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Pollen‐based biome reconstruction for southern Europe and Africa 18,000 yr bp

Identifieur interne : 000B70 ( Istex/Corpus ); précédent : 000B69; suivant : 000B71

Pollen‐based biome reconstruction for southern Europe and Africa 18,000 yr bp

Auteurs : H. Elenga ; O. Peyron ; R. Bonnefille ; D. Jolly ; R. Cheddadi ; J. Guiot ; V. Andrieu ; S. Bottema ; G. Buchet ; J. De Beaulieu ; A. C. Hamilton ; J. Maley ; R. Marchant ; R. Perez-Obiol ; M. Reille ; G. Riollet ; L. Scott ; H. Straka ; D. Taylor ; E. Van Campo ; A. Vincens ; F. Laarif ; H. Jonson

Source :

RBID : ISTEX:D536AAA58FA621C362DCC6C5E278EC116EF0AF7E

English descriptors

Abstract

Pollen data from 18,000 14C yr bp were compiled in order to reconstruct biome distributions at the last glacial maximum in southern Europe and Africa. Biome reconstructions were made using the objective biomization method applied to pollen counts using a complete list of dryland taxa wherever possible. Consistent and major differences from present‐day biomes are shown. Forest and xerophytic woods/scrub were replaced by steppe, both in the Mediterranean region and in southern Africa, except in south‐western Cape Province where fynbos (xerophytic scrub) persisted. Sites in the tropical highlands, characterized today by evergreen forest, were dominated by steppe and/or xerophytic vegetation (cf. today’s Ericaceous belt and Afroalpine grassland) at the last glacial maximum. Available data from the tropical lowlands are sparse but suggest that the modern tropical rain forest was largely replaced by tropical seasonal forest while the modern seasonal or dry forests were encroached on by savanna or steppe. Montane forest elements descended to lower elevations than today.

Url:
DOI: 10.1046/j.1365-2699.2000.00430.x

Links to Exploration step

ISTEX:D536AAA58FA621C362DCC6C5E278EC116EF0AF7E

Le document en format XML

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<div type="abstract" xml:lang="en">Pollen data from 18,000 14C yr bp were compiled in order to reconstruct biome distributions at the last glacial maximum in southern Europe and Africa. Biome reconstructions were made using the objective biomization method applied to pollen counts using a complete list of dryland taxa wherever possible. Consistent and major differences from present‐day biomes are shown. Forest and xerophytic woods/scrub were replaced by steppe, both in the Mediterranean region and in southern Africa, except in south‐western Cape Province where fynbos (xerophytic scrub) persisted. Sites in the tropical highlands, characterized today by evergreen forest, were dominated by steppe and/or xerophytic vegetation (cf. today’s Ericaceous belt and Afroalpine grassland) at the last glacial maximum. Available data from the tropical lowlands are sparse but suggest that the modern tropical rain forest was largely replaced by tropical seasonal forest while the modern seasonal or dry forests were encroached on by savanna or steppe. Montane forest elements descended to lower elevations than today.</div>
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<json:string>European Pollen Database, Place de la République, 13200 Arles, France,</json:string>
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<name>V. Andrieu</name>
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<name>S. Bottema</name>
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<name>J. Maley</name>
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<name>R. Perez‐Obiol</name>
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<name>M. Reille</name>
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<name>A. Vincens</name>
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<name>F. Laarif</name>
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<name>H. Jonson</name>
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<value>Pollen data</value>
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<json:item>
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<json:string>eng</json:string>
</lang>
<value>plant functional types</value>
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<lang>
<json:string>eng</json:string>
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<value>biomes</value>
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<json:string>eng</json:string>
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<value>vegetation changes</value>
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<json:string>eng</json:string>
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<value>Europe</value>
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<value>Africa</value>
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<value>last glacial maximum</value>
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<abstract>Pollen data from 18,000 14C yr bp were compiled in order to reconstruct biome distributions at the last glacial maximum in southern Europe and Africa. Biome reconstructions were made using the objective biomization method applied to pollen counts using a complete list of dryland taxa wherever possible. Consistent and major differences from present‐day biomes are shown. Forest and xerophytic woods/scrub were replaced by steppe, both in the Mediterranean region and in southern Africa, except in south‐western Cape Province where fynbos (xerophytic scrub) persisted. Sites in the tropical highlands, characterized today by evergreen forest, were dominated by steppe and/or xerophytic vegetation (cf. today’s Ericaceous belt and Afroalpine grassland) at the last glacial maximum. Available data from the tropical lowlands are sparse but suggest that the modern tropical rain forest was largely replaced by tropical seasonal forest while the modern seasonal or dry forests were encroached on by savanna or steppe. Montane forest elements descended to lower elevations than today.</abstract>
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<title>Pollen‐based biome reconstruction for southern Europe and Africa 18,000 yr bp</title>
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<p>Pollen data from 18,000 14C yr bp were compiled in order to reconstruct biome distributions at the last glacial maximum in southern Europe and Africa. Biome reconstructions were made using the objective biomization method applied to pollen counts using a complete list of dryland taxa wherever possible. Consistent and major differences from present‐day biomes are shown. Forest and xerophytic woods/scrub were replaced by steppe, both in the Mediterranean region and in southern Africa, except in south‐western Cape Province where fynbos (xerophytic scrub) persisted. Sites in the tropical highlands, characterized today by evergreen forest, were dominated by steppe and/or xerophytic vegetation (cf. today’s Ericaceous belt and Afroalpine grassland) at the last glacial maximum. Available data from the tropical lowlands are sparse but suggest that the modern tropical rain forest was largely replaced by tropical seasonal forest while the modern seasonal or dry forests were encroached on by savanna or steppe. Montane forest elements descended to lower elevations than today.</p>
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<correspondenceTo> *Correspondence: Dr D. Jolly, Département Paléoenvironnements & Palynologie, ISEM, Case 61, Université Montpellier II, Place E. Bataillon, 34095 Montpellier cedex 5, France. E‐mail:
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<p>Pollen data from 18,000 
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<p>Sites in the tropical highlands, characterized today by evergreen forest, were dominated by steppe and/or xerophytic vegetation (cf. today’s Ericaceous belt and Afroalpine grassland) at the last glacial maximum.</p>
<p>Available data from the tropical lowlands are sparse but suggest that the modern tropical rain forest was largely replaced by tropical seasonal forest while the modern seasonal or dry forests were encroached on by savanna or steppe. Montane forest elements descended to lower elevations than today.</p>
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<abstract lang="en">Pollen data from 18,000 14C yr bp were compiled in order to reconstruct biome distributions at the last glacial maximum in southern Europe and Africa. Biome reconstructions were made using the objective biomization method applied to pollen counts using a complete list of dryland taxa wherever possible. Consistent and major differences from present‐day biomes are shown. Forest and xerophytic woods/scrub were replaced by steppe, both in the Mediterranean region and in southern Africa, except in south‐western Cape Province where fynbos (xerophytic scrub) persisted. Sites in the tropical highlands, characterized today by evergreen forest, were dominated by steppe and/or xerophytic vegetation (cf. today’s Ericaceous belt and Afroalpine grassland) at the last glacial maximum. Available data from the tropical lowlands are sparse but suggest that the modern tropical rain forest was largely replaced by tropical seasonal forest while the modern seasonal or dry forests were encroached on by savanna or steppe. Montane forest elements descended to lower elevations than today.</abstract>
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