Search from over 60,000 research works

Advanced Search

Climate change and biogeographic connectivity across the Brazilian cerrado

Full text not archived in this repository.
Add to AnyAdd to TwitterAdd to FacebookAdd to LinkedinAdd to PinterestAdd to Email

De Oliveira, P. E., Raczka, M. orcid id iconORCID: https://orcid.org/0000-0002-6602-8087, McMichael, C. N. H., Pinaya, J. L. D. and Bush, M. B. (2020) Climate change and biogeographic connectivity across the Brazilian cerrado. Journal of Biogeography, 47 (2). pp. 396-407. ISSN 1365-2699 doi: 10.1111/jbi.13732

Abstract/Summary

Aim To investigate cerrado responses to glacial–interglacial climate change and the potential for connective rain forest corridors between the Atlantic Coastal Forest and Amazonian rain forest. Location The crater lake of Serra Negra (18 °S, 46 °W) in Minas Gerais, Brazil. Taxon 117 fossil pollen types, 22 non‐pollen palynomorphs were documented. Methods We recovered 7.82 m of sediment from the lake, and analysed fossil pollen at 62 depth intervals throughout the core. We derived a chronology based on radiocarbon dating with simple rate extrapolation to the base of the core. Results The c. 90,000‐year fossil record showed a trend towards cooler climates at the Last Glacial Maximum (LGM), but interstadial warming coupled with reduced evaporative stress allowed the expansion of woodlands under cool, moist conditions. Cool‐adapted trees were most abundant between c. 67,000 and 48,000 years ago. A cool cerrado‐like environment marked full glacial conditions between c. 48,000 and 34,000 years ago. The peak of the LGM between c. 34,000 and 17,000 years ago is inferred to have been dry as no sediment accumulated in the system. Main conclusions Expanded ranges of cold‐tolerant forest taxa led to establishment of a series of assemblages without modern analogue. A system characteristic of modern cerrado was rare in the history of this site. Multiple forest expansions were observed, each differing in composition. The periods of forest abundance at Serra Negra were not temporally aligned with forest expansion in the Atlantic Coastal Forest, and did not provide a continuous corridor of similar forest that connected the cerrado to the Atlantic Coastal Forest.

Altmetric Badge

Item Type Article
URI https://reading-clone.eprints-hosting.org/id/eprint/89923
Item Type Article
Refereed Yes
Divisions No Reading authors. Back catalogue items
Science > School of Archaeology, Geography and Environmental Science > Department of Geography and Environmental Science
Publisher Wiley
Download/View statistics View download statistics for this item

University Staff: Request a correction | Centaur Editors: Update this record

Search Google Scholar