Neotropical vegetation responses to Younger Dryas climates as analogs for future climate change scenarios and lessons for conservation

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doi: 10.1016/j.quascirev.2015.03.003
Author(s): Rull, V.; Vegas-Vilarrúbia, T.; Montoya, E.
Author Affiliation(s): Primary:
Botanic Institute of Barcelona, Palynology and Paleoecology Laboratory, Barcelona, Spain
Other:
University of Barcelona, Spain
Open University, United Kingdom
Volume Title: Quaternary Science Reviews
Source: Quaternary Science Reviews, Vol.115, p.28-38. Publisher: Elsevier, International. ISSN: 0277-3791
Note: In English. 86 refs.; illus., incl. 1 table, sketch map
Summary: The Younger Dryas (YD) climatic reversal (12.86-11.65 cal ky BP), especially the warming initiated at ∼12.6 cal ky BP, and the associated vegetation changes have been proposed as past analogs to forecast the potential vegetation responses to future global warming. In this paper, we applied this model to highland and midland Neotropical localities. We used pollen analysis of lake sediments to record vegetation responses to YD climatic changes, which are reconstructed from independent paleoclimatic proxies such as the Mg/Ca ratio on foraminiferal tests and Equilibrium Line Altitude (ELA) for paleotemperature, and grayscale density and Titanium content for paleoprecipitation. Paleoclimatic reconstructions at both highlands and midlands showed a clear YD signal with a conspicuous warming extending into the early Holocene. A small percentage of taxa resulted to be sensitive to these YD climate changes. Response lags were negligible at the resolution of the study. However, changes in the sensitive taxa were relevant enough to determine changes in biodiversity and taxonomic composition. Highland vegetation experienced mainly intra-community reorganizations, whereas midland vegetation underwent major changes leading to community substitutions. This was explained in terms of threshold-crossing non-linear responses in which the coupling of climatic and other forcings (fire) was proposed as the main driving mechanism. Paleoecology provides meaningful insights on the responses of highland and midland Neotropical vegetation to the YD climatic reversal. Biotic responses at both individual (species) and collective (assemblage) levels showed patterns and processes of vegetation change useful to understand its ecological dynamics, as well as the mechanisms and external drivers involved. The use of paleoecological methods to document the biotic responses to the YD climate shifts can be useful to help forecasting the potential consequences of future global warming. Due to its quasi-global character, the YD reversal emerges as a well suited candidate for providing useful insights of global scope by analyzing the corresponding biotic responses virtually at any geographical and biological setting. Abstract Copyright (2015) Elsevier, B.V.
Year of Publication: 2015
Research Program: ODP Ocean Drilling Program
Key Words: 24 Surficial Geology, Quaternary Geology; Alkaline earth metals; Atlantic Ocean; Biodiversity; Biostratigraphy; Calcium; Cariaco Basin; Caribbean Sea; Cenozoic; Chemostratigraphy; Ecology; Foraminifera; Global change; Global warming; Invertebrata; Lacustrine environment; Lake sediments; Leg 165; Lithostratigraphy; Magnesium; Marine sediments; Metals; Mg/Ca; Microfossils; Miospores; North Atlantic; ODP Site 1002; Ocean Drilling Program; Paleoclimatology; Paleoecology; Paleotemperature; Palynomorphs; Pleistocene; Pollen; Prediction; Protista; Quaternary; Reconstruction; Sediments; South America; Upper Pleistocene; Upper Weichselian; Vegetation; Venezuela; Weichselian; Younger Dryas
Coordinates: N104222 N104222 W0651011 W0651011
Record ID: 2015073198
Copyright Information: GeoRef, Copyright 2019 American Geosciences Institute. Reference includes data from CAPCAS, Elsevier Scientific Publishers, Amsterdam, Netherlands