Devonian rise in atmospheric oxygen correlated to the radiations of terrestrial plants and large predatory fish
Research output: Contribution to journal › Journal article › Research › peer-review
Standard
Devonian rise in atmospheric oxygen correlated to the radiations of terrestrial plants and large predatory fish. / Dahl, Tais W.; Hammarlund, Emma U.; Anbar, Ariel D.; Bond, David P.G.; Gill, Benjamin C.; Gordon, Gwyneth W.; Knoll, Andrew H.; Nielsen, Arne Thorshøj; Schovsbo, Niels H.; Canfield, Donald E.
In: National Academy of Sciences. Proceedings, Vol. 107, No. 42, 2010, p. 17911-17915.Research output: Contribution to journal › Journal article › Research › peer-review
Harvard
APA
Vancouver
Author
Bibtex
}
RIS
TY - JOUR
T1 - Devonian rise in atmospheric oxygen correlated to the radiations of terrestrial plants and large predatory fish
AU - Dahl, Tais W.
AU - Hammarlund, Emma U.
AU - Anbar, Ariel D.
AU - Bond, David P.G.
AU - Gill, Benjamin C.
AU - Gordon, Gwyneth W.
AU - Knoll, Andrew H.
AU - Nielsen, Arne Thorshøj
AU - Schovsbo, Niels H.
AU - Canfield, Donald E.
PY - 2010
Y1 - 2010
N2 - The evolution of Earth’s biota is intimately linked to the oxygenationof the oceans and atmosphere. We use the isotopic compositionand concentration of molybdenum (Mo) in sedimentary rocksto explore this relationship. Our results indicate two episodes ofglobal ocean oxygenation. The first coincides with the emergenceof the Ediacaran fauna, including large, motile bilaterian animals,ca. 550–560 million year ago (Ma), reinforcing previous geochemicalindications that Earth surface oxygenation facilitated thisradiation. The second, perhaps larger, oxygenation took placearound 400 Ma, well after the initial rise of animals and, therefore,suggesting that early metazoans evolved in a relatively low oxygenenvironment. This later oxygenation correlates with the diversificationof vascular plants, which likely contributed to increasedoxygenation through the enhanced burial of organic carbon insediments. It also correlates with a pronounced radiation of largepredatory fish, animals with high oxygen demand. We therebycouple the redox history of the atmosphere and oceans to majorevents in animal evolution.
AB - The evolution of Earth’s biota is intimately linked to the oxygenationof the oceans and atmosphere. We use the isotopic compositionand concentration of molybdenum (Mo) in sedimentary rocksto explore this relationship. Our results indicate two episodes ofglobal ocean oxygenation. The first coincides with the emergenceof the Ediacaran fauna, including large, motile bilaterian animals,ca. 550–560 million year ago (Ma), reinforcing previous geochemicalindications that Earth surface oxygenation facilitated thisradiation. The second, perhaps larger, oxygenation took placearound 400 Ma, well after the initial rise of animals and, therefore,suggesting that early metazoans evolved in a relatively low oxygenenvironment. This later oxygenation correlates with the diversificationof vascular plants, which likely contributed to increasedoxygenation through the enhanced burial of organic carbon insediments. It also correlates with a pronounced radiation of largepredatory fish, animals with high oxygen demand. We therebycouple the redox history of the atmosphere and oceans to majorevents in animal evolution.
U2 - 10.1073/pnas.1011287107
DO - 10.1073/pnas.1011287107
M3 - Journal article
C2 - 20884852
VL - 107
SP - 17911
EP - 17915
JO - Proceedings of the National Academy of Sciences of the United States of America
JF - Proceedings of the National Academy of Sciences of the United States of America
SN - 0027-8424
IS - 42
ER -
ID: 33965549