Fig. 5 in The changing course of the Amazon River in the Neogene: center stage for Neotropical diversification

Fig. 5. Summary of hydrological connections among major sedimentary basins of northern South America through the Neogene. Caribbean-draining Andean foreland basins in orange. Atlantic-draining basins contributing to transcontinental Amazon in yellow. Other north Atlantic-draining basins in shades of...

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Main Authors: Albert, James S., Val, Pedro, Hoorn, Carina
Format: Other/Unknown Material
Language:unknown
Published: Zenodo 2018
Subjects:
Online Access:https://doi.org/10.5281/zenodo.3709970
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spelling ftzenodo:oai:zenodo.org:3709970 2024-09-15T18:23:43+00:00 Fig. 5 in The changing course of the Amazon River in the Neogene: center stage for Neotropical diversification Albert, James S. Val, Pedro Hoorn, Carina 2018-10-18 https://doi.org/10.5281/zenodo.3709970 unknown Zenodo https://doi.org/10.1590/1982-0224-20180033 lsid:urn:lsid:plazi.org:pub:FFE93527B5156B1CF621FFCDB02BFFD2 https://zenodo.org/record/3709960 https://zenodo.org/communities/biosyslit https://doi.org/10.5281/zenodo.3709969 https://doi.org/10.5281/zenodo.3709970 oai:zenodo.org:3709970 info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode Neotropical Ichthyology, 16(3), 1-24, (2018-10-18) Biodiversity Taxonomy info:eu-repo/semantics/other 2018 ftzenodo https://doi.org/10.5281/zenodo.370997010.1590/1982-0224-2018003310.5281/zenodo.3709969 2024-07-26T14:52:12Z Fig. 5. Summary of hydrological connections among major sedimentary basins of northern South America through the Neogene. Caribbean-draining Andean foreland basins in orange. Atlantic-draining basins contributing to transcontinental Amazon in yellow. Other north Atlantic-draining basins in shades of green. South Atlantic-draining (La Plata) basins in blue. Connectivity as a block-design landscape evolution model at right preserving general spatial relationships. Red arrows depict predominant direction of sediment and water flow. Double-headed arrow indicates bidirectional connections during that time interval. Vicariance events when basins of the same color change to different colors between time intervals; geodispersal events when basins with different colors change to same color. Connections of basins in grey are poorly constrained by avai- lable data. Basin in white is entirely marine. "W. Amazon" refers to the combined Putumayo, Napo, Marañón and Ucayali sedimentary basins, "Llanos" to the combined Llanos, and Barinas/Apure basins, "Amazonas" to the combined Amazonas and Marajo basins, and "Essequibo" to the Proto-Berbice basin. Sedimentary basins with four letter abbreviations at left in top panel. Base-maps with modern coastlines and topography to facilitate orientation. Published as part of Albert, James S., Val, Pedro & Hoorn, Carina, 2018, The changing course of the Amazon River in the Neogene: center stage for Neotropical diversification, pp. 1-24 in Neotropical Ichthyology 16 (3) on page 11, DOI:10.1590/1982-0224-20180033, http://zenodo.org/record/3709960 Other/Unknown Material North Atlantic Zenodo
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language unknown
topic Biodiversity
Taxonomy
spellingShingle Biodiversity
Taxonomy
Albert, James S.
Val, Pedro
Hoorn, Carina
Fig. 5 in The changing course of the Amazon River in the Neogene: center stage for Neotropical diversification
topic_facet Biodiversity
Taxonomy
description Fig. 5. Summary of hydrological connections among major sedimentary basins of northern South America through the Neogene. Caribbean-draining Andean foreland basins in orange. Atlantic-draining basins contributing to transcontinental Amazon in yellow. Other north Atlantic-draining basins in shades of green. South Atlantic-draining (La Plata) basins in blue. Connectivity as a block-design landscape evolution model at right preserving general spatial relationships. Red arrows depict predominant direction of sediment and water flow. Double-headed arrow indicates bidirectional connections during that time interval. Vicariance events when basins of the same color change to different colors between time intervals; geodispersal events when basins with different colors change to same color. Connections of basins in grey are poorly constrained by avai- lable data. Basin in white is entirely marine. "W. Amazon" refers to the combined Putumayo, Napo, Marañón and Ucayali sedimentary basins, "Llanos" to the combined Llanos, and Barinas/Apure basins, "Amazonas" to the combined Amazonas and Marajo basins, and "Essequibo" to the Proto-Berbice basin. Sedimentary basins with four letter abbreviations at left in top panel. Base-maps with modern coastlines and topography to facilitate orientation. Published as part of Albert, James S., Val, Pedro & Hoorn, Carina, 2018, The changing course of the Amazon River in the Neogene: center stage for Neotropical diversification, pp. 1-24 in Neotropical Ichthyology 16 (3) on page 11, DOI:10.1590/1982-0224-20180033, http://zenodo.org/record/3709960
format Other/Unknown Material
author Albert, James S.
Val, Pedro
Hoorn, Carina
author_facet Albert, James S.
Val, Pedro
Hoorn, Carina
author_sort Albert, James S.
title Fig. 5 in The changing course of the Amazon River in the Neogene: center stage for Neotropical diversification
title_short Fig. 5 in The changing course of the Amazon River in the Neogene: center stage for Neotropical diversification
title_full Fig. 5 in The changing course of the Amazon River in the Neogene: center stage for Neotropical diversification
title_fullStr Fig. 5 in The changing course of the Amazon River in the Neogene: center stage for Neotropical diversification
title_full_unstemmed Fig. 5 in The changing course of the Amazon River in the Neogene: center stage for Neotropical diversification
title_sort fig. 5 in the changing course of the amazon river in the neogene: center stage for neotropical diversification
publisher Zenodo
publishDate 2018
url https://doi.org/10.5281/zenodo.3709970
genre North Atlantic
genre_facet North Atlantic
op_source Neotropical Ichthyology, 16(3), 1-24, (2018-10-18)
op_relation https://doi.org/10.1590/1982-0224-20180033
lsid:urn:lsid:plazi.org:pub:FFE93527B5156B1CF621FFCDB02BFFD2
https://zenodo.org/record/3709960
https://zenodo.org/communities/biosyslit
https://doi.org/10.5281/zenodo.3709969
https://doi.org/10.5281/zenodo.3709970
oai:zenodo.org:3709970
op_rights info:eu-repo/semantics/openAccess
Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
op_doi https://doi.org/10.5281/zenodo.370997010.1590/1982-0224-2018003310.5281/zenodo.3709969
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