Palynological analyses in the laminated sediment of Lake Holzmaar (Eifel, Germany): duration of Lateglacial and Preboreal biozones
Identifieur interne : 000E84 ( Main/Exploration ); précédent : 000E83; suivant : 000E85Palynological analyses in the laminated sediment of Lake Holzmaar (Eifel, Germany): duration of Lateglacial and Preboreal biozones
Auteurs : Suzanne Alice G. Leroy [Irlande (pays)] ; Bernd Zolitschka [Allemagne] ; Jörg F. W. Negendank [Allemagne] ; Guy Seret [Belgique]Source :
- Boreas [ 0300-9483 ] ; 2000-02.
Abstract
The laminated sediment of Lake Holzmaar (Germany) has provided a continuous varve chronology for the last 3500 varve years (vy) and beyond that a floating varve chronology back to more than 22500 vy BP. This chronology in calendar years, in combination with palynology, enables us to determine the timing and the magnitude of Lateglacial and Early Holocene environmental changes on land (from 13838 to 10930 vy BP). The palynological diagram has a mean time resolution of 27 vy between samples. This paper establishes for the first time the biozonation for Lake Holzmaar below the Laacher See Tephra. Fifteen pollen subzones grouped in four biozones are defined by cluster analysis. After a period disturbed by microturbidites, only a part of the Bølling is present. Three cold periods have been evidenced by pollen analyses: the Older Dryas (96‐vy‐long), the Younger Dryas (654‐vy‐long) and the Rammelbeek phase (237‐vy‐long). The Allerød (883‐vy‐long) is bipartite with a first Betula‐dominated period followed by a Pinus‐dominated one. The Younger Dryas is also bipartite, with first a decrease of winter temperatures along with a change to a more continental climate. It is followed by a drier phase with a second decrease in temperatures, probably this time also affecting summer temperatures. The Preboreal is 702‐yr‐long. The duration of most phases corresponds to published records, except for that of the Younger Dryas. Cluster and rate‐of‐change analyses indicate a sharp change in the terrestrial vegetation assemblages that may be caused by a sedimentary hiatus of erosive origin during this cold and dry period. As a result, the chronology of Holzmaar has to be revised most likely below the middle of the Younger Dryas. Comparison with the varve record of Meerfelder Maar, a neighbour maar lake, suggests adding 320 vy below 12025 vy.
Url:
DOI: 10.1111/j.1502-3885.2000.tb01200.x
Affiliations:
- Allemagne, Belgique, Irlande (pays)
- Brandebourg, Province du Brabant wallon, Région wallonne
- Louvain-la-Neuve, Potsdam
- Université catholique de Louvain
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This chronology in calendar years, in combination with palynology, enables us to determine the timing and the magnitude of Lateglacial and Early Holocene environmental changes on land (from 13838 to 10930 vy BP). The palynological diagram has a mean time resolution of 27 vy between samples. This paper establishes for the first time the biozonation for Lake Holzmaar below the Laacher See Tephra. Fifteen pollen subzones grouped in four biozones are defined by cluster analysis. After a period disturbed by microturbidites, only a part of the Bølling is present. Three cold periods have been evidenced by pollen analyses: the Older Dryas (96‐vy‐long), the Younger Dryas (654‐vy‐long) and the Rammelbeek phase (237‐vy‐long). The Allerød (883‐vy‐long) is bipartite with a first Betula‐dominated period followed by a Pinus‐dominated one. The Younger Dryas is also bipartite, with first a decrease of winter temperatures along with a change to a more continental climate. It is followed by a drier phase with a second decrease in temperatures, probably this time also affecting summer temperatures. The Preboreal is 702‐yr‐long. The duration of most phases corresponds to published records, except for that of the Younger Dryas. Cluster and rate‐of‐change analyses indicate a sharp change in the terrestrial vegetation assemblages that may be caused by a sedimentary hiatus of erosive origin during this cold and dry period. As a result, the chronology of Holzmaar has to be revised most likely below the middle of the Younger Dryas. Comparison with the varve record of Meerfelder Maar, a neighbour maar lake, suggests adding 320 vy below 12025 vy.</div></front></TEI><affiliations><list><country><li>Allemagne</li><li>Belgique</li><li>Irlande (pays)</li></country><region><li>Brandebourg</li><li>Province du Brabant wallon</li><li>Région wallonne</li></region><settlement><li>Louvain-la-Neuve</li><li>Potsdam</li></settlement><orgName><li>Université catholique de Louvain</li></orgName></list><tree><country name="Irlande (pays)"><noRegion><name sortKey="Leroy, Suzanne Alice G" sort="Leroy, Suzanne Alice G" uniqKey="Leroy S" first="Suzanne Alice G." last="Leroy">Suzanne Alice G. Leroy</name></noRegion></country><country name="Allemagne"><region name="Brandebourg"><name sortKey="Zolitschka, Bernd" sort="Zolitschka, Bernd" uniqKey="Zolitschka B" first="Bernd" last="Zolitschka">Bernd Zolitschka</name></region><name sortKey="Negendank, Jorg F W" sort="Negendank, Jorg F W" uniqKey="Negendank J" first="Jörg F. W." last="Negendank">Jörg F. W. Negendank</name></country><country name="Belgique"><region name="Région wallonne"><name sortKey="Seret, Guy" sort="Seret, Guy" uniqKey="Seret G" first="Guy" last="Seret">Guy Seret</name></region></country></tree></affiliations></record>Pour manipuler ce document sous Unix (Dilib)
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