New sedimentary evidence reveals a unique history of C4 biomass in continental East Asia since the early Miocene

Abstract Pyrogenic carbon (PyC) and n-alkane data from sediments in the northern South China Sea reveal variations in material from C4 plants in East Asia over the last ~19 Ma. These data indicate the likely presence of C4 taxa during the earliest part of the record analysed, with C4 species also pr...

Descripción completa

Guardado en:
Detalles Bibliográficos
Autores principales: Bin Zhou, Michael Bird, Hongbo Zheng, Enlou Zhang, Christopher M. Wurster, Luhua Xie, David Taylor
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2017
Materias:
R
Q
Acceso en línea:https://doaj.org/article/e2575fdf0aaa4b12a6c4caab4d223078
Etiquetas: Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
id oai:doaj.org-article:e2575fdf0aaa4b12a6c4caab4d223078
record_format dspace
spelling oai:doaj.org-article:e2575fdf0aaa4b12a6c4caab4d2230782021-12-02T15:05:01ZNew sedimentary evidence reveals a unique history of C4 biomass in continental East Asia since the early Miocene10.1038/s41598-017-00285-72045-2322https://doaj.org/article/e2575fdf0aaa4b12a6c4caab4d2230782017-03-01T00:00:00Zhttps://doi.org/10.1038/s41598-017-00285-7https://doaj.org/toc/2045-2322Abstract Pyrogenic carbon (PyC) and n-alkane data from sediments in the northern South China Sea reveal variations in material from C4 plants in East Asia over the last ~19 Ma. These data indicate the likely presence of C4 taxa during the earliest part of the record analysed, with C4 species also prominent during the mid and late Miocene and especially the mid Quaternary. Notably the two records diverge after the mid Quaternary, when PyC data indicate a reduced contribution of C4 taxa to biomass burning, whereas plant-derived n-alkanes indicate a greater abundance of C4 plants. This divergence likely reflects differences in the predominant source areas of organic materials accumulating at the coring site, with PyC representing a larger source area that includes material transported in the atmosphere from more temperate (relatively cooler and drier) parts of East Asia. Variations in the relative abundances of C3 and C4 taxa appear to be linked to a combination of environmental factors that have varied temporally and geographically and that are unique to East Asia. A major expansion of C4 biomass in warmer subtropical parts of eastern Asia from ~1 Ma and particularly from ~0.4 Ma is later than other parts of the world.Bin ZhouMichael BirdHongbo ZhengEnlou ZhangChristopher M. WursterLuhua XieDavid TaylorNature PortfolioarticleMedicineRScienceQENScientific Reports, Vol 7, Iss 1, Pp 1-9 (2017)
institution DOAJ
collection DOAJ
language EN
topic Medicine
R
Science
Q
spellingShingle Medicine
R
Science
Q
Bin Zhou
Michael Bird
Hongbo Zheng
Enlou Zhang
Christopher M. Wurster
Luhua Xie
David Taylor
New sedimentary evidence reveals a unique history of C4 biomass in continental East Asia since the early Miocene
description Abstract Pyrogenic carbon (PyC) and n-alkane data from sediments in the northern South China Sea reveal variations in material from C4 plants in East Asia over the last ~19 Ma. These data indicate the likely presence of C4 taxa during the earliest part of the record analysed, with C4 species also prominent during the mid and late Miocene and especially the mid Quaternary. Notably the two records diverge after the mid Quaternary, when PyC data indicate a reduced contribution of C4 taxa to biomass burning, whereas plant-derived n-alkanes indicate a greater abundance of C4 plants. This divergence likely reflects differences in the predominant source areas of organic materials accumulating at the coring site, with PyC representing a larger source area that includes material transported in the atmosphere from more temperate (relatively cooler and drier) parts of East Asia. Variations in the relative abundances of C3 and C4 taxa appear to be linked to a combination of environmental factors that have varied temporally and geographically and that are unique to East Asia. A major expansion of C4 biomass in warmer subtropical parts of eastern Asia from ~1 Ma and particularly from ~0.4 Ma is later than other parts of the world.
format article
author Bin Zhou
Michael Bird
Hongbo Zheng
Enlou Zhang
Christopher M. Wurster
Luhua Xie
David Taylor
author_facet Bin Zhou
Michael Bird
Hongbo Zheng
Enlou Zhang
Christopher M. Wurster
Luhua Xie
David Taylor
author_sort Bin Zhou
title New sedimentary evidence reveals a unique history of C4 biomass in continental East Asia since the early Miocene
title_short New sedimentary evidence reveals a unique history of C4 biomass in continental East Asia since the early Miocene
title_full New sedimentary evidence reveals a unique history of C4 biomass in continental East Asia since the early Miocene
title_fullStr New sedimentary evidence reveals a unique history of C4 biomass in continental East Asia since the early Miocene
title_full_unstemmed New sedimentary evidence reveals a unique history of C4 biomass in continental East Asia since the early Miocene
title_sort new sedimentary evidence reveals a unique history of c4 biomass in continental east asia since the early miocene
publisher Nature Portfolio
publishDate 2017
url https://doaj.org/article/e2575fdf0aaa4b12a6c4caab4d223078
work_keys_str_mv AT binzhou newsedimentaryevidencerevealsauniquehistoryofc4biomassincontinentaleastasiasincetheearlymiocene
AT michaelbird newsedimentaryevidencerevealsauniquehistoryofc4biomassincontinentaleastasiasincetheearlymiocene
AT hongbozheng newsedimentaryevidencerevealsauniquehistoryofc4biomassincontinentaleastasiasincetheearlymiocene
AT enlouzhang newsedimentaryevidencerevealsauniquehistoryofc4biomassincontinentaleastasiasincetheearlymiocene
AT christophermwurster newsedimentaryevidencerevealsauniquehistoryofc4biomassincontinentaleastasiasincetheearlymiocene
AT luhuaxie newsedimentaryevidencerevealsauniquehistoryofc4biomassincontinentaleastasiasincetheearlymiocene
AT davidtaylor newsedimentaryevidencerevealsauniquehistoryofc4biomassincontinentaleastasiasincetheearlymiocene
_version_ 1718388988736176128