Contents and isotopic composition of black carbon from ODP Sites 184-1147 and 184-1148

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Autori principali: Jia, Guodong, Peng, Pingan, Zhao, Quanhong, Jian, Zhimin
Natura: Dataset Open Access
Lingua:en
Pubblicazione: PANGAEA 2003
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author Jia, Guodong
Peng, Pingan
Zhao, Quanhong
Jian, Zhimin
author_facet Jia, Guodong
Peng, Pingan
Zhao, Quanhong
Jian, Zhimin
collection Datos científicos de ciencias marinas y ambientales
contents A 30 m.y. stable isotopic record of marine-deposited black carbon from regional terrestrial biomass burning from the northern South China Sea reveals photosynthetic pathway evolution for terrestrial ecosystems in the late Cenozoic. This record indicates that C3 plants negatively adjusted their isotopic discrimination and C4 plants appeared gradually as a component of land vegetation in East Asia since the early Miocene, a long time before sudden C4 expansion occurred during the late Miocene to the Pliocene. The changes in terrestrial ecosystems with time can be reasonably related to the evolution of East Asian monsoons, which are thought to have been induced by several intricate mechanisms during the late Cenozoic and could contribute significantly to the post-Miocene marine carbonate isotope decline.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_713550
institution PANGAEA
language en
publishDate 2003
publisher PANGAEA
record_format pangaea
spellingShingle Contents and isotopic composition of black carbon from ODP Sites 184-1147 and 184-1148
Jia, Guodong
Peng, Pingan
Zhao, Quanhong
Jian, Zhimin
184-1147A; 184-1147B; 184-1147C; 184-1148A; 184-1148B; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Joides Resolution; Leg184; South China Sea
A 30 m.y. stable isotopic record of marine-deposited black carbon from regional terrestrial biomass burning from the northern South China Sea reveals photosynthetic pathway evolution for terrestrial ecosystems in the late Cenozoic. This record indicates that C3 plants negatively adjusted their isotopic discrimination and C4 plants appeared gradually as a component of land vegetation in East Asia since the early Miocene, a long time before sudden C4 expansion occurred during the late Miocene to the Pliocene. The changes in terrestrial ecosystems with time can be reasonably related to the evolution of East Asian monsoons, which are thought to have been induced by several intricate mechanisms during the late Cenozoic and could contribute significantly to the post-Miocene marine carbonate isotope decline.
title Contents and isotopic composition of black carbon from ODP Sites 184-1147 and 184-1148
topic 184-1147A; 184-1147B; 184-1147C; 184-1148A; 184-1148B; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Joides Resolution; Leg184; South China Sea
url https://doi.org/10.1594/PANGAEA.713550