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Fossil Chondrichthyes from the Central Eastern Pacific Ocean and their Paleoceanographic Significance

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dc.contributor.author Carrillo-Briceño, Jorge D. en
dc.contributor.author Aguilera, Orangel A. en
dc.contributor.author Rodriguez, Félix en
dc.date.accessioned 2014-07-15T12:52:12Z
dc.date.available 2014-07-15T12:52:12Z
dc.date.issued 2014
dc.identifier.citation Carrillo-Briceño, Jorge D., Aguilera, Orangel A., and Rodriguez, Félix. 2014. "<a href="https://repository.si.edu/handle/10088/21987">Fossil Chondrichthyes from the Central Eastern Pacific Ocean and their Paleoceanographic Significance</a>." <em>Journal of South American Earth Sciences</em>. 51:76&ndash;90. <a href="https://doi.org/10.1016/j.jsames.2014.01.001">https://doi.org/10.1016/j.jsames.2014.01.001</a> en
dc.identifier.issn 0895-9811
dc.identifier.uri http://hdl.handle.net/10088/21987
dc.description.abstract The study of the chondrichthyan fauna from the Angostura, Onzole, Canoa and Jama formations, in the Neogene of Bordón and Manabí basins, Ecuador, reveals the presence of 30 taxa, including the deep water shark +Chlamydoselachus landinii sp. nov. The assemblages are dominated by tropical shallow and deep water chondrichthyans, suggesting paleoenvironments associated with a short platform shelf bordering a deep margin. These assemblages are the most diverse shark and ray association known from the Tropical Central Eastern Pacific Ocean in the South American coastal basin, and provide new information on the paleoecology and paleodiversity of Neogene chondrichthyans. en
dc.relation.ispartof Journal of South American Earth Sciences en
dc.title Fossil Chondrichthyes from the Central Eastern Pacific Ocean and their Paleoceanographic Significance en
dc.type Journal Article en
dc.identifier.srbnumber 118326
dc.identifier.doi 10.1016/j.jsames.2014.01.001
rft.jtitle Journal of South American Earth Sciences
rft.volume 51
rft.spage 76
rft.epage 90
dc.description.SIUnit STRI en
dc.description.SIUnit Peer-reviewed en
dc.citation.spage 76
dc.citation.epage 90


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