AustralieFrV1, PascalFrancis, Curation, bibRecord, 005F27

Response of aeolian systems to Holocene climatic and hydrologic changes on the northern margin of the Sahara : a high-resolution record from the Chott Rharsa basin, Tunisia

Identifieur interne : 005F27 ( PascalFrancis/Curation ); précédent : 005F26; suivant : 005F28

Response of aeolian systems to Holocene climatic and hydrologic changes on the northern margin of the Sahara : a high-resolution record from the Chott Rharsa basin, Tunisia

Auteurs : C. Swezey [États-Unis] ; N. Lancaster [États-Unis] ; G. Kocurek [États-Unis] ; M. Deynoux [France] ; M. Blum [États-Unis] ; D. Prices [Australie] ; J.-C. Pion [France]

Source :

The Holocene : (Sevenoaks) [ 0959-6836 ] ; 1999.

RBID : Francis:525-99-12250

Descripteurs français

Pascal (Inist)
- Afrique, Sahara, Tunisie, Géologie et climatologie, Géomorphologie, Sédimentologie, Pléistocène, Holocène, Chott Rharsa.
Wicri :
- geographic : Tunisie.
- topic : Géomorphologie, Sédimentologie.

English descriptors

KwdEn :
- Africa, Geology and climatology, Geomorphology, Holocene, Pleistocene, Sahara, Sedimentology, Tunisia.

Abstract

Four millennial-scale latest Pleistocene to Holocene climatic cycles are recorded by aeolian-lacustrine strata along the southern margin of Chott Rharsa, a playa situated within an active tectonic basin along the northern margin of the Sahara Desert in Tunisia. Cycles are characterized by (I) a humid phase of dunefield stabilization and high lake levels, and (2) an arid phase of playa desiccation and deflation with dunefield construction. The cycles overall define a progressive drying trend and correlate well with a detailed chronology from Morocco and with the Sahara region in general for the latest Pleistocene and early Holocene. Climatic events appear more regional in nature for the later Holocene. An isolated outcrop of aeolian deposits dated at >86 ka BP argues for records of older cycles in the Chott Rharsa Basin that were subsequently removed by long-term deflation in the area.

A01	`01`	`1`		`@0 0959-6836`
A03		`1`		`@0 Holocene : (Sevenoaks)`
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A08	`01`	`1`	`ENG`	`@1 Response of aeolian systems to Holocene climatic and hydrologic changes on the northern margin of the Sahara : a high-resolution record from the Chott Rharsa basin, Tunisia`
A11	`01`	`1`		`@1 SWEZEY (C.)`
A11	`02`	`1`		`@1 LANCASTER (N.)`
A11	`03`	`1`		`@1 KOCUREK (G.)`
A11	`04`	`1`		`@1 DEYNOUX (M.)`
A11	`05`	`1`		`@1 BLUM (M.)`
A11	`06`	`1`		`@1 PRICES (D.)`
A11	`07`	`1`		`@1 PION (J.-C.)`
A14	`01`			`@1 Department of Geological Sciences, University of Texas @2 Austin, Texas 78712 @3 USA @Z 1 aut. @Z 3 aut.`
A14	`02`			`@1 Desert Research Institute, University of Nevada @2 Reno, Nevada 89506 @3 USA @Z 2 aut.`
A14	`03`			`@1 CNRS-Centre de Géochimie de la Surface, Université Louis Pasteur @2 Strasbourg 67084 @3 FRA @Z 4 aut.`
A14	`04`			`@1 Department of Geosciences, University of Nebraska @2 Lincoln, Nebraska 68588 @3 USA @Z 5 aut.`
A14	`05`			`@1 Thermoluminescence Dating Laboratory, School of Geosciences, University of Wollongong @2 Wollongong, NSW 2522 @3 AUS @Z 6 aut.`
A14	`06`			`@1 ORSTOM-GSTS, Université Louis Pasteur @2 Strasbourg 67084 @3 FRA @Z 7 aut.`
A20				`@1 141-147`
A21				`@1 1999`
A23	`01`			`@0 ENG`
A43	`01`			`@1 INIST @2 25948 @5 354000083411670020`
A44				`@0 0000 @1 © 1999 INIST-CNRS. All rights reserved.`
A45				`@0 37 ref.`
A47	`01`	`1`		`@0 525-99-12250`
A60				`@1 P`
A61				`@0 A`
A64	`01`	`1`		`@0 The Holocene : (Sevenoaks)`
A66	`01`			`@0 GBR`
A68	`01`	`1`	`FRE`	`@1 La réponse des systèmes éoliens aux modifications climatiques et hydrologiques de la frange nord du Sahara : des données à haute résolution du bassin de Chott Rharsa, Tunisie`
C01	`01`		`ENG`	@0 Four millennial-scale latest Pleistocene to Holocene climatic cycles are recorded by aeolian-lacustrine strata along the southern margin of Chott Rharsa, a playa situated within an active tectonic basin along the northern margin of the Sahara Desert in Tunisia. Cycles are characterized by (I) a humid phase of dunefield stabilization and high lake levels, and (2) an arid phase of playa desiccation and deflation with dunefield construction. The cycles overall define a progressive drying trend and correlate well with a detailed chronology from Morocco and with the Sahara region in general for the latest Pleistocene and early Holocene. Climatic events appear more regional in nature for the later Holocene. An isolated outcrop of aeolian deposits dated at >86 ka BP argues for records of older cycles in the Chott Rharsa Basin that were subsequently removed by long-term deflation in the area.
C02	`01`	`H`		`@0 52526 @1 II`
C02	`02`	`H`		`@0 525`
C03	`01`	`H`	`FRE`	`@0 Afrique @2 NG @5 01`
C03	`01`	`H`	`ENG`	`@0 Africa @2 NG @5 01`
C03	`02`	`H`	`FRE`	`@0 Sahara @2 NG @5 02`
C03	`02`	`H`	`ENG`	`@0 Sahara @2 NG @5 02`
C03	`03`	`H`	`FRE`	`@0 Tunisie @2 NG @5 03`
C03	`03`	`H`	`ENG`	`@0 Tunisia @2 NG @5 03`
C03	`04`	`H`	`FRE`	`@0 Géologie et climatologie @5 04`
C03	`04`	`H`	`ENG`	`@0 Geology and climatology @5 04`
C03	`05`	`H`	`FRE`	`@0 Géomorphologie @5 05`
C03	`05`	`H`	`ENG`	`@0 Geomorphology @5 05`
C03	`06`	`H`	`FRE`	`@0 Sédimentologie @5 06`
C03	`06`	`H`	`ENG`	`@0 Sedimentology @5 06`
C03	`07`	`H`	`FRE`	`@0 Pléistocène @2 NI @5 08`
C03	`07`	`H`	`ENG`	`@0 Pleistocene @2 NI @5 08`
C03	`08`	`H`	`FRE`	`@0 Holocène @2 NI @5 09`
C03	`08`	`H`	`ENG`	`@0 Holocene @2 NI @5 09`
C03	`09`	`H`	`FRE`	`@0 Chott Rharsa @2 NG @2 FS @4 INC @5 31`
N21				`@1 277`

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Le document en format XML

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<author><name sortKey="Swezey, C" sort="Swezey, C" uniqKey="Swezey C" first="C." last="Swezey">C. Swezey</name>
<affiliation wicri:level="1"><inist:fA14 i1="01"><s1>Department of Geological Sciences, University of Texas</s1>
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<author><name sortKey="Lancaster, N" sort="Lancaster, N" uniqKey="Lancaster N" first="N." last="Lancaster">N. Lancaster</name>
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<author><name sortKey="Kocurek, G" sort="Kocurek, G" uniqKey="Kocurek G" first="G." last="Kocurek">G. Kocurek</name>
<affiliation wicri:level="1"><inist:fA14 i1="01"><s1>Department of Geological Sciences, University of Texas</s1>
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<author><name sortKey="Deynoux, M" sort="Deynoux, M" uniqKey="Deynoux M" first="M." last="Deynoux">M. Deynoux</name>
<affiliation wicri:level="1"><inist:fA14 i1="03"><s1>CNRS-Centre de Géochimie de la Surface, Université Louis Pasteur</s1>
<s2>Strasbourg 67084</s2>
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<sZ>4 aut.</sZ>
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<author><name sortKey="Blum, M" sort="Blum, M" uniqKey="Blum M" first="M." last="Blum">M. Blum</name>
<affiliation wicri:level="1"><inist:fA14 i1="04"><s1>Department of Geosciences, University of Nebraska</s1>
<s2>Lincoln, Nebraska 68588</s2>
<s3>USA</s3>
<sZ>5 aut.</sZ>
</inist:fA14>
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<author><name sortKey="Prices, D" sort="Prices, D" uniqKey="Prices D" first="D." last="Prices">D. Prices</name>
<affiliation wicri:level="1"><inist:fA14 i1="05"><s1>Thermoluminescence Dating Laboratory, School of Geosciences, University of Wollongong</s1>
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<profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Africa</term>
<term>Geology and climatology</term>
<term>Geomorphology</term>
<term>Holocene</term>
<term>Pleistocene</term>
<term>Sahara</term>
<term>Sedimentology</term>
<term>Tunisia</term>
</keywords>
<keywords scheme="Pascal" xml:lang="fr"><term>Afrique</term>
<term>Sahara</term>
<term>Tunisie</term>
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<front><div type="abstract" xml:lang="en">Four millennial-scale latest Pleistocene to Holocene climatic cycles are recorded by aeolian-lacustrine strata along the southern margin of Chott Rharsa, a playa situated within an active tectonic basin along the northern margin of the Sahara Desert in Tunisia. Cycles are characterized by (I) a humid phase of dunefield stabilization and high lake levels, and (2) an arid phase of playa desiccation and deflation with dunefield construction. The cycles overall define a progressive drying trend and correlate well with a detailed chronology from Morocco and with the Sahara region in general for the latest Pleistocene and early Holocene. Climatic events appear more regional in nature for the later Holocene. An isolated outcrop of aeolian deposits dated at >86 ka BP argues for records of older cycles in the Chott Rharsa Basin that were subsequently removed by long-term deflation in the area.</div>
</front>
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<fA11 i1="01" i2="1"><s1>SWEZEY (C.)</s1>
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<fA11 i1="07" i2="1"><s1>PION (J.-C.)</s1>
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<fA14 i1="01"><s1>Department of Geological Sciences, University of Texas</s1>
<s2>Austin, Texas 78712</s2>
<s3>USA</s3>
<sZ>1 aut.</sZ>
<sZ>3 aut.</sZ>
</fA14>
<fA14 i1="02"><s1>Desert Research Institute, University of Nevada</s1>
<s2>Reno, Nevada 89506</s2>
<s3>USA</s3>
<sZ>2 aut.</sZ>
</fA14>
<fA14 i1="03"><s1>CNRS-Centre de Géochimie de la Surface, Université Louis Pasteur</s1>
<s2>Strasbourg 67084</s2>
<s3>FRA</s3>
<sZ>4 aut.</sZ>
</fA14>
<fA14 i1="04"><s1>Department of Geosciences, University of Nebraska</s1>
<s2>Lincoln, Nebraska 68588</s2>
<s3>USA</s3>
<sZ>5 aut.</sZ>
</fA14>
<fA14 i1="05"><s1>Thermoluminescence Dating Laboratory, School of Geosciences, University of Wollongong</s1>
<s2>Wollongong, NSW 2522</s2>
<s3>AUS</s3>
<sZ>6 aut.</sZ>
</fA14>
<fA14 i1="06"><s1>ORSTOM-GSTS, Université Louis Pasteur</s1>
<s2>Strasbourg 67084</s2>
<s3>FRA</s3>
<sZ>7 aut.</sZ>
</fA14>
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</fA20>
<fA21><s1>1999</s1>
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<s5>354000083411670020</s5>
</fA43>
<fA44><s0>0000</s0>
<s1>© 1999 INIST-CNRS. All rights reserved.</s1>
</fA44>
<fA45><s0>37 ref.</s0>
</fA45>
<fA47 i1="01" i2="1"><s0>525-99-12250</s0>
</fA47>
<fA60><s1>P</s1>
</fA60>
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</fA61>
<fA64 i1="01" i2="1"><s0>The Holocene : (Sevenoaks)</s0>
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<fA66 i1="01"><s0>GBR</s0>
</fA66>
<fA68 i1="01" i2="1" l="FRE"><s1>La réponse des systèmes éoliens aux modifications climatiques et hydrologiques de la frange nord du Sahara : des données à haute résolution du bassin de Chott Rharsa, Tunisie</s1>
</fA68>
<fC01 i1="01" l="ENG"><s0>Four millennial-scale latest Pleistocene to Holocene climatic cycles are recorded by aeolian-lacustrine strata along the southern margin of Chott Rharsa, a playa situated within an active tectonic basin along the northern margin of the Sahara Desert in Tunisia. Cycles are characterized by (I) a humid phase of dunefield stabilization and high lake levels, and (2) an arid phase of playa desiccation and deflation with dunefield construction. The cycles overall define a progressive drying trend and correlate well with a detailed chronology from Morocco and with the Sahara region in general for the latest Pleistocene and early Holocene. Climatic events appear more regional in nature for the later Holocene. An isolated outcrop of aeolian deposits dated at >86 ka BP argues for records of older cycles in the Chott Rharsa Basin that were subsequently removed by long-term deflation in the area.</s0>
</fC01>
<fC02 i1="01" i2="H"><s0>52526</s0>
<s1>II</s1>
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<fC02 i1="02" i2="H"><s0>525</s0>
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<fC03 i1="01" i2="H" l="FRE"><s0>Afrique</s0>
<s2>NG</s2>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="H" l="ENG"><s0>Africa</s0>
<s2>NG</s2>
<s5>01</s5>
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<fC03 i1="02" i2="H" l="FRE"><s0>Sahara</s0>
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<s5>02</s5>
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   |area=    AustralieFrV1
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   |texte=   Response of aeolian systems to Holocene climatic and hydrologic changes on the northern margin of the Sahara : a high-resolution record from the Chott Rharsa basin, Tunisia
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	Serveur d'exploration sur les relations entre la France et l'Australie
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Serveur d'exploration sur les relations entre la France et l'Australie

Response of aeolian systems to Holocene climatic and hydrologic changes on the northern margin of the Sahara : a high-resolution record from the Chott Rharsa basin, Tunisia

Response of aeolian systems to Holocene climatic and hydrologic changes on the northern margin of the Sahara : a high-resolution record from the Chott Rharsa basin, Tunisia

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