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	<journal>
		<journal_title>Climate of the Past</journal_title>
		<journal_url>www.clim-past.net</journal_url>
		<issn>1814-9324</issn>
		<eissn>1814-9332</eissn>
		<volume_number>5</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/cp-5-725-2009</doi>
	<article_url>http://www.clim-past.net/5/725/2009/</article_url>
	<abstract_html>http://www.clim-past.net/5/725/2009/cp-5-725-2009.html</abstract_html>
	<fulltext_pdf>http://www.clim-past.net/5/725/2009/cp-5-725-2009.pdf</fulltext_pdf>
	<start_page>725</start_page>
	<end_page>767</end_page>
	<publication_date>2009-12-01</publication_date>
	<article_title content_type="html">Pollen-based biome reconstructions for Latin America at 0, 6000 and 18 000 radiocarbon years ago</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>R. Marchant</name>
			<email>rm524@york.ac.uk</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>A. Cleef</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>S. P. Harrison</name>
		</author>
		<author numeration="4" affiliations="2">
			<name>H. Hooghiemstra</name>
		</author>
		<author numeration="5" affiliations="4">
			<name>V. Markgraf</name>
		</author>
		<author numeration="6" affiliations="2">
			<name>J. van Boxel</name>
		</author>
		<author numeration="7" affiliations="5">
			<name>T. Ager</name>
		</author>
		<author numeration="8" affiliations="6">
			<name>L. Almeida</name>
		</author>
		<author numeration="9" affiliations="7">
			<name>R. Anderson</name>
		</author>
		<author numeration="10" affiliations="8">
			<name>C. Baied</name>
		</author>
		<author numeration="11" affiliations="9">
			<name>H. Behling</name>
		</author>
		<author numeration="12" affiliations="10">
			<name>J. C. Berrio</name>
		</author>
		<author numeration="13" affiliations="10">
			<name>R. Burbridge</name>
		</author>
		<author numeration="14" affiliations="11">
			<name>S. BjÃ¶rck</name>
		</author>
		<author numeration="15" affiliations="12">
			<name>R. Byrne</name>
		</author>
		<author numeration="16" affiliations="13">
			<name>M. Bush</name>
		</author>
		<author numeration="17" affiliations="2">
			<name>J. Duivenvoorden</name>
		</author>
		<author numeration="18" affiliations="14">
			<name>J. Flenley</name>
		</author>
		<author numeration="19" affiliations="15">
			<name>P. De Oliveira</name>
		</author>
		<author numeration="20" affiliations="2">
			<name>B. van Geel</name>
		</author>
		<author numeration="21" affiliations="16">
			<name>K. Graf</name>
		</author>
		<author numeration="22" affiliations="17">
			<name>W. D. Gosling</name>
		</author>
		<author numeration="23" affiliations="18">
			<name>S. Harbele</name>
		</author>
		<author numeration="24" affiliations="19">
			<name>T. van der Hammen</name>
		</author>
		<author numeration="25" affiliations="20">
			<name>B. Hansen</name>
		</author>
		<author numeration="26" affiliations="21">
			<name>S. Horn</name>
		</author>
		<author numeration="27" affiliations="22">
			<name>P. Kuhry</name>
		</author>
		<author numeration="28" affiliations="23">
			<name>M.-P. Ledru</name>
		</author>
		<author numeration="29" affiliations="24">
			<name>F. Mayle</name>
		</author>
		<author numeration="30" affiliations="25">
			<name>B. Leyden</name>
		</author>
		<author numeration="31" affiliations="26">
			<name>S. Lozano-GarcÃ­a</name>
		</author>
		<author numeration="32" affiliations="27">
			<name>A. M. Melief</name>
		</author>
		<author numeration="33" affiliations="28">
			<name>P. Moreno</name>
		</author>
		<author numeration="34" affiliations="29">
			<name>N. T. Moar</name>
		</author>
		<author numeration="35" affiliations="30">
			<name>A. Prieto</name>
		</author>
		<author numeration="36" affiliations="2">
			<name>G. van Reenen</name>
		</author>
		<author numeration="37" affiliations="31">
			<name>M. Salgado-Labouriau</name>
		</author>
		<author numeration="38" affiliations="32">
			<name>F. SchÃ¤bitz</name>
		</author>
		<author numeration="39" affiliations="33">
			<name>E. J. Schreve-Brinkman</name>
		</author>
		<author numeration="40" affiliations="34">
			<name>M. Wille</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">The York Institute for Tropical Ecosystem Dynamics (KITE), Environment Department, University of York, York, Heslington, YO10 5DD, UK</affiliation>
		<affiliation numeration="2" content_type="html">Institute for Biodiversity and Ecosystem Dynamics (IBED), Faculty of Science, University of Amsterdam, Postbus 94062, 1090 GB Amsterdam, The Netherlands</affiliation>
		<affiliation numeration="3" content_type="html">Bristol Research Initiative for the Dynamic Global Environment (BRIDGE), School of Geographical Sciences, University Road, University of Bristol, Bristol BS8 1SS, UK</affiliation>
		<affiliation numeration="4" content_type="html">INSTAAR, University of Colorado, Boulder, CO 80309, USA</affiliation>
		<affiliation numeration="5" content_type="html">USGS, National Centre, MS 970, Reston, VA 22092, USA</affiliation>
		<affiliation numeration="6" content_type="html">Laboratorio BiogeografÃ­a, Facultad de Ciencias, Universidad Nacional AutÃ³noma de MÃ©xico, Aptdo Postal 70-296, 04510 MÃ©xico D.F., Mexico</affiliation>
		<affiliation numeration="7" content_type="html">Department of Geography, University of Montana, Missoula, Montana 59812-1018, USA</affiliation>
		<affiliation numeration="8" content_type="html">Environmental Studies Program, University of Montana, Missoula Montana 59812, USA</affiliation>
		<affiliation numeration="9" content_type="html">Georg-August-UniversitÃ¤t, Albrecht-von-Haller-Institut fÃ¼r Pflanzenwissenschaften, Abteilung Palynologie und Klimadynamik, Untere KarspÃ¼le 2, 37073 GÃ¶ttingen, Germany</affiliation>
		<affiliation numeration="10" content_type="html">Department of Geography, University Road, University of Leicester, LE1 7RH, UK</affiliation>
		<affiliation numeration="11" content_type="html">Geological Institute, University of Copenhagen, Ã˜ster Volgade 10, 1350 Copenhagen, Denmark</affiliation>
		<affiliation numeration="12" content_type="html">Department of Geography, University of California, Berkeley, California 94720-4740, USA</affiliation>
		<affiliation numeration="13" content_type="html">Dept. of Biological Sciences, Florida Institute of Technology, 150 W. University Boulevard, Melbourne, FL 32905, USA</affiliation>
		<affiliation numeration="14" content_type="html">Department of Geography, Massey University, Palmerston, New Zealand</affiliation>
		<affiliation numeration="15" content_type="html">Instituto de Geociencias-DPE, Universidade de SÃ£o Paulo, Caixa Postal 11348, SÃ£o Paulo, SP 05422-970, Brazil</affiliation>
		<affiliation numeration="16" content_type="html">Geographisches Institut der UniversitÃ¤t, WinterthÃ¼rerstra{ÃŸ}e 190, 8057 ZÃ¼rich, Switzerland</affiliation>
		<affiliation numeration="17" content_type="html">Dept. of Earth and Environmental Sciences, CEPSA, The Open University, Walton Hall, Milton Keynes, MK7 6AA, UK</affiliation>
		<affiliation numeration="18" content_type="html">Department of Archaeology and Natural History, College of Asia and the Pacific, Australian National University, Canberra, ACT 0200, Australia</affiliation>
		<affiliation numeration="19" content_type="html">FundaciÃ³n Tropenbos Colombia, Carrera 21 # 39-35, Santafe de BogotÃ¡, Colombia</affiliation>
		<affiliation numeration="20" content_type="html">Limnological Research Centre, University of Minnesota, 220 Pillsbury Hall, 310 Pillsbury Drive, Minneapolis, MN 55455-0219, USA</affiliation>
		<affiliation numeration="21" content_type="html">Arctic Centre, University of Lapland, PL 122, 96101 Rovaniemi, Finland</affiliation>
		<affiliation numeration="22" content_type="html">Department of Geography, University of Tennessee, 408 G&amp;G Building, Knoxville, TN 37996-1420, USA</affiliation>
		<affiliation numeration="23" content_type="html">Equipe PalÃ©oenvironements, Institut des Sciences de l&apos;Evolution Institut de Recherche pour le Developement, Montpellier, France</affiliation>
		<affiliation numeration="24" content_type="html">Geography Building, Drummond Street, Edinburgh, EH8 9XP, UK</affiliation>
		<affiliation numeration="25" content_type="html">Department of Geology, University of South Florida, 4202 East Fowler Avenue, SCA 203, Tampa, FL 33620-5200, USA</affiliation>
		<affiliation numeration="26" content_type="html">Universidad Nacional AutÃ³noma de MÃ©xico, Instituto de GeologÃ­a, Aptdo Postal 70-296, 04510 MÃ©xico D.F., Mexico</affiliation>
		<affiliation numeration="27" content_type="html">2E Oosterparkstraat 163A, 1092 BE Amsterdam, The Netherlands</affiliation>
		<affiliation numeration="28" content_type="html">Facultad de Ciencias, Universidad de Chile, Casilla 653, Santiago, Chile</affiliation>
		<affiliation numeration="29" content_type="html">Botany Division, D.S.I.R., Private Bag, Christchurch, New Zealand</affiliation>
		<affiliation numeration="30" content_type="html">Laboratorio de Palinologia, National Universidad Mar del Plata, Dept. de Biologia, Funes 3250, 7600 Mar del Plata, Argentina</affiliation>
		<affiliation numeration="31" content_type="html">Inst. de Geociencias, FundaÃ§Ã£o Universidade do Brazilia, Campus Universitario, Asa Norte, 0910-900, DF Brazilia, Brazil</affiliation>
		<affiliation numeration="32" content_type="html">Geographisches Institut, UniversitÃ¤t Bamberg, Am Kranen 1, 96045 Bamberg, Germany</affiliation>
		<affiliation numeration="33" content_type="html">Welbergsweg 8, 7495 SZ Delden, The Netherlands</affiliation>
		<affiliation numeration="34" content_type="html">Geographisches Institut, UniversitÃ¤t Essen, Essen, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">The biomisation method is used to reconstruct Latin American vegetation at
6000&amp;plusmn;500 and 18 000&amp;plusmn;1000 radiocarbon years before present
(&lt;sup&gt;14&lt;/sup&gt;C yr BP) from pollen data. Tests using modern pollen data from 381
samples derived from 287 locations broadly reproduce potential natural
vegetation. The strong temperature gradient associated with the Andes is
recorded by a transition from high altitude cool grass/shrubland and cool
mixed forest to mid-altitude cool temperate rain forest, to tropical dry,
seasonal and rain forest at low altitudes. Reconstructed biomes from a
number of sites do not match the potential vegetation due to local factors
such as human impact, methodological artefacts and mechanisms of pollen
representivity of the parent vegetation.

&lt;br&gt;&lt;br&gt;

At 6000&amp;plusmn;500 &lt;sup&gt;14&lt;/sup&gt;C yr BP 255 samples are analysed from 127 sites.
Differences between the modern and the 6000&amp;plusmn;500 &lt;sup&gt;14&lt;/sup&gt;C yr BP
reconstruction are comparatively small; change relative to the modern
reconstruction are mainly to biomes characteristic of drier climate in the
north of the region with a slight more mesic shift in the south. Cool
temperate rain forest remains dominant in western South America. In
northwestern South America a number of sites record transitions from
tropical seasonal forest to tropical dry forest and tropical rain forest to
tropical seasonal forest. Sites in Central America show a change in biome
assignment, but to more mesic vegetation, indicative of greater plant
available moisture, e.g. on the YucatÃ¡n peninsula sites record warm
evergreen forest, replacing tropical dry forest and warm mixed forest
presently recorded.

&lt;br&gt;&lt;br&gt;

At 18 000&amp;plusmn;1000 &lt;sup&gt;14&lt;/sup&gt;C yr BP 61 samples from 34 sites record
vegetation reflecting a generally cool and dry environment. Cool grass/shrubland
is prevalent in southeast Brazil whereas Amazonian sites record
tropical dry forest, warm temperate rain forest and tropical seasonal
forest. Southernmost South America is dominated by cool grass/shrubland, a
single site retains cool temperate rain forest indicating that forest was
present at some locations at the LGM. Some sites in Central Mexico and
lowland Colombia remain unchanged in the biome assignments of warm mixed
forest and tropical dry forest respectively, although the affinities that
these sites have to different biomes do change between 18 000&amp;plusmn;1000 
 &lt;sup&gt;14&lt;/sup&gt;C yr BP and present. The &quot;unresponsive&quot; nature of these sites results
from their location and the impact of local edaphic influence.</abstract>
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</article>

