UnivTrevesV1, PascalFrancis, Corpus, bibRecord, 001114

Reconstruction of palaeoenvironmental conditions by investigation of Holocene playa sediments in the Ebro Basin, Spain : preliminary results

Identifieur interne : 001114 ( PascalFrancis/Corpus ); précédent : 001113; suivant : 001115

Reconstruction of palaeoenvironmental conditions by investigation of Holocene playa sediments in the Ebro Basin, Spain : preliminary results

Auteurs : B. Schütt

Source :

Geomorphology : (Amsterdam) [ 0169-555X ] ; 1998.

RBID : Pascal:98-0423014

Descripteurs français

Pascal (Inist)
- Espagne, Bassin Ebre, Province Zaragoza, Carotte, Sédimentation, Holocène, Humidité, Bedrock, Altération météorique, Playa, Paléoclimat, Analyse éléments majeurs, Bilan eau, Morphodynamique.

English descriptors

KwdEn :
- Ebro Basin, Holocene, Saragossa Spain, Spain, bedrock, drill cores, humidity, landform evolution, major-element analyses, paleoclimate, playas, sedimentation, water balance, weathering.

Abstract

Endorheic basins are typical landscape elements found in several parts of the Ebro Basin, Spain. Mineralogical and geochemical analysis of sediment cores from the endorheic basins facilitates the reconstruction of local palaeoenvironmental and palaeoclimatic conditions during the Holocene. The different morphogenetic and lithological environments of the areas investigated allows one to calibrate such information. First results of the analysis of the geochemistry and mineralogy of sediments from two endorheic basins within the central Ebro Basin indicate that the climatic conditions governing sedimentation during the Holocene changed from humid and subhumid to the present subarid conditions, but was interrupted by a phase of increased humidity. The varying character of solid bedrock caused different weathering products, which are reflected in the varying geochemical and mineralogical composition of lake deposits.

Notice en format standard (ISO 2709)

Pour connaître la documentation sur le format Inist Standard.

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A09	`01`	`1`	`ENG`	`@1 Geomorphic response of mediterranean and arid areas to climate change`
A11	`01`	`1`		`@1 SCHÜTT (B.)`
A12	`01`	`1`		`@1 BERKOWICZ (Simon) @9 ed.`
A12	`02`	`1`		`@1 LAVEE (Hanoch) @9 ed.`
A12	`03`	`1`		`@1 YAIR (Aaron) @9 ed.`
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A15	`01`			`@1 Institute of Earth Science, Hebrew University of Jerusalem, Givat-Ram Campus @2 Jerusalem 91904 @3 ISR @Z 1 aut.`
A15	`02`			`@1 Laboratory of Geomorphology, Department of Geography, Bar-Ilan University @2 Ramat-Gan 52900 @3 ISR @Z 2 aut.`
A15	`03`			`@1 Department of Physical Geography, Hebrew University of Jerusalem, Givat-Ram Campas @2 Jerusalem 91904 @3 ISR @Z 3 aut.`
A18	`01`	`1`		`@1 International Geographical Union @3 INT @9 patr.`
A18	`02`	`1`		`@1 Hebrew University of Jerusalem @3 ISR @9 patr.`
A18	`03`	`1`		`@1 Bar-Ilan University @3 ISR @9 patr.`
A18	`04`	`1`		`@1 Israel Geographical Association @3 ISR @9 patr.`
A18	`05`	`1`		`@1 Israel Academy of Sciences and Humanities @2 Jerusalem @3 ISR @9 patr.`
A18	`06`	`1`		`@1 Israel Ministry of Science and of the Arts @3 ISR @9 patr.`
A18	`07`	`1`		`@1 Arid Ecosystems ResearchCentre (Hebrew University) @3 ISR @9 patr.`
A18	`08`	`1`		`@1 Jewish National Fund (Keren Kayemeth Leisrael) @3 INC @9 patr.`
A18	`09`	`1`		`@1 Commission on Geomorphology and Environmental Change @3 INC @9 patr.`
A20				`@1 273-283 @7 2`
A21				`@1 1998`
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A61				`@0 A`
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C01	`01`		`ENG`	@0 Endorheic basins are typical landscape elements found in several parts of the Ebro Basin, Spain. Mineralogical and geochemical analysis of sediment cores from the endorheic basins facilitates the reconstruction of local palaeoenvironmental and palaeoclimatic conditions during the Holocene. The different morphogenetic and lithological environments of the areas investigated allows one to calibrate such information. First results of the analysis of the geochemistry and mineralogy of sediments from two endorheic basins within the central Ebro Basin indicate that the climatic conditions governing sedimentation during the Holocene changed from humid and subhumid to the present subarid conditions, but was interrupted by a phase of increased humidity. The varying character of solid bedrock caused different weathering products, which are reflected in the varying geochemical and mineralogical composition of lake deposits.
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C03	`01`	`2`	`SPA`	`@0 España @2 NG @5 01`
C03	`02`	`2`	`FRE`	`@0 Bassin Ebre @2 NG @5 02`
C03	`02`	`2`	`ENG`	`@0 Ebro Basin @2 NG @5 02`
C03	`02`	`2`	`SPA`	`@0 Cuenca del Ebro @2 NG @5 02`
C03	`03`	`2`	`FRE`	`@0 Province Zaragoza @2 NG @5 03`
C03	`03`	`2`	`ENG`	`@0 Saragossa Spain @2 NG @5 03`
C03	`03`	`2`	`SPA`	`@0 Provincia Zaragoza @2 NG @5 03`
C03	`04`	`2`	`FRE`	`@0 Carotte @5 06`
C03	`04`	`2`	`ENG`	`@0 drill cores @5 06`
C03	`04`	`2`	`SPA`	`@0 Testigo @5 06`
C03	`05`	`2`	`FRE`	`@0 Sédimentation @5 13`
C03	`05`	`2`	`ENG`	`@0 sedimentation @5 13`
C03	`05`	`2`	`SPA`	`@0 Sedimentación @5 13`
C03	`06`	`2`	`FRE`	`@0 Holocène @2 NX @5 14`
C03	`06`	`2`	`ENG`	`@0 Holocene @2 NX @5 14`
C03	`06`	`2`	`SPA`	`@0 Holoceno @2 NX @5 14`
C03	`07`	`2`	`FRE`	`@0 Humidité @5 15`
C03	`07`	`2`	`ENG`	`@0 humidity @5 15`
C03	`07`	`2`	`SPA`	`@0 Humedad @5 15`
C03	`08`	`2`	`FRE`	`@0 Bedrock @5 16`
C03	`08`	`2`	`ENG`	`@0 bedrock @5 16`
C03	`08`	`2`	`SPA`	`@0 Roca firme @5 16`
C03	`09`	`2`	`FRE`	`@0 Altération météorique @5 17`
C03	`09`	`2`	`ENG`	`@0 weathering @5 17`
C03	`09`	`2`	`SPA`	`@0 Alteración meteórica @5 17`
C03	`10`	`2`	`FRE`	`@0 Playa @5 18`
C03	`10`	`2`	`ENG`	`@0 playas @5 18`
C03	`11`	`2`	`FRE`	`@0 Paléoclimat @5 19`
C03	`11`	`2`	`ENG`	`@0 paleoclimate @5 19`
C03	`11`	`2`	`SPA`	`@0 Paleoclima @5 19`
C03	`12`	`2`	`FRE`	`@0 Analyse éléments majeurs @5 21`
C03	`12`	`2`	`ENG`	`@0 major-element analyses @5 21`
C03	`13`	`2`	`FRE`	`@0 Bilan eau @5 22`
C03	`13`	`2`	`ENG`	`@0 water balance @5 22`
C03	`13`	`2`	`SPA`	`@0 Balance agua @5 22`
C03	`14`	`2`	`FRE`	`@0 Morphodynamique @5 23`
C03	`14`	`2`	`ENG`	`@0 landform evolution @5 23`
C03	`14`	`2`	`SPA`	`@0 Morfodinámica @5 23`
C06				`@0 ILS @0 TAS`
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C07	`01`	`2`	`SPA`	`@0 Península ibérica @2 NG`
C07	`02`	`2`	`FRE`	`@0 Europe Sud @2 NG`
C07	`02`	`2`	`ENG`	`@0 Southern Europe @2 NG`
C07	`02`	`2`	`SPA`	`@0 Europa Sur @2 NG`
C07	`03`	`2`	`FRE`	`@0 Europe`
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C07	`04`	`2`	`ENG`	`@0 Aragon Spain @2 NG`
C07	`04`	`2`	`SPA`	`@0 Aragón @2 NG`
C07	`05`	`2`	`FRE`	`@0 Quaternaire sup @2 NX`
C07	`05`	`2`	`ENG`	`@0 upper Quaternary @2 NX`
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C07	`07`	`2`	`ENG`	`@0 Cenozoic @2 NX`
C07	`07`	`2`	`SPA`	`@0 Cenozoico @2 NX`
C07	`08`	`2`	`FRE`	`@0 Phanérozoïque`
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N21				`@1 285`

A30	`01`	`1`	`ENG`	`@1 IGU-GERTEC Conference @3 ISR @4 1995-05-13`

Format Inist (serveur)

NO :	PASCAL 98-0423014 INIST
ET :	Reconstruction of palaeoenvironmental conditions by investigation of Holocene playa sediments in the Ebro Basin, Spain : preliminary results
AU :	SCHÜTT (B.); BERKOWICZ (Simon); LAVEE (Hanoch); YAIR (Aaron)
AF :	Physische Geographie, Universität Trier, FB VI-Geographie/Geowissenschaften/54286 Trier/Allemagne (1 aut.); Institute of Earth Science, Hebrew University of Jerusalem, Givat-Ram Campus/Jerusalem 91904/Israël (1 aut.); Laboratory of Geomorphology, Department of Geography, Bar-Ilan University/Ramat-Gan 52900/Israël (2 aut.); Department of Physical Geography, Hebrew University of Jerusalem, Givat-Ram Campas/Jerusalem 91904/Israël (3 aut.)
DT :	Publication en série; Congrès; Niveau analytique
SO :	Geomorphology : (Amsterdam); ISSN 0169-555X; Pays-Bas; Da. 1998; Vol. 23; No. 2-4; Pp. 273-283; Bibl. 29 ref.
LA :	Anglais
EA :	Endorheic basins are typical landscape elements found in several parts of the Ebro Basin, Spain. Mineralogical and geochemical analysis of sediment cores from the endorheic basins facilitates the reconstruction of local palaeoenvironmental and palaeoclimatic conditions during the Holocene. The different morphogenetic and lithological environments of the areas investigated allows one to calibrate such information. First results of the analysis of the geochemistry and mineralogy of sediments from two endorheic basins within the central Ebro Basin indicate that the climatic conditions governing sedimentation during the Holocene changed from humid and subhumid to the present subarid conditions, but was interrupted by a phase of increased humidity. The varying character of solid bedrock caused different weathering products, which are reflected in the varying geochemical and mineralogical composition of lake deposits.
CC :	226C02; 001E01P02
FD :	Espagne; Bassin Ebre; Province Zaragoza; Carotte; Sédimentation; Holocène; Humidité; Bedrock; Altération météorique; Playa; Paléoclimat; Analyse éléments majeurs; Bilan eau; Morphodynamique
FG :	Péninsule Ibérique; Europe Sud; Europe; Aragon; Quaternaire sup; Quaternaire; Cénozoïque; Phanérozoïque
ED :	Spain; Ebro Basin; Saragossa Spain; drill cores; sedimentation; Holocene; humidity; bedrock; weathering; playas; paleoclimate; major-element analyses; water balance; landform evolution
EG :	Iberian Peninsula; Southern Europe; Europe; Aragon Spain; upper Quaternary; Quaternary; Cenozoic; Phanerozoic
SD :	España; Cuenca del Ebro; Provincia Zaragoza; Testigo; Sedimentación; Holoceno; Humedad; Roca firme; Alteración meteórica; Paleoclima; Balance agua; Morfodinámica
LO :	INIST-21151.354000077114020130
ID :	98-0423014

Links to Exploration step

Pascal:98-0423014

Le document en format XML

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<front><div type="abstract" xml:lang="en">Endorheic basins are typical landscape elements found in several parts of the Ebro Basin, Spain. Mineralogical and geochemical analysis of sediment cores from the endorheic basins facilitates the reconstruction of local palaeoenvironmental and palaeoclimatic conditions during the Holocene. The different morphogenetic and lithological environments of the areas investigated allows one to calibrate such information. First results of the analysis of the geochemistry and mineralogy of sediments from two endorheic basins within the central Ebro Basin indicate that the climatic conditions governing sedimentation during the Holocene changed from humid and subhumid to the present subarid conditions, but was interrupted by a phase of increased humidity. The varying character of solid bedrock caused different weathering products, which are reflected in the varying geochemical and mineralogical composition of lake deposits.</div>
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<fA18 i1="08" i2="1"><s1>Jewish National Fund (Keren Kayemeth Leisrael)</s1>
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<fC01 i1="01" l="ENG"><s0>Endorheic basins are typical landscape elements found in several parts of the Ebro Basin, Spain. Mineralogical and geochemical analysis of sediment cores from the endorheic basins facilitates the reconstruction of local palaeoenvironmental and palaeoclimatic conditions during the Holocene. The different morphogenetic and lithological environments of the areas investigated allows one to calibrate such information. First results of the analysis of the geochemistry and mineralogy of sediments from two endorheic basins within the central Ebro Basin indicate that the climatic conditions governing sedimentation during the Holocene changed from humid and subhumid to the present subarid conditions, but was interrupted by a phase of increased humidity. The varying character of solid bedrock caused different weathering products, which are reflected in the varying geochemical and mineralogical composition of lake deposits.</s0>
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<fC03 i1="03" i2="2" l="ENG"><s0>Saragossa Spain</s0>
<s2>NG</s2>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="2" l="SPA"><s0>Provincia Zaragoza</s0>
<s2>NG</s2>
<s5>03</s5>
</fC03>
<fC03 i1="04" i2="2" l="FRE"><s0>Carotte</s0>
<s5>06</s5>
</fC03>
<fC03 i1="04" i2="2" l="ENG"><s0>drill cores</s0>
<s5>06</s5>
</fC03>
<fC03 i1="04" i2="2" l="SPA"><s0>Testigo</s0>
<s5>06</s5>
</fC03>
<fC03 i1="05" i2="2" l="FRE"><s0>Sédimentation</s0>
<s5>13</s5>
</fC03>
<fC03 i1="05" i2="2" l="ENG"><s0>sedimentation</s0>
<s5>13</s5>
</fC03>
<fC03 i1="05" i2="2" l="SPA"><s0>Sedimentación</s0>
<s5>13</s5>
</fC03>
<fC03 i1="06" i2="2" l="FRE"><s0>Holocène</s0>
<s2>NX</s2>
<s5>14</s5>
</fC03>
<fC03 i1="06" i2="2" l="ENG"><s0>Holocene</s0>
<s2>NX</s2>
<s5>14</s5>
</fC03>
<fC03 i1="06" i2="2" l="SPA"><s0>Holoceno</s0>
<s2>NX</s2>
<s5>14</s5>
</fC03>
<fC03 i1="07" i2="2" l="FRE"><s0>Humidité</s0>
<s5>15</s5>
</fC03>
<fC03 i1="07" i2="2" l="ENG"><s0>humidity</s0>
<s5>15</s5>
</fC03>
<fC03 i1="07" i2="2" l="SPA"><s0>Humedad</s0>
<s5>15</s5>
</fC03>
<fC03 i1="08" i2="2" l="FRE"><s0>Bedrock</s0>
<s5>16</s5>
</fC03>
<fC03 i1="08" i2="2" l="ENG"><s0>bedrock</s0>
<s5>16</s5>
</fC03>
<fC03 i1="08" i2="2" l="SPA"><s0>Roca firme</s0>
<s5>16</s5>
</fC03>
<fC03 i1="09" i2="2" l="FRE"><s0>Altération météorique</s0>
<s5>17</s5>
</fC03>
<fC03 i1="09" i2="2" l="ENG"><s0>weathering</s0>
<s5>17</s5>
</fC03>
<fC03 i1="09" i2="2" l="SPA"><s0>Alteración meteórica</s0>
<s5>17</s5>
</fC03>
<fC03 i1="10" i2="2" l="FRE"><s0>Playa</s0>
<s5>18</s5>
</fC03>
<fC03 i1="10" i2="2" l="ENG"><s0>playas</s0>
<s5>18</s5>
</fC03>
<fC03 i1="11" i2="2" l="FRE"><s0>Paléoclimat</s0>
<s5>19</s5>
</fC03>
<fC03 i1="11" i2="2" l="ENG"><s0>paleoclimate</s0>
<s5>19</s5>
</fC03>
<fC03 i1="11" i2="2" l="SPA"><s0>Paleoclima</s0>
<s5>19</s5>
</fC03>
<fC03 i1="12" i2="2" l="FRE"><s0>Analyse éléments majeurs</s0>
<s5>21</s5>
</fC03>
<fC03 i1="12" i2="2" l="ENG"><s0>major-element analyses</s0>
<s5>21</s5>
</fC03>
<fC03 i1="13" i2="2" l="FRE"><s0>Bilan eau</s0>
<s5>22</s5>
</fC03>
<fC03 i1="13" i2="2" l="ENG"><s0>water balance</s0>
<s5>22</s5>
</fC03>
<fC03 i1="13" i2="2" l="SPA"><s0>Balance agua</s0>
<s5>22</s5>
</fC03>
<fC03 i1="14" i2="2" l="FRE"><s0>Morphodynamique</s0>
<s5>23</s5>
</fC03>
<fC03 i1="14" i2="2" l="ENG"><s0>landform evolution</s0>
<s5>23</s5>
</fC03>
<fC03 i1="14" i2="2" l="SPA"><s0>Morfodinámica</s0>
<s5>23</s5>
</fC03>
<fC06><s0>ILS</s0>
<s0>TAS</s0>
</fC06>
<fC07 i1="01" i2="2" l="FRE"><s0>Péninsule Ibérique</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="01" i2="2" l="ENG"><s0>Iberian Peninsula</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="01" i2="2" l="SPA"><s0>Península ibérica</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="02" i2="2" l="FRE"><s0>Europe Sud</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="02" i2="2" l="ENG"><s0>Southern Europe</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="02" i2="2" l="SPA"><s0>Europa Sur</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="03" i2="2" l="FRE"><s0>Europe</s0>
</fC07>
<fC07 i1="03" i2="2" l="ENG"><s0>Europe</s0>
</fC07>
<fC07 i1="03" i2="2" l="SPA"><s0>Europa</s0>
</fC07>
<fC07 i1="04" i2="2" l="FRE"><s0>Aragon</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="04" i2="2" l="ENG"><s0>Aragon Spain</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="04" i2="2" l="SPA"><s0>Aragón</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="05" i2="2" l="FRE"><s0>Quaternaire sup</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="05" i2="2" l="ENG"><s0>upper Quaternary</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="05" i2="2" l="SPA"><s0>Cuaternario sup</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="06" i2="2" l="FRE"><s0>Quaternaire</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="06" i2="2" l="ENG"><s0>Quaternary</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="06" i2="2" l="SPA"><s0>Cuaternario</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="07" i2="2" l="FRE"><s0>Cénozoïque</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="07" i2="2" l="ENG"><s0>Cenozoic</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="07" i2="2" l="SPA"><s0>Cenozoico</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="08" i2="2" l="FRE"><s0>Phanérozoïque</s0>
</fC07>
<fC07 i1="08" i2="2" l="ENG"><s0>Phanerozoic</s0>
</fC07>
<fC07 i1="08" i2="2" l="SPA"><s0>Fanerozoico</s0>
</fC07>
<fN21><s1>285</s1>
</fN21>
</pA>
<pR><fA30 i1="01" i2="1" l="ENG"><s1>IGU-GERTEC Conference</s1>
<s3>ISR</s3>
<s4>1995-05-13</s4>
</fA30>
</pR>
</standard>
<server><NO>PASCAL 98-0423014 INIST</NO>
<ET>Reconstruction of palaeoenvironmental conditions by investigation of Holocene playa sediments in the Ebro Basin, Spain : preliminary results</ET>
<AU>SCHÜTT (B.); BERKOWICZ (Simon); LAVEE (Hanoch); YAIR (Aaron)</AU>
<AF>Physische Geographie, Universität Trier, FB VI-Geographie/Geowissenschaften/54286 Trier/Allemagne (1 aut.); Institute of Earth Science, Hebrew University of Jerusalem, Givat-Ram Campus/Jerusalem 91904/Israël (1 aut.); Laboratory of Geomorphology, Department of Geography, Bar-Ilan University/Ramat-Gan 52900/Israël (2 aut.); Department of Physical Geography, Hebrew University of Jerusalem, Givat-Ram Campas/Jerusalem 91904/Israël (3 aut.)</AF>
<DT>Publication en série; Congrès; Niveau analytique</DT>
<SO>Geomorphology : (Amsterdam); ISSN 0169-555X; Pays-Bas; Da. 1998; Vol. 23; No. 2-4; Pp. 273-283; Bibl. 29 ref.</SO>
<LA>Anglais</LA>
<EA>Endorheic basins are typical landscape elements found in several parts of the Ebro Basin, Spain. Mineralogical and geochemical analysis of sediment cores from the endorheic basins facilitates the reconstruction of local palaeoenvironmental and palaeoclimatic conditions during the Holocene. The different morphogenetic and lithological environments of the areas investigated allows one to calibrate such information. First results of the analysis of the geochemistry and mineralogy of sediments from two endorheic basins within the central Ebro Basin indicate that the climatic conditions governing sedimentation during the Holocene changed from humid and subhumid to the present subarid conditions, but was interrupted by a phase of increased humidity. The varying character of solid bedrock caused different weathering products, which are reflected in the varying geochemical and mineralogical composition of lake deposits.</EA>
<CC>226C02; 001E01P02</CC>
<FD>Espagne; Bassin Ebre; Province Zaragoza; Carotte; Sédimentation; Holocène; Humidité; Bedrock; Altération météorique; Playa; Paléoclimat; Analyse éléments majeurs; Bilan eau; Morphodynamique</FD>
<FG>Péninsule Ibérique; Europe Sud; Europe; Aragon; Quaternaire sup; Quaternaire; Cénozoïque; Phanérozoïque</FG>
<ED>Spain; Ebro Basin; Saragossa Spain; drill cores; sedimentation; Holocene; humidity; bedrock; weathering; playas; paleoclimate; major-element analyses; water balance; landform evolution</ED>
<EG>Iberian Peninsula; Southern Europe; Europe; Aragon Spain; upper Quaternary; Quaternary; Cenozoic; Phanerozoic</EG>
<SD>España; Cuenca del Ebro; Provincia Zaragoza; Testigo; Sedimentación; Holoceno; Humedad; Roca firme; Alteración meteórica; Paleoclima; Balance agua; Morfodinámica</SD>
<LO>INIST-21151.354000077114020130</LO>
<ID>98-0423014</ID>
</server>
</inist>
</record>

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Reconstruction of palaeoenvironmental conditions by investigation of Holocene playa sediments in the Ebro Basin, Spain : preliminary results

Reconstruction of palaeoenvironmental conditions by investigation of Holocene playa sediments in the Ebro Basin, Spain : preliminary results

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