2020
DOI: 10.3389/ffgc.2020.00008
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Connectivity of Neotropical River Basins in the Central Guiana Shield Based on Fish Distributions

Abstract: The Guiana Shield in northeastern South America contains some of the largest tracts of intact forests on the globe. Guyana alone has more than 80% forest cover. In south-central Guyana a unique biogeographic feature allows for a hydrological connection between the Guiana Shield with the Amazon basin via the Rupununi savannas and wetlands (Rupununi Portal). This corridor allows for connectivity between two of the most biodiverse, carbon rich, and intact forests in the world. The significance of this (and other)… Show more

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Cited by 7 publications
(4 citation statements)
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References 53 publications
(59 reference statements)
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“…The close relationships between Branco, Essequibo, and Guiana Shield taxa recovered for the Pliocene and Pleistocene can be explained by intermittent river connections between the lower portions of these drainages (as discussed in Lima, 2017); alternatively, these patterns could be related to headwater capture events between the Branco and the proto‐Berbice (a large drainage system from the central Guiana Shield that drained most of the Guyana and parts of Brazil, Venezuela, and Surinam from the Cenozoic to the Pleistocene – see Sinha, 1968; Lujan & Armbruster, 2011; Schaefer & Vale Júnior, 1997). Pleistocene and younger interactions between the Branco and Essequibo basins can be attributed to the Rupununi Portal, a flooded savanna area that allows for seasonal faunal interchange between these basins (De Souza et al, 2012, 2020; Hubert & Renno, 2006; Lovejoy & Araújo, 2000).…”
Section: Discussionmentioning
confidence: 99%
“…The close relationships between Branco, Essequibo, and Guiana Shield taxa recovered for the Pliocene and Pleistocene can be explained by intermittent river connections between the lower portions of these drainages (as discussed in Lima, 2017); alternatively, these patterns could be related to headwater capture events between the Branco and the proto‐Berbice (a large drainage system from the central Guiana Shield that drained most of the Guyana and parts of Brazil, Venezuela, and Surinam from the Cenozoic to the Pleistocene – see Sinha, 1968; Lujan & Armbruster, 2011; Schaefer & Vale Júnior, 1997). Pleistocene and younger interactions between the Branco and Essequibo basins can be attributed to the Rupununi Portal, a flooded savanna area that allows for seasonal faunal interchange between these basins (De Souza et al, 2012, 2020; Hubert & Renno, 2006; Lovejoy & Araújo, 2000).…”
Section: Discussionmentioning
confidence: 99%
“…the Prone‐8 hypothesis of Lujan & Armbruster, 2011). Alternatively, the lineage may have dispersed from Proto‐Berbice to the central Amazon basin and then to north‐eastern Brazil, using corridors resembling those connecting the modern Branco and Essequibo basins (Fontenelle et al, 2021; Lujan & Armbruster, 2011; de Souza et al, 2020).…”
Section: Discussionmentioning
confidence: 99%
“…Multivariate statistical analyses can reveal significant trends in fish assemblage structure and environmental conditions (de Souza et al ., 2020). Multivariate analysis, including hierarchical cluster and MDS, determined relationships among the six fish assemblages in the present study.…”
Section: Discussionmentioning
confidence: 99%