Ocean Carbon Storage across the middle Miocene: a new interpretation for the Monterey Event
In this study, the authors use planktic foraminiferal data to reconstruct ocean carbonate chemistry and temperature from 16.5 to 11 Ma from a size in the tropical eastern Indian Ocean to look at the causes of the Monterey Excursion (ME). They find a positive relationship between dissolved inorganic...
Guardado en:
Autores principales: | , , , , |
---|---|
Formato: | article |
Lenguaje: | EN |
Publicado: |
Nature Portfolio
2020
|
Materias: | |
Acceso en línea: | https://doaj.org/article/684b2b4c502749d680eb8805e70e12ea |
Etiquetas: |
Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
|
id |
oai:doaj.org-article:684b2b4c502749d680eb8805e70e12ea |
---|---|
record_format |
dspace |
spelling |
oai:doaj.org-article:684b2b4c502749d680eb8805e70e12ea2021-12-02T17:31:56ZOcean Carbon Storage across the middle Miocene: a new interpretation for the Monterey Event10.1038/s41467-019-13792-02041-1723https://doaj.org/article/684b2b4c502749d680eb8805e70e12ea2020-01-01T00:00:00Zhttps://doi.org/10.1038/s41467-019-13792-0https://doaj.org/toc/2041-1723In this study, the authors use planktic foraminiferal data to reconstruct ocean carbonate chemistry and temperature from 16.5 to 11 Ma from a size in the tropical eastern Indian Ocean to look at the causes of the Monterey Excursion (ME). They find a positive relationship between dissolved inorganic (DIC) carbon and the ME and a negative one for DIC and the carbon maxima events.S. M. SosdianT. L. BabilaR. GreenopG. L. FosterC. H. LearNature PortfolioarticleScienceQENNature Communications, Vol 11, Iss 1, Pp 1-11 (2020) |
institution |
DOAJ |
collection |
DOAJ |
language |
EN |
topic |
Science Q |
spellingShingle |
Science Q S. M. Sosdian T. L. Babila R. Greenop G. L. Foster C. H. Lear Ocean Carbon Storage across the middle Miocene: a new interpretation for the Monterey Event |
description |
In this study, the authors use planktic foraminiferal data to reconstruct ocean carbonate chemistry and temperature from 16.5 to 11 Ma from a size in the tropical eastern Indian Ocean to look at the causes of the Monterey Excursion (ME). They find a positive relationship between dissolved inorganic (DIC) carbon and the ME and a negative one for DIC and the carbon maxima events. |
format |
article |
author |
S. M. Sosdian T. L. Babila R. Greenop G. L. Foster C. H. Lear |
author_facet |
S. M. Sosdian T. L. Babila R. Greenop G. L. Foster C. H. Lear |
author_sort |
S. M. Sosdian |
title |
Ocean Carbon Storage across the middle Miocene: a new interpretation for the Monterey Event |
title_short |
Ocean Carbon Storage across the middle Miocene: a new interpretation for the Monterey Event |
title_full |
Ocean Carbon Storage across the middle Miocene: a new interpretation for the Monterey Event |
title_fullStr |
Ocean Carbon Storage across the middle Miocene: a new interpretation for the Monterey Event |
title_full_unstemmed |
Ocean Carbon Storage across the middle Miocene: a new interpretation for the Monterey Event |
title_sort |
ocean carbon storage across the middle miocene: a new interpretation for the monterey event |
publisher |
Nature Portfolio |
publishDate |
2020 |
url |
https://doaj.org/article/684b2b4c502749d680eb8805e70e12ea |
work_keys_str_mv |
AT smsosdian oceancarbonstorageacrossthemiddlemioceneanewinterpretationforthemontereyevent AT tlbabila oceancarbonstorageacrossthemiddlemioceneanewinterpretationforthemontereyevent AT rgreenop oceancarbonstorageacrossthemiddlemioceneanewinterpretationforthemontereyevent AT glfoster oceancarbonstorageacrossthemiddlemioceneanewinterpretationforthemontereyevent AT chlear oceancarbonstorageacrossthemiddlemioceneanewinterpretationforthemontereyevent |
_version_ |
1718380433411932160 |