4.7 Article

Miocene fossils from the southeastern Pacific shed light on the last radiation of marine crocodylians

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ROYAL SOC
DOI: 10.1098/rspb.2022.0380

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Gavialoidea; marine crocodylians; phylogenetics; biogeography; longirostrine ecomorphs

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  1. CONCYTEC, Peru. (Incorporacion de Investigadores) [034-2019-02-FONDECYT-BM-INC.INV, 104-2018-FONDECYT, 149-2018-FON-DECYT-BM-IADT-AV]

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Fossils from marine deposits in Peru reveal that crocodylians were coastal residents in the southeastern Pacific for approximately 14 million years during the Miocene epoch. The fossil record shows that the evolution of marine crocodylians primarily occurred in gavialids and their stem relatives. Marine gavialoids were shallow sea dwellers and their diversification was influenced by coastal habitats. However, they disappeared from the sea during the Pliocene marine megafauna extinction.
The evolution of crocodylians as sea dwellers remains obscure because living representatives are basically freshwater inhabitants and fossil evidence lacks crucial aspects about crocodylian occupation of marine ecosystems. New fossils from marine deposits of Peru reveal that crocodylians were habitual coastal residents of the southeastern Pacific (SEP) for approximately 14 million years within the Miocene (ca 19 to 5 Ma), an epoch including the highest global peak of marine crocodylian diversity. The assemblage of the SEP comprised two long and slender-snouted (longirostrine) taxa of the Gavialidae: the giant Piscogavialis and a new early diverging species, Sacacosuchus cordovai. Although living gavialids (Gavialis and Tomistoma) are freshwater forms, this remarkable fossil record and a suite of evolutionary morphological analyses reveal that the whole evolution of marine crocodylians pertained to the gavialids and their stem relatives (Gavialoidea). This adaptive radiation produced two longirostrine ecomorphs with dissimilar trophic roles in seawaters and involved multiple transmarine dispersals to South America and most landmasses. Marine gavialoids were shallow sea dwellers, and their Cenozoic diversification was influenced by the availability of coastal habitats. Soon after the richness peak of the Miocene, gavialoid crocodylians disappeared from the sea, probably as part of the marine megafauna extinction of the Pliocene.

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