Continent-wide drainage reorganization in North America driven by mantle flow

North America (NA) experienced pronounced changes in continental-scale drainage characterized by a reversal for much of the continental interior from north into the Canadian arctic to south into the Gulf of Mexico (GoM) from the Mid-Cretaceous to the Paleocene. However, the driving mechanism for the...

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Published in:Earth and Planetary Science Letters
Main Authors: Wang, Huilin, Gurnis, Michael, Skogseid, Jakob
Format: Article in Journal/Newspaper
Language:unknown
Published: Elsevier 2020
Subjects:
Online Access:https://doi.org/10.1016/j.epsl.2019.115910
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spelling ftcaltechauth:oai:authors.library.caltech.edu:eeh8d-hfe60 2024-09-09T19:27:31+00:00 Continent-wide drainage reorganization in North America driven by mantle flow Wang, Huilin Gurnis, Michael Skogseid, Jakob 2020-01-15 https://doi.org/10.1016/j.epsl.2019.115910 unknown Elsevier https://doi.org/10.1016/j.epsl.2019.115910 oai:authors.library.caltech.edu:eeh8d-hfe60 eprintid:99663 resolverid:CaltechAUTHORS:20191105-092837340 info:eu-repo/semantics/openAccess Other Earth and Planetary Science Letters, 530, Art. No. 115910, (2020-01-15) drainage system mantle flow surface processes Gulf-of-Mexico-routing drainage basin info:eu-repo/semantics/article 2020 ftcaltechauth https://doi.org/10.1016/j.epsl.2019.115910 2024-08-06T15:35:00Z North America (NA) experienced pronounced changes in continental-scale drainage characterized by a reversal for much of the continental interior from north into the Canadian arctic to south into the Gulf of Mexico (GoM) from the Mid-Cretaceous to the Paleocene. However, the driving mechanism for these profound drainage reorganizations remain unexplained. Here, we investigate the role of mantle flow on landscape evolution, by coupling dynamic topography with surface processes. This approach enables us to simulate catchment dynamics and the rearrangement of sediment transport in response to mantle flow. We show that a west-to-east drainage reversal can be induced by the NA overriding the subducted Farallon plate. Moreover, augmented dynamic subsidence caused by a basalt-to-eclogite transformation of an oceanic plateau within the Farallon slab, depressed the GoM region and expanded the integrated drainage to the GoM since the Early Paleocene. For the first time, we show that dynamic topography can explain the north-to-south continental-scale drainage reorganization in North America. © 2019 Elsevier B.V. Received 16 April 2019, Revised 22 September 2019, Accepted 15 October 2019, Available online 5 November 2019. We thank two anonymous reviewers for constructive comments, and Rebecca Bendick for her editorial handling of this manuscript. H.W. and M.G. were funded by the National Science Foundation through EAR-1358646, EAR-1600956, and EAR-1645775 and by Equinor ASA. The original CitcomS code is obtained from Computational Infrastructure for Geodynamics (https://geodynamics.org). The Badlands code is obtained from https://github.com/badlands-model/badlands. Supplemental Material - 1-s2.0-S0012821X19306028-mmc1.pdf Article in Journal/Newspaper Arctic Caltech Authors (California Institute of Technology) Arctic Earth and Planetary Science Letters 530 115910
institution Open Polar
collection Caltech Authors (California Institute of Technology)
op_collection_id ftcaltechauth
language unknown
topic drainage system
mantle flow
surface processes
Gulf-of-Mexico-routing drainage basin
spellingShingle drainage system
mantle flow
surface processes
Gulf-of-Mexico-routing drainage basin
Wang, Huilin
Gurnis, Michael
Skogseid, Jakob
Continent-wide drainage reorganization in North America driven by mantle flow
topic_facet drainage system
mantle flow
surface processes
Gulf-of-Mexico-routing drainage basin
description North America (NA) experienced pronounced changes in continental-scale drainage characterized by a reversal for much of the continental interior from north into the Canadian arctic to south into the Gulf of Mexico (GoM) from the Mid-Cretaceous to the Paleocene. However, the driving mechanism for these profound drainage reorganizations remain unexplained. Here, we investigate the role of mantle flow on landscape evolution, by coupling dynamic topography with surface processes. This approach enables us to simulate catchment dynamics and the rearrangement of sediment transport in response to mantle flow. We show that a west-to-east drainage reversal can be induced by the NA overriding the subducted Farallon plate. Moreover, augmented dynamic subsidence caused by a basalt-to-eclogite transformation of an oceanic plateau within the Farallon slab, depressed the GoM region and expanded the integrated drainage to the GoM since the Early Paleocene. For the first time, we show that dynamic topography can explain the north-to-south continental-scale drainage reorganization in North America. © 2019 Elsevier B.V. Received 16 April 2019, Revised 22 September 2019, Accepted 15 October 2019, Available online 5 November 2019. We thank two anonymous reviewers for constructive comments, and Rebecca Bendick for her editorial handling of this manuscript. H.W. and M.G. were funded by the National Science Foundation through EAR-1358646, EAR-1600956, and EAR-1645775 and by Equinor ASA. The original CitcomS code is obtained from Computational Infrastructure for Geodynamics (https://geodynamics.org). The Badlands code is obtained from https://github.com/badlands-model/badlands. Supplemental Material - 1-s2.0-S0012821X19306028-mmc1.pdf
format Article in Journal/Newspaper
author Wang, Huilin
Gurnis, Michael
Skogseid, Jakob
author_facet Wang, Huilin
Gurnis, Michael
Skogseid, Jakob
author_sort Wang, Huilin
title Continent-wide drainage reorganization in North America driven by mantle flow
title_short Continent-wide drainage reorganization in North America driven by mantle flow
title_full Continent-wide drainage reorganization in North America driven by mantle flow
title_fullStr Continent-wide drainage reorganization in North America driven by mantle flow
title_full_unstemmed Continent-wide drainage reorganization in North America driven by mantle flow
title_sort continent-wide drainage reorganization in north america driven by mantle flow
publisher Elsevier
publishDate 2020
url https://doi.org/10.1016/j.epsl.2019.115910
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_source Earth and Planetary Science Letters, 530, Art. No. 115910, (2020-01-15)
op_relation https://doi.org/10.1016/j.epsl.2019.115910
oai:authors.library.caltech.edu:eeh8d-hfe60
eprintid:99663
resolverid:CaltechAUTHORS:20191105-092837340
op_rights info:eu-repo/semantics/openAccess
Other
op_doi https://doi.org/10.1016/j.epsl.2019.115910
container_title Earth and Planetary Science Letters
container_volume 530
container_start_page 115910
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