dc.contributor.author |
Bralower, Timothy J. |
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dc.contributor.author |
Cosmidis, Julie |
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dc.contributor.author |
Fantle, M. S. |
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dc.contributor.author |
Lowery, Christopher M. |
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dc.contributor.author |
Passey, B. H. |
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dc.contributor.author |
Gulick, Sean P. S. |
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dc.contributor.author |
Morgan, V. J. |
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dc.contributor.author |
Vajda, V. |
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dc.contributor.author |
Whalen, Michael T. |
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dc.contributor.author |
Wittmann, Axel 1971- |
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dc.contributor.author |
Artemieva, Natalia A. |
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dc.contributor.author |
Farley, K. |
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dc.contributor.author |
Goderis, Steven |
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dc.contributor.author |
Hajek, E. |
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dc.contributor.author |
Heaney, P. J. |
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dc.contributor.author |
Kring, David A. (David Allen) |
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dc.contributor.author |
Lyons, S. L. |
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dc.contributor.author |
Rasmussen, C. |
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dc.contributor.author |
Sibert, E. |
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dc.contributor.author |
Rodríguez Tovar, Francisco J. |
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dc.contributor.author |
Turner‐Walker, G. |
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dc.contributor.author |
Zachos, James C. |
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dc.contributor.author |
Carte, J. |
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dc.contributor.author |
Chen, S. A. |
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dc.contributor.author |
Cockell, Charles |
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dc.contributor.author |
Coolen, M. |
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dc.contributor.author |
Freeman, K. H. |
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dc.contributor.author |
Garber, J. |
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dc.contributor.author |
Gonzalez, M. |
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dc.contributor.author |
Gray, J. L. |
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dc.contributor.author |
Grice, Kliti |
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dc.contributor.author |
Jones, Heather L. |
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dc.contributor.author |
Schaefer, Bettina |
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dc.contributor.author |
Smit, Jan |
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dc.contributor.author |
Tikoo, S. M. |
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dc.coverage.spatial |
Gulf of Mexico |
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dc.date.accessioned |
2020-12-07T18:47:40Z |
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dc.date.available |
2020-12-07T18:47:40Z |
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dc.date.issued |
2020-11-24 |
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dc.identifier.citation |
Bralower, T. J., Cosmidis, J., Fantle, M. S., Lowery, C. M., Passey, B. H., Gulick, S. P. S., et al. (2020). The habitat of the nascent Chicxulub crater. AGU Advances, 2, e2020AV000208. https://doi.org/10.1029/2020AV000208 |
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dc.identifier.other |
DOI: 10.1029/2020av000208 |
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dc.identifier.uri |
https://hdl.handle.net/20.500.11753/1726 |
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dc.description.abstract |
The newly formed Chicxulub crater was rapidly filled by seawater then disturbed by tsunami and seiche waves. Sedimentary layers deposited as wave energy declined provide a unique window into the environment of the nascent crater in the months and years to millennia after the impact. |
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dc.description.sponsorship |
Downloaded from the publisher site |
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dc.description.statementofresponsibility |
T. J. Bralower, J. Cosmidis, M. S. Fantle, C. M. Lowery, B. H. Passey, S. P. S. Gulick, J. V. Morgan, V. Vajda, M. T. Whalen, A. Wittmann, N. Artemieva, K. Farley, S. Goderis, E. Hajek, P. J. Heaney, D. A. Kring, S. L. Lyons, C. Rasmussen, E. Sibert, F. J. Rodríguez Tovar, G. Turner‐Walker, J. C. Zachos, J. Carte, S. A. Chen, C. Cockell, M. Coolen, K. H. Freeman, J. Garber, M. Gonzalez, J. L. Gray, K. Grice, H. L. Jones, B. Schaefer, J. Smit, S. M. Tikoo |
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dc.format.extent |
27 pages |
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dc.format.mimetype |
application/pdf |
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dc.language.iso |
en |
en |
dc.publisher |
Wiley |
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dc.relation.ispartofseries |
LPI contribution ; no. 2572 |
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dc.subject |
Chicxulub Crater |
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dc.subject |
Cretaceous-Paleogene boundary |
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dc.title |
The Habitat of the Nascent Chicxulub Crater |
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dc.type |
Article |
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dc.rights.license |
This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited. |
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