Note to users. If you're seeing this message, it means that your browser cannot find this page's style/presentation instructions -- or possibly that you are using a browser that does not support current Web standards. Find out more about why this message is appearing, and what you can do to make your experience of our site the best it can be.


Science 22 December 2000:
Vol. 290. no. 5500, pp. 2291 - 2294
DOI: 10.1126/science.290.5500.2291

Reports

Millennial-Scale Dynamics of Southern Amazonian Rain Forests

Francis E. Mayle,1* Rachel Burbridge,1 Timothy J. Killeen23

Amazonian rain forest-savanna boundaries are highly sensitive to climatic change and may also play an important role in rain forest speciation. However, their dynamics over millennial time scales are poorly understood. Here, we present late Quaternary pollen records from the southern margin of Amazonia, which show that the humid evergreen rain forests of eastern Bolivia have been expanding southward over the past 3000 years and that their present-day limit represents the southernmost extent of Amazonian rain forest over at least the past 50,000 years. This rain forest expansion is attributed to increased seasonal latitudinal migration of the Intertropical Convergence Zone, which can in turn be explained by Milankovitch astronomic forcing.

1 Department of Geography, University of Leicester, Leicester LE1 7RH, UK.
2 Center for Applied Biodiversity Science, Conservation International, 2501 M Street, NW, Suite 200, Washington, DC 20037, USA.
3 Museo de Historia Natural "Noel Kempff Mercado," Avenida Irala 565, Casilla 2489, Santa Cruz de la Sierra, Santa Cruz, Bolivia.
*   To whom correspondence should be addressed. E-mail: fem1{at}leicester.ac.uk


Read the Full Text



THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
Quantitative estimates of glacial and Holocene temperature and precipitation change in lowland Amazonian Bolivia.
S. W. Punyasena, F. E. Mayle, and J. C. McElwain (2008)
Geology 36, 667-670
   Abstract »    Full Text »    PDF »
The influence of changes in orbital parameters over South American climate using the CPTEC AGCM: simulation of climate during the mid Holocene.
M. Luciene Dias de Melo and J. A. Marengo (2008)
The Holocene 18, 501-516
   Abstract »    PDF »
Impact of a drier Early-Mid-Holocene climate upon Amazonian forests.
F. E Mayle and M. J Power (2008)
Phil Trans R Soc B 363, 1829-1838
   Abstract »    Full Text »    PDF »
Holocene fire and occupation in Amazonia: records from two lake districts.
M. B Bush, M. R Silman, M. B de Toledo, C. Listopad, W. D Gosling, C. Williams, P. E de Oliveira, and C. Krisel (2007)
Phil Trans R Soc B 362, 209-218
   Abstract »    Full Text »    PDF »
Long-term forest-savannah dynamics in the Bolivian Amazon: implications for conservation.
F. E Mayle, R. P Langstroth, R. A Fisher, and P. Meir (2007)
Phil Trans R Soc B 362, 291-307
   Abstract »    Full Text »    PDF »
48,000 Years of Climate and Forest Change in a Biodiversity Hot Spot.
M. B. Bush, M. R. Silman, and D. H. Urrego (2004)
Science 303, 827-829
   Abstract »    Full Text »    PDF »
Quaternary pollen analysis: recent progress in palaeoecology and palaeoclimatology.
H. Seppa and K.D. Bennett (2003)
Progress in Physical Geography 27, 548-579
   Abstract »    PDF »
REPLY.
P. Mourguiart and M.-P. Ledru (2003)
Geology 31, e27
   Full Text »    PDF »
A simple and effective methodology for sampling modern pollen rain in tropical environments.
W. D. Gosling, F. E. Mayle, T. J. Killeen, M. Siles, L. Sanchez, and S. Boreham (2003)
The Holocene 13, 613-618
   Abstract »    PDF »
Last Glacial Maximum in an Andean cloud forest environment (Eastern Cordillera, Bolivia): Comment and Reply: REPLY.
P. Mourguiart and M.-P. Ledru (2003)
Geology 31, e27
   Full Text »    PDF »
El Nino-Like Pattern in Ice Age Tropical Pacific Sea Surface Temperature.
A. Koutavas, J. Lynch-Stieglitz, T. M. Marchitto Jr., and J. P. Sachs (2002)
Science 297, 226-230
   Abstract »    Full Text »    PDF »
Response of tropical vegetation to Paleogene warming.
(2002)
Paleobiology 28, 222-243
Southward Migration of the Intertropical Convergence Zone Through the Holocene.
G. H. Haug, K. A. Hughen, D. M. Sigman, L. C. Peterson, and U. Rohl (2001)
Science 293, 1304-1308
   Abstract »    Full Text »    PDF »
Isotopic evidence for cooler and drier conditions in the tropical Andes during the last glacial stage.
G. Mora and L. M. Pratt (2001)
Geology 29, 519-522
   Abstract »    Full Text »    PDF »



To Advertise     Find Products


Science. ISSN 0036-8075 (print), 1095-9203 (online)