Beyond the intertropical convergence zone: A regional synthesis of Late Pleistocene hydroclimate in the northern Tropical Americas
Palaeogeography Palaeoclimatology Palaeoecology, pp. 114250
Abstract
The northern Tropical Americas (NTA) is influenced by multiple large-scale hydroclimate drivers, including the Intertropical Convergence Zone (ITCZ), whose position and strength varied significantly during the Late Pleistocene (130–11.7 kyr BP). Since the 1960s, paleoclimate studies have provided valuable but often scattered insights into environmental changes and precipitation variability. Recent advances in dating techniques, access to older sediment records, and the development of novel proxies have improved our understanding of regional climate dynamics during recent glacial-interglacial cycles. This review compiles paleoclimate records from 166 sites across the NTA, derived from 241 studies spanning terrestrial and marine archives, to assess the current state of paleoclimatological knowledge and identify gaps and limitations. We examine a subset of 83 sites covering Marine Isotope Stage 5 (MIS5; 130–70 kyr BP) to the Last Glacial Maximum (LGM; 22–17.5 kyr BP) in detail, focusing on precipitation patterns. We explore the interactions among major atmospheric and oceanic processes, including the ITCZ, the Atlantic Meridional Overturning Circulation, the North Atlantic High System, the Caribbean Low-Level Jet, and the North American Monsoon. Our synthesis reveals pronounced spatial differences in precipitation regimes across tropical and subtropical ecosystems from MIS5 to the LGM. These findings challenge the prevailing view of the warm-wet interglacial versus cold-dry glacial framework in the NTA. Instead, orbital and millennial-scale variability, combined with altitude, meridional gradients and local orography, modulate the timing and amplitude of hydroclimate responses. This review places the NTA within the broader framework of global Late Pleistocene climatology and identifies key directions for future paleoclimate research in the region.
Authors 7
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Rodrigo Martínez-Abarca corresponding
Technische Universität Braunschweig · LIAG Institute for Applied Geophysics
Affiliation as printed
Institute of Geosystems and Bioindication, Technische Universität Braunschweig, Braunschweig 38106, Germany
LIAG-Institute for Applied Geophysics, Hanover 30655, Germany
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Christian-Albrechts-Universität zu Kiel
Affiliation as printed
Institute of Geosciences, Kiel University, 24118 Kiel, Germany
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Universidad Nacional Autónoma de México · Instituto de Geociencias
Affiliation as printed
Instituto de Geociencias, Universidad Nacional Autónoma de México, Juriquilla 76230, Mexico
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University of Helsinki · Bolin Centre for Climate Research
Affiliation as printed
Department of Geological Sciences and Bolin Centre for Climate Research, Stockholm University, Stockholm 11418, Sweden
Department of Geosciences and Geography, University of Helsinki, Helsinki 00014, Finland
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Technische Universität Braunschweig
Affiliation as printed
Institute of Geosystems and Bioindication, Technische Universität Braunschweig, Braunschweig 38106, Germany
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LIAG Institute for Applied Geophysics
Affiliation as printed
LIAG-Institute for Applied Geophysics, Hanover 30655, Germany
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Affiliation as printed
Chair of Organic Biogeochemistry in Geo-Systems, RWTH Aachen University, Aachen 52064, Germany
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