4.7 Article

The Neogene-Quaternary diversification trend in the shaping of modern Caribbean mangroves

Journal

QUATERNARY SCIENCE REVIEWS
Volume 300, Issue -, Pages -

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.quascirev.2022.107920

Keywords

Caribbean; Neotropics; Neogene; Quaternary; Mangroves; Pollen; Diversity

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This paper analyzes the diversification of the Neotropical mangrove flora in the Caribbean region from the Miocene to the present. A Neogene-Quaternary diversification trend has been identified, with an increase of 25 genera compared to the existing Paleogene representatives. The appearance of mangrove genera occurred mainly in the Miocene and Oligo-Miocene transition, contributing to the overall diversification pattern. The absence of regional extinctions since the Miocene suggests the persistence of mangrove diversity in the Caribbean.
This paper analyzes the diversification of the Neotropical mangrove flora from the Miocene to the present, using a fairly comprehensive database of 110 pollen records distributed across the whole Caribbean region. A Neogene-Quaternary diversification trend (NQDT) has been identified, characterized by an increase of 25 genera (similar to 78%) with respect to the 7 already existing Paleogene representatives. Only two genera appeared during the Miocene and the maximum increases were observed in the Pliocene-Quaternary transition and the modern-living record. Half of the true-mangrove genera (Rhizophora, Pelliciera, Acrostichum) were already present before the Neogene and the others appeared gradually in the Oligo-Miocene (Crenea), the Early-Middle Miocene (Avicennia) and the Mio-Pliocene (Laguncularia). None of the extant associate mangrove genera were present during the Paleogene and all appeared in the Miocene (23 genera) or the Oligo-Miocene transition (3 genera), being the main responsible for the NQDT, in absolute numbers. No regional extinctions were recorded since the Miocene in the Caribbean mangroves, at the generic level. These observations should be complemented with further high-resolution quantitative studies aimed at finding potential causal relationships with climatic, eustatic and paleogeographical shifts. (c) 2022 The Author. Published by Elsevier Ltd.

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