ; Geologic Sediments - chemistry ; Historical sedimentary record ; History, 20th Century ; History, 21st Century ; Metal pollution ; Nitrogen - analysis ; Phosphorus - analysis ; Rivers - chemistry ; Shima River ; Time ; Trace Elements ; Water Pollutants, Chemical - analysis ; Water Pollutants, Chemical - history ; Water Quality</subject><ispartof>Environmental pollution (1987), 2017-05, Vol.224, p.70-81</ispartof><rights>2017 Elsevier Ltd</rights><rights>Copyright © 2017 Elsevier Ltd. All rights reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a451t-75cb60f678fec63138c865ddee333c5281a73cc0d8c01ec4c64b3e5aa23b4ab3</citedby><cites>FETCH-LOGICAL-a451t-75cb60f678fec63138c865ddee333c5281a73cc0d8c01ec4c64b3e5aa23b4ab3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,27901,27902</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/28284543$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Gao, Lei</creatorcontrib><creatorcontrib>Wang, Zhuowei</creatorcontrib><creatorcontrib>Shan, Jiju</creatorcontrib><creatorcontrib>Chen, Jianyao</creatorcontrib><creatorcontrib>Tang, Changyuan</creatorcontrib><creatorcontrib>Yi, Ming</creatorcontrib><title>Aquatic environmental changes and anthropogenic activities reflected by the sedimentary records of the Shima River, Southern China</title><title>Environmental pollution (1987)</title><addtitle>Environ Pollut</addtitle><description>Reconstructing historical sedimentary records is essential for better understanding the effects of anthropogenic activities on river environments. We used lead-210 to date riverine sediment core from the Shima River in China. We obtained a sedimentary history of 34 years (1982–2015) for core S2, which had a length of 34 cm. The sedimentation rate of 0.304–2.04 cm y−1 was controlled by both flood events and anthropogenic activities. The conservative element content depth profiles remained relatively constant, suggestive of a relatively stable sediment provenance; therefore, the increase in the sedimentation rate over time was mainly the result of domestic and industrial wastewater effluent and the construction of a rubber dam at the middle and lower reach of the Shima River. From 1982 to 2015, the nutrient and trace metal depth profiles could be divided in three periods based on their trends. From 1982 to 1993, the vertical profiles of nutrients (organic carbon, total phosphorus, and total nitrogen) and three trace metals (nickel, zinc, and manganese) were relatively stable; however, the gradual decrease in copper and cadmium was likely associated with a reduction in agricultural chemical application. From 1993 to 2003, a population explosion and rapid industrialization were responsible for an increase in the input of pollutants into the Shima River, which was partly attenuated by water from the Dong River, leading to a gradual increase in nutrient and trace metal contents. Finally, from 2003 to 2015, the Shima River stopped being used as a source of water due to its deteriorating water quality. The relatively lower velocity of the water flow after the recovery of its flow direction and the reconstruction of the rubber dam in 2009 provided advantageous sedimentary conditions, promoting nutrient accumulation and significant trace metal enrichment. [Display omitted] •34-years record of sedimentation was reconstructed in an urbanizing watershed.•Economic transition in the PRD areas was reflected by sedimentary history.•Urbanization and industrialization were prevailing contamination sources.•Significant enrichment of heavy metals was observed during the last two decades.</description><subject>Agriculture</subject><subject>Anthropogenic activities</subject><subject>Cadmium - analysis</subject><subject>China</subject><subject>Environmental changes</subject><subject>Environmental Monitoring</subject><subject>Geologic Sediments - chemistry</subject><subject>Historical sedimentary record</subject><subject>History, 20th Century</subject><subject>History, 21st Century</subject><subject>Metal pollution</subject><subject>Nitrogen - analysis</subject><subject>Phosphorus - analysis</subject><subject>Rivers - chemistry</subject><subject>Shima River</subject><subject>Time</subject><subject>Trace Elements</subject><subject>Water Pollutants, Chemical - analysis</subject><subject>Water Pollutants, Chemical - history</subject><subject>Water Quality</subject><issn>0269-7491</issn><issn>1873-6424</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><recordid>eNp9kE9r3DAQxUVpaDZpv0EpOvZQO_pn2bkUwpImhUChyV3I8jjW4pU2kryw13zyTrJpjz0IoZk3b_R-hHzmrOaM64tNDWG_i3Mt8FVzUbNGvyMr3rWy0kqo92TFhL6sWnXJT8lZzhvGmJJSfiCnohOdapRckeerp8UW7yia-RTDFkKxM3WTDY-QqQ0DnjKluIuPEFBnXfF7Xzw2E4wzuAID7Q-0TEAzDP7VIB2w6WIaMo3ja-t-8ltLf_s9pG_0Pi5YS4GuJx_sR3Iy2jnDp7f7nDz8uH5Y31Z3v25-rq_uKqsaXqq2cb1mo267EZyWXHau080wAGAm14iO21Y6x4bOMQ5OOa16CY21QvbK9vKcfD3a7lJ8WiAXs_XZwTzbAHHJBsHpjrdIDqXqKHUp5owxzS7h99PBcGZe4JuNOcI3L_ANFwbh49iXtw1Lv4Xh39Bf2ij4fhQAxtx7SCY7D8EhNsRVzBD9_zf8AdIzmt4</recordid><startdate>20170501</startdate><enddate>20170501</enddate><creator>Gao, Lei</creator><creator>Wang, Zhuowei</creator><creator>Shan, Jiju</creator><creator>Chen, Jianyao</creator><creator>Tang, Changyuan</creator><creator>Yi, Ming</creator><general>Elsevier Ltd</general><scope>CGR</scope><scope>CUY</scope><scope>CVF</scope><scope>ECM</scope><scope>EIF</scope><scope>NPM</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7X8</scope></search><sort><creationdate>20170501</creationdate><title>Aquatic environmental changes and anthropogenic activities reflected by the sedimentary records of the Shima River, Southern China</title><author>Gao, Lei ; Wang, Zhuowei ; Shan, Jiju ; Chen, Jianyao ; Tang, Changyuan ; Yi, Ming</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a451t-75cb60f678fec63138c865ddee333c5281a73cc0d8c01ec4c64b3e5aa23b4ab3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2017</creationdate><topic>Agriculture</topic><topic>Anthropogenic activities</topic><topic>Cadmium - analysis</topic><topic>China</topic><topic>Environmental changes</topic><topic>Environmental Monitoring</topic><topic>Geologic Sediments - chemistry</topic><topic>Historical sedimentary record</topic><topic>History, 20th Century</topic><topic>History, 21st Century</topic><topic>Metal pollution</topic><topic>Nitrogen - analysis</topic><topic>Phosphorus - analysis</topic><topic>Rivers - chemistry</topic><topic>Shima River</topic><topic>Time</topic><topic>Trace Elements</topic><topic>Water Pollutants, Chemical - analysis</topic><topic>Water Pollutants, Chemical - history</topic><topic>Water Quality</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Gao, Lei</creatorcontrib><creatorcontrib>Wang, Zhuowei</creatorcontrib><creatorcontrib>Shan, Jiju</creatorcontrib><creatorcontrib>Chen, Jianyao</creatorcontrib><creatorcontrib>Tang, Changyuan</creatorcontrib><creatorcontrib>Yi, Ming</creatorcontrib><collection>Medline</collection><collection>MEDLINE</collection><collection>MEDLINE (Ovid)</collection><collection>MEDLINE</collection><collection>MEDLINE</collection><collection>PubMed</collection><collection>CrossRef</collection><collection>MEDLINE - Academic</collection><jtitle>Environmental pollution (1987)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Gao, Lei</au><au>Wang, Zhuowei</au><au>Shan, Jiju</au><au>Chen, Jianyao</au><au>Tang, Changyuan</au><au>Yi, Ming</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Aquatic environmental changes and anthropogenic activities reflected by the sedimentary records of the Shima River, Southern China</atitle><jtitle>Environmental pollution (1987)</jtitle><addtitle>Environ Pollut</addtitle><date>2017-05-01</date><risdate>2017</risdate><volume>224</volume><spage>70</spage><epage>81</epage><pages>70-81</pages><issn>0269-7491</issn><eissn>1873-6424</eissn><abstract>Reconstructing historical sedimentary records is essential for better understanding the effects of anthropogenic activities on river environments. We used lead-210 to date riverine sediment core from the Shima River in China. We obtained a sedimentary history of 34 years (1982–2015) for core S2, which had a length of 34 cm. The sedimentation rate of 0.304–2.04 cm y−1 was controlled by both flood events and anthropogenic activities. The conservative element content depth profiles remained relatively constant, suggestive of a relatively stable sediment provenance; therefore, the increase in the sedimentation rate over time was mainly the result of domestic and industrial wastewater effluent and the construction of a rubber dam at the middle and lower reach of the Shima River. From 1982 to 2015, the nutrient and trace metal depth profiles could be divided in three periods based on their trends. From 1982 to 1993, the vertical profiles of nutrients (organic carbon, total phosphorus, and total nitrogen) and three trace metals (nickel, zinc, and manganese) were relatively stable; however, the gradual decrease in copper and cadmium was likely associated with a reduction in agricultural chemical application. From 1993 to 2003, a population explosion and rapid industrialization were responsible for an increase in the input of pollutants into the Shima River, which was partly attenuated by water from the Dong River, leading to a gradual increase in nutrient and trace metal contents. Finally, from 2003 to 2015, the Shima River stopped being used as a source of water due to its deteriorating water quality. The relatively lower velocity of the water flow after the recovery of its flow direction and the reconstruction of the rubber dam in 2009 provided advantageous sedimentary conditions, promoting nutrient accumulation and significant trace metal enrichment. [Display omitted] •34-years record of sedimentation was reconstructed in an urbanizing watershed.•Economic transition in the PRD areas was reflected by sedimentary history.•Urbanization and industrialization were prevailing contamination sources.•Significant enrichment of heavy metals was observed during the last two decades.</abstract><cop>England</cop><pub>Elsevier Ltd</pub><pmid>28284543</pmid><doi>10.1016/j.envpol.2016.12.056</doi><tpages>12</tpages></addata></record>
fulltext fulltext
identifier ISSN: 0269-7491
ispartof Environmental pollution (1987), 2017-05, Vol.224, p.70-81
issn 0269-7491
1873-6424
language eng
recordid cdi_proquest_miscellaneous_1876817424
source Elsevier
subjects Agriculture
Anthropogenic activities
Cadmium - analysis
China
Environmental changes
Environmental Monitoring
Geologic Sediments - chemistry
Historical sedimentary record
History, 20th Century
History, 21st Century
Metal pollution
Nitrogen - analysis
Phosphorus - analysis
Rivers - chemistry
Shima River
Time
Trace Elements
Water Pollutants, Chemical - analysis
Water Pollutants, Chemical - history
Water Quality
title Aquatic environmental changes and anthropogenic activities reflected by the sedimentary records of the Shima River, Southern China
url http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-02-06T12%3A42%3A58IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Aquatic%20environmental%20changes%20and%20anthropogenic%20activities%20reflected%20by%20the%20sedimentary%20records%20of%20the%20Shima%20River,%20Southern%20China&rft.jtitle=Environmental%20pollution%20(1987)&rft.au=Gao,%20Lei&rft.date=2017-05-01&rft.volume=224&rft.spage=70&rft.epage=81&rft.pages=70-81&rft.issn=0269-7491&rft.eissn=1873-6424&rft_id=info:doi/10.1016/j.envpol.2016.12.056&rft_dat=%3Cproquest_cross%3E1876817424%3C/proquest_cross%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-a451t-75cb60f678fec63138c865ddee333c5281a73cc0d8c01ec4c64b3e5aa23b4ab3%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_pqid=1876817424&rft_id=info:pmid/28284543&rfr_iscdi=true