Distribution of 14 C and 13 C in Forest Soils of the Dinghushan Biosphere Reserve

Distribution of 14 C and 13 C in Forest Soils of the Dinghushan Biosphere Reserve

We report here first results on the bulk soil organic carbon (SOC), apparent radiocarbon ages and δ 13 C characteristics of the tropical and subtropical forest soil in Dinghushan Biosphere Reserve (DHSBR). The forest oxisol in Dinghushan has developed during the Holocene. The δ 13 C variation curves...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Radiocarbon 2001, Vol.43 (2B), p.671-678
Hauptverfasser: Shen, Chengde, Yi, Weixi, Sun, Yanmin, Xing, Changping, Yang, Ying, Yuan, Chao, Li, Zhian, Peng, Shaolin, An, Zhisheng, Liu, Tungsheng
Format: Artikel
Sprache:eng
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page 678
container_issue 2B
container_start_page 671
container_title Radiocarbon
container_volume 43
creator Shen, Chengde
Yi, Weixi
Sun, Yanmin
Xing, Changping
Yang, Ying
Yuan, Chao
Li, Zhian
Peng, Shaolin
An, Zhisheng
Liu, Tungsheng
description We report here first results on the bulk soil organic carbon (SOC), apparent radiocarbon ages and δ 13 C characteristics of the tropical and subtropical forest soil in Dinghushan Biosphere Reserve (DHSBR). The forest oxisol in Dinghushan has developed during the Holocene. The δ 13 C variation curves in all three profiles may be divided into two sections. The upper section from 0 to 40 cm has δ 13 C values varying from −27.4 to −24.1‰, −27.5 to −22.2‰, and −24.4 to −20.1‰. in the Wukesong, Qingyunsi and Kengkou profiles, respectively. The lower section, including the 40–160 cm horizons, has a uniform δ 13 C. The mean δ 13 C values of the soil organic carbon could be used not only to discriminate between C 3 and C 4 plants, but also to distinguish between coniferous and broad-leaf plants.
doi_str_mv 10.1017/S0033822200041321
format Article
fullrecord <record><control><sourceid>crossref</sourceid><recordid>TN_cdi_crossref_primary_10_1017_S0033822200041321</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>10_1017_S0033822200041321</sourcerecordid><originalsourceid>FETCH-LOGICAL-c901-3eb09bc981c70a1911aab63379396d22cdbc2080c59a30057b1d772c29d3809c3</originalsourceid><addsrcrecordid>eNplkMFKxDAURYMoWEc_wF1-oPpeXtM0S-04ozAgOrMvaZrayNgMSUfw77XoztW9cC53cRi7RrhBQHW7BSCqhBAAUCAJPGEZ6kLmUkl5yrIZ5zM_ZxcpvQMILCuVsZelT1P07XHyYeSh51jwmpux40g_xY98FaJLE98Gv0_zYBocX_rxbTimwYz83od0GFx0_NUlFz_dJTvrzT65q79csN3qYVc_5pvn9VN9t8mtBszJtaBbqyu0CgxqRGPakkhp0mUnhO1aK6ACK7UhAKla7JQSVuiOKtCWFgx_b20MKUXXN4foP0z8ahCaWUnzTwl9AzwAUQw</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype></control><display><type>article</type><title>Distribution of 14 C and 13 C in Forest Soils of the Dinghushan Biosphere Reserve</title><source>Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals</source><source>Free Full-Text Journals in Chemistry</source><source>Cambridge University Press Journals Complete</source><creator>Shen, Chengde ; Yi, Weixi ; Sun, Yanmin ; Xing, Changping ; Yang, Ying ; Yuan, Chao ; Li, Zhian ; Peng, Shaolin ; An, Zhisheng ; Liu, Tungsheng</creator><creatorcontrib>Shen, Chengde ; Yi, Weixi ; Sun, Yanmin ; Xing, Changping ; Yang, Ying ; Yuan, Chao ; Li, Zhian ; Peng, Shaolin ; An, Zhisheng ; Liu, Tungsheng</creatorcontrib><description>We report here first results on the bulk soil organic carbon (SOC), apparent radiocarbon ages and δ 13 C characteristics of the tropical and subtropical forest soil in Dinghushan Biosphere Reserve (DHSBR). The forest oxisol in Dinghushan has developed during the Holocene. The δ 13 C variation curves in all three profiles may be divided into two sections. The upper section from 0 to 40 cm has δ 13 C values varying from −27.4 to −24.1‰, −27.5 to −22.2‰, and −24.4 to −20.1‰. in the Wukesong, Qingyunsi and Kengkou profiles, respectively. The lower section, including the 40–160 cm horizons, has a uniform δ 13 C. The mean δ 13 C values of the soil organic carbon could be used not only to discriminate between C 3 and C 4 plants, but also to distinguish between coniferous and broad-leaf plants.</description><identifier>ISSN: 0033-8222</identifier><identifier>EISSN: 1945-5755</identifier><identifier>DOI: 10.1017/S0033822200041321</identifier><language>eng</language><ispartof>Radiocarbon, 2001, Vol.43 (2B), p.671-678</ispartof><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c901-3eb09bc981c70a1911aab63379396d22cdbc2080c59a30057b1d772c29d3809c3</citedby><cites>FETCH-LOGICAL-c901-3eb09bc981c70a1911aab63379396d22cdbc2080c59a30057b1d772c29d3809c3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,4024,27923,27924,27925</link.rule.ids></links><search><creatorcontrib>Shen, Chengde</creatorcontrib><creatorcontrib>Yi, Weixi</creatorcontrib><creatorcontrib>Sun, Yanmin</creatorcontrib><creatorcontrib>Xing, Changping</creatorcontrib><creatorcontrib>Yang, Ying</creatorcontrib><creatorcontrib>Yuan, Chao</creatorcontrib><creatorcontrib>Li, Zhian</creatorcontrib><creatorcontrib>Peng, Shaolin</creatorcontrib><creatorcontrib>An, Zhisheng</creatorcontrib><creatorcontrib>Liu, Tungsheng</creatorcontrib><title>Distribution of 14 C and 13 C in Forest Soils of the Dinghushan Biosphere Reserve</title><title>Radiocarbon</title><description>We report here first results on the bulk soil organic carbon (SOC), apparent radiocarbon ages and δ 13 C characteristics of the tropical and subtropical forest soil in Dinghushan Biosphere Reserve (DHSBR). The forest oxisol in Dinghushan has developed during the Holocene. The δ 13 C variation curves in all three profiles may be divided into two sections. The upper section from 0 to 40 cm has δ 13 C values varying from −27.4 to −24.1‰, −27.5 to −22.2‰, and −24.4 to −20.1‰. in the Wukesong, Qingyunsi and Kengkou profiles, respectively. The lower section, including the 40–160 cm horizons, has a uniform δ 13 C. The mean δ 13 C values of the soil organic carbon could be used not only to discriminate between C 3 and C 4 plants, but also to distinguish between coniferous and broad-leaf plants.</description><issn>0033-8222</issn><issn>1945-5755</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2001</creationdate><recordtype>article</recordtype><recordid>eNplkMFKxDAURYMoWEc_wF1-oPpeXtM0S-04ozAgOrMvaZrayNgMSUfw77XoztW9cC53cRi7RrhBQHW7BSCqhBAAUCAJPGEZ6kLmUkl5yrIZ5zM_ZxcpvQMILCuVsZelT1P07XHyYeSh51jwmpux40g_xY98FaJLE98Gv0_zYBocX_rxbTimwYz83od0GFx0_NUlFz_dJTvrzT65q79csN3qYVc_5pvn9VN9t8mtBszJtaBbqyu0CgxqRGPakkhp0mUnhO1aK6ACK7UhAKla7JQSVuiOKtCWFgx_b20MKUXXN4foP0z8ahCaWUnzTwl9AzwAUQw</recordid><startdate>2001</startdate><enddate>2001</enddate><creator>Shen, Chengde</creator><creator>Yi, Weixi</creator><creator>Sun, Yanmin</creator><creator>Xing, Changping</creator><creator>Yang, Ying</creator><creator>Yuan, Chao</creator><creator>Li, Zhian</creator><creator>Peng, Shaolin</creator><creator>An, Zhisheng</creator><creator>Liu, Tungsheng</creator><scope>AAYXX</scope><scope>CITATION</scope></search><sort><creationdate>2001</creationdate><title>Distribution of 14 C and 13 C in Forest Soils of the Dinghushan Biosphere Reserve</title><author>Shen, Chengde ; Yi, Weixi ; Sun, Yanmin ; Xing, Changping ; Yang, Ying ; Yuan, Chao ; Li, Zhian ; Peng, Shaolin ; An, Zhisheng ; Liu, Tungsheng</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c901-3eb09bc981c70a1911aab63379396d22cdbc2080c59a30057b1d772c29d3809c3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2001</creationdate><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Shen, Chengde</creatorcontrib><creatorcontrib>Yi, Weixi</creatorcontrib><creatorcontrib>Sun, Yanmin</creatorcontrib><creatorcontrib>Xing, Changping</creatorcontrib><creatorcontrib>Yang, Ying</creatorcontrib><creatorcontrib>Yuan, Chao</creatorcontrib><creatorcontrib>Li, Zhian</creatorcontrib><creatorcontrib>Peng, Shaolin</creatorcontrib><creatorcontrib>An, Zhisheng</creatorcontrib><creatorcontrib>Liu, Tungsheng</creatorcontrib><collection>CrossRef</collection><jtitle>Radiocarbon</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Shen, Chengde</au><au>Yi, Weixi</au><au>Sun, Yanmin</au><au>Xing, Changping</au><au>Yang, Ying</au><au>Yuan, Chao</au><au>Li, Zhian</au><au>Peng, Shaolin</au><au>An, Zhisheng</au><au>Liu, Tungsheng</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Distribution of 14 C and 13 C in Forest Soils of the Dinghushan Biosphere Reserve</atitle><jtitle>Radiocarbon</jtitle><date>2001</date><risdate>2001</risdate><volume>43</volume><issue>2B</issue><spage>671</spage><epage>678</epage><pages>671-678</pages><issn>0033-8222</issn><eissn>1945-5755</eissn><abstract>We report here first results on the bulk soil organic carbon (SOC), apparent radiocarbon ages and δ 13 C characteristics of the tropical and subtropical forest soil in Dinghushan Biosphere Reserve (DHSBR). The forest oxisol in Dinghushan has developed during the Holocene. The δ 13 C variation curves in all three profiles may be divided into two sections. The upper section from 0 to 40 cm has δ 13 C values varying from −27.4 to −24.1‰, −27.5 to −22.2‰, and −24.4 to −20.1‰. in the Wukesong, Qingyunsi and Kengkou profiles, respectively. The lower section, including the 40–160 cm horizons, has a uniform δ 13 C. The mean δ 13 C values of the soil organic carbon could be used not only to discriminate between C 3 and C 4 plants, but also to distinguish between coniferous and broad-leaf plants.</abstract><doi>10.1017/S0033822200041321</doi><tpages>8</tpages></addata></record>
fulltext fulltext
identifier ISSN: 0033-8222
ispartof Radiocarbon, 2001, Vol.43 (2B), p.671-678
issn 0033-8222
1945-5755
language eng
recordid cdi_crossref_primary_10_1017_S0033822200041321
source Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals; Free Full-Text Journals in Chemistry; Cambridge University Press Journals Complete
title Distribution of 14 C and 13 C in Forest Soils of the Dinghushan Biosphere Reserve
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-08T04%3A27%3A26IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-crossref&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Distribution%20of%2014%20C%20and%2013%20C%20in%20Forest%20Soils%20of%20the%20Dinghushan%20Biosphere%20Reserve&rft.jtitle=Radiocarbon&rft.au=Shen,%20Chengde&rft.date=2001&rft.volume=43&rft.issue=2B&rft.spage=671&rft.epage=678&rft.pages=671-678&rft.issn=0033-8222&rft.eissn=1945-5755&rft_id=info:doi/10.1017/S0033822200041321&rft_dat=%3Ccrossref%3E10_1017_S0033822200041321%3C/crossref%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_id=info:pmid/&rfr_iscdi=true