Where were the Caribbean mangroves during the Last Glacial Maximum? A preliminary microtopographical appraisal

During the Last Glacial Maximum (LGM), when global sea levels dropped by ∼132 m, the Caribbean continental shelf was fully exposed, which drastically reduced the flat topographical habitat necessary for mangrove growth. It has been proposed that mangroves survived in flat microsites beyond the shelf break and later expanded from these microrefugia to their current distribution after the LGM. However, this hypothesis remains untested. This study aims to identify potential refugia by locating flat areas around the -132 m isobath using Global Multiresolution Topography (GMRT) images. A significant ∼200-km-long potential refugium was identified on the northern Trinidad (NT) shelf, along with several scattered kilometer-scale microrefugia near the Cariaco Basin (CB) in northeastern Venezuela. Additionally, two isolated prospective microrefugia were detected in northern Colombia (NC) and western Hispaniola (WH). The remaining LGM Caribbean coasts were considered unsuitable for mangrove growth. The NT refugium, along with the CB microrefugia, may have served as the primary sources for subsequent mangrove expansion. This expansion was likely facilitated by postglacial sea-level rise and the SE-NE Caribbean Current (CC), which would have acted as a major agent for propagule dispersal. This microtopographical survey not only supports the microrefugial hypothesis but also narrows the focus to the most promising areas, significantly reducing the time, effort and resources required for future seismic and coring campaigns. • Caribbean mangroves would have survived the LGM lowstand (-132 m) in (micro)refugia beyond the shelf break • High-resolution image analyses identified a major potential refugium in northern Trinidad (NT) and other scattered microrefugia • The remaining LGM Caribbean coasts were considered topographically unsuitable for mangrove growth • The NT refugium may have served as the primary source for postglacial mangrove expansion favored by the SE-NE Caribbean current • These results narrow the focus to the most promising areas for future coring campaigns

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Journal
Estuarine Coastal and Shelf Science
Published
2025-06-17
DOI
https://doi.org/10.1016/j.ecss.2025.109404
Citations
1
Primary Topic
Geology and Paleoclimatology Research
Type
article
Field-Weighted Citation Impact
1.30
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article

Where were the Caribbean mangroves during the Last Glacial Maximum? A preliminary microtopographical appraisal

Valentı́ Rull
1 citations
Estuarine Coastal and Shelf Science
Geology and Paleoclimatology Research
1.30
article

Where were the Caribbean mangroves during the Last Glacial Maximum? A preliminary microtopographical appraisal

Valentı́ Rull
article en
1 citations

Abstract

During the Last Glacial Maximum (LGM), when global sea levels dropped by ∼132 m, the Caribbean continental shelf was fully exposed, which drastically reduced the flat topographical habitat necessary for mangrove growth. It has been proposed that mangroves survived in flat microsites beyond the shelf break and later expanded from these microrefugia to their current distribution after the LGM. However, this hypothesis remains untested. This study aims to identify potential refugia by locating flat areas around the -132 m isobath using Global Multiresolution Topography (GMRT) images. A significant ∼200-km-long potential refugium was identified on the northern Trinidad (NT) shelf, along with several scattered kilometer-scale microrefugia near the Cariaco Basin (CB) in northeastern Venezuela. Additionally, two isolated prospective microrefugia were detected in northern Colombia (NC) and western Hispaniola (WH). The remaining LGM Caribbean coasts were considered unsuitable for mangrove growth. The NT refugium, along with the CB microrefugia, may have served as the primary sources for subsequent mangrove expansion. This expansion was likely facilitated by postglacial sea-level rise and the SE-NE Caribbean Current (CC), which would have acted as a major agent for propagule dispersal. This microtopographical survey not only supports the microrefugial hypothesis but also narrows the focus to the most promising areas, significantly reducing the time, effort and resources required for future seismic and coring campaigns. • Caribbean mangroves would have survived the LGM lowstand (-132 m) in (micro)refugia beyond the shelf break • High-resolution image analyses identified a major potential refugium in northern Trinidad (NT) and other scattered microrefugia • The remaining LGM Caribbean coasts were considered topographically unsuitable for mangrove growth • The NT refugium may have served as the primary source for postglacial mangrove expansion favored by the SE-NE Caribbean current • These results narrow the focus to the most promising areas for future coring campaigns

Estuarine Coastal and Shelf ScienceVol. 323
Universitat Autònoma de Barcelona (ES), Institut Botànic de Barcelona (ES), Institut Català de Paleontologia Miquel Crusafont (ES)
Life below water
Openalex Percentile: Top 21%
Geology and Paleoclimatology Research
1.30
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