EdenteV2, Istex, Corpus, bibRecord, 005367

Recurring Taiga forest-steppe habitats in the Carpathian Basin in the Upper Weichselian

Identifieur interne : 005367 ( Istex/Corpus ); précédent : 005366; suivant : 005368

Recurring Taiga forest-steppe habitats in the Carpathian Basin in the Upper Weichselian

Auteurs : Zita Edina Rudner ; Pál Sümegi

Source :

Quaternary International [ 1040-6182 ] ; 2001.

RBID : ISTEX:A7351CDB6AD1C1902A6B1114EC0E79F86A551D42

English descriptors

KwdEn :
- Akademiai kiado, Basin, Boreal, Carpathian, Carpathian basin, Carpinus, Cembra, Central european, Charcoal analysis, Charcoal fragments, Climatic, Climatic changes, Cryophilous species, Dobosi, Fauna, Foldtani kozlony, Foothill region, Fracture, Fracture surface, Great hungarian, Hertelendi, Hungarian loess, Hungary, July palaeotemperature, Kossuth lajos university, Krolopp, Lake sediments, Land snails, Late pleistocene, Loess, Loess layer, Macroscopic, Malacological, Malacological data, Malacothermometer method, Mesophilous, Mollusc, Mollusc fauna, Molluscan, Molluscan shells, Palaeoecological, Palaeosol, Pecsi, Picea, Pinus, Pinus cembra, Pinus sylvestris, Pinus sylvestris picea, Pleistocene, Quaternary, Quaternary research, Radiocarbon, Radiocarbon data, Relict areas, Rudner, Sediment, Snail, Southern part, Sumegi, Sumegi quaternary, Sylvestris, Temperate zone, Tokaj, Upper weichselian, Upper wurm, Vegetation, Vegetation history, Weichselian, Wurm.
Teeft :
- Akademiai kiado, Basin, Boreal, Carpathian, Carpathian basin, Carpinus, Cembra, Central european, Charcoal analysis, Charcoal fragments, Climatic, Climatic changes, Cryophilous species, Dobosi, Fauna, Foldtani kozlony, Foothill region, Fracture, Fracture surface, Great hungarian, Hertelendi, Hungarian loess, Hungary, July palaeotemperature, Kossuth lajos university, Krolopp, Lake sediments, Land snails, Late pleistocene, Loess, Loess layer, Macroscopic, Malacological, Malacological data, Malacothermometer method, Mesophilous, Mollusc, Mollusc fauna, Molluscan, Molluscan shells, Palaeoecological, Palaeosol, Pecsi, Picea, Pinus, Pinus cembra, Pinus sylvestris, Pinus sylvestris picea, Pleistocene, Quaternary, Quaternary research, Radiocarbon, Radiocarbon data, Relict areas, Rudner, Sediment, Snail, Southern part, Sumegi, Sumegi quaternary, Sylvestris, Temperate zone, Tokaj, Upper weichselian, Upper wurm, Vegetation, Vegetation history, Weichselian, Wurm.

Abstract

Abstract: Many loess profiles, some lake sediments and archaeological sites in different parts of the Carpathian Basin were analysed in respect of their geology, sedimentology, Molluscs and macro-charcoal remains. Radiocarbon dating was also carried out on charcoal remains as well as on Molluscan shells. The loess profiles prove to have been formed during the last glacial period, between ca. 70,000 and 15,000 years BP. Two well-developed and a weakly developed charcoal layer can be found at the sites dating from that period. All rest on the top of a palaeosol. On the basis of palaeoecological investigations of these charcoal layers and the Molluscs found within the loess, it is concluded that recurring boreal forest-steppe habitats characterised the Carpathian Basin, the woodlands mostly consisting of Picea trees in the North and Pinus sylvestris in the South, as well as six other arboreal species. By reference to the subsequent charcoal layers, reforestation occurred every 2000–5000 years with the same composition, although their density may have varied. These forests thus recur in the same places, after extensive forest fires. How often and why these reforestation events took place, and how much time was needed for the forests-steppes to redevelop needs further clarification.

Url:

https://api.istex.fr/document/A7351CDB6AD1C1902A6B1114EC0E79F86A551D42/fulltext/pdf

DOI: 10.1016/S1040-6182(00)00101-4

Links to Exploration step

ISTEX:A7351CDB6AD1C1902A6B1114EC0E79F86A551D42

Le document en format XML

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<abstract>Abstract: Many loess profiles, some lake sediments and archaeological sites in different parts of the Carpathian Basin were analysed in respect of their geology, sedimentology, Molluscs and macro-charcoal remains. Radiocarbon dating was also carried out on charcoal remains as well as on Molluscan shells. The loess profiles prove to have been formed during the last glacial period, between ca. 70,000 and 15,000 years BP. Two well-developed and a weakly developed charcoal layer can be found at the sites dating from that period. All rest on the top of a palaeosol. On the basis of palaeoecological investigations of these charcoal layers and the Molluscs found within the loess, it is concluded that recurring boreal forest-steppe habitats characterised the Carpathian Basin, the woodlands mostly consisting of Picea trees in the North and Pinus sylvestris in the South, as well as six other arboreal species. By reference to the subsequent charcoal layers, reforestation occurred every 2000–5000 years with the same composition, although their density may have varied. These forests thus recur in the same places, after extensive forest fires. How often and why these reforestation events took place, and how much time was needed for the forests-steppes to redevelop needs further clarification.</abstract>
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<notesStmt><note type="content">Fig. 1: Map of the Carpathian Basin, showing location of the analysed sites.</note>
<note type="content">Fig. 2: Map of the Tokaj region with the analysed sites around Kopasz-hill: (A) Analysed sites with macro-charcoal and Molluscs; (B) sites with only macro-charcoal; (C) road or track; (D) railway; (1) Bodrogkeresztúr brickyard; (3) Kereszthegy-II; (4) Kereszthegy-I; (5) Csorgókút-I; (6) Csorgókút-II; (7) Patkóbánya; (9) Terem-tető; (10) Tarcal; (11) Bodrogkeresztúr-Henye hill.</note>
<note type="content">Fig. 3: Climatic zones of the Carpathian Basin: (1) Distribution of Cf Köppen zone; (2) forest-steppe (Bs) climatic zone of Köppen; (3) sub-Carpathian and Carpathian (Df) climatic zone; (4) transition zone; (5) frequency of sub-Mediterranean climatic effects.</note>
<note type="content">Fig. 4: Vegetation zones in the Carpathian Basin: (1) Pannonian forest steppe; (2) sub-Mediterranean oak forest; (3) Central European and sub-Mediterranean mixed oak forest; (4) Balcanic oak forest; (5) Central European oak forest; (6) beech and needle-leaved forest; (7) northern limit of Tilia tomentosa distribution.</note>
<note type="content">Fig. 5: Base rocks of the soils in the Carpathian Basin: (1) sandy with gravel; (2) loessic; (3) alluvial, clayey sediment; (4) consolidate sediment, volcanic and metamorphic rocks.</note>
<note type="content">Fig. 6: SEM photomicrographs of charcoal of (1) Picea sp., longitudinal radial fracture surface, (2) Larix sp., longitudinal radial fracture surface, (3) Pinus sylvestris, longitudinal radial fracture surface, (4) Pinus cembra, longitudinal radial fracture surface, (5) Carpinus betulus, transversal fracture surface, (6) Salix sp., transversal fracture surface.</note>
<note type="content">Fig. 7: Loess sections around Kopasz-hill at Tokaj. tszfm=metres above sea level: (I) Bodrogkeresztúr I; (II) Bodrogkeresztúr II; (III) Kereszthegy-I; (IV) Kereszthegy-II; (V) Csorgókút-I; (VI) Csorgókút-II; (VII) Patkóbánya; (VIII) Terem-tető; (IX) railway-station profile; (X) Tarcal; (1) soil; (2) Tokaj upper aeolian loess layer; (3) charcoal layer; (4) Tokaj upper palaeosol; (5) Tokaj intermediate loess layer; (6) Tokaj lower palaeosol; (7) Tokaj lower loess layer.</note>
<note type="content">Table 1: Modified radiocarbon data after Willis et al. (2000), with additionsa</note>
<note type="content">Table 2:</note>
<note type="content">Table 3: Dominance of different palaeoecological Mollusca groups in the Late Pleistocene time intervals from 21 radiocarbon-dated Hungarian loess profiles. The shaded columns are the palaeosol layers</note>
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<affiliation>Geographical Research Institute, Hungarian Academy of Sciences, Budaörsi u. 43-45, H-1112 Budapest, Hungary</affiliation>
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<abstract xml:lang="en"><p>Many loess profiles, some lake sediments and archaeological sites in different parts of the Carpathian Basin were analysed in respect of their geology, sedimentology, Molluscs and macro-charcoal remains. Radiocarbon dating was also carried out on charcoal remains as well as on Molluscan shells. The loess profiles prove to have been formed during the last glacial period, between ca. 70,000 and 15,000 years BP. Two well-developed and a weakly developed charcoal layer can be found at the sites dating from that period. All rest on the top of a palaeosol. On the basis of palaeoecological investigations of these charcoal layers and the Molluscs found within the loess, it is concluded that recurring boreal forest-steppe habitats characterised the Carpathian Basin, the woodlands mostly consisting of Picea trees in the North and Pinus sylvestris in the South, as well as six other arboreal species. By reference to the subsequent charcoal layers, reforestation occurred every 2000–5000 years with the same composition, although their density may have varied. These forests thus recur in the same places, after extensive forest fires. How often and why these reforestation events took place, and how much time was needed for the forests-steppes to redevelop needs further clarification.</p>
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<head><ce:title>Recurring Taiga forest-steppe habitats in the Carpathian Basin in the Upper Weichselian</ce:title>
<ce:author-group><ce:author><ce:given-name>Zita Edina</ce:given-name>
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<ce:abstract><ce:section-title>Abstract</ce:section-title>
<ce:abstract-sec><ce:simple-para>Many loess profiles, some lake sediments and archaeological sites in different parts of the Carpathian Basin were analysed in respect of their geology, sedimentology, Molluscs and macro-charcoal remains. Radiocarbon dating was also carried out on charcoal remains as well as on Molluscan shells. The loess profiles prove to have been formed during the last glacial period, between ca. 70,000 and 15,000 years BP. Two well-developed and a weakly developed charcoal layer can be found at the sites dating from that period. All rest on the top of a palaeosol. On the basis of palaeoecological investigations of these charcoal layers and the Molluscs found within the loess, it is concluded that recurring boreal forest-steppe habitats characterised the Carpathian Basin, the woodlands mostly consisting of <ce:italic>Picea</ce:italic>
 trees in the North and <ce:italic>Pinus sylvestris</ce:italic>
 in the South, as well as six other arboreal species. By reference to the subsequent charcoal layers, reforestation occurred every 2000–5000 years with the same composition, although their density may have varied. These forests thus recur in the same places, after extensive forest fires. How often and why these reforestation events took place, and how much time was needed for the forests-steppes to redevelop needs further clarification.</ce:simple-para>
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<abstract lang="en">Abstract: Many loess profiles, some lake sediments and archaeological sites in different parts of the Carpathian Basin were analysed in respect of their geology, sedimentology, Molluscs and macro-charcoal remains. Radiocarbon dating was also carried out on charcoal remains as well as on Molluscan shells. The loess profiles prove to have been formed during the last glacial period, between ca. 70,000 and 15,000 years BP. Two well-developed and a weakly developed charcoal layer can be found at the sites dating from that period. All rest on the top of a palaeosol. On the basis of palaeoecological investigations of these charcoal layers and the Molluscs found within the loess, it is concluded that recurring boreal forest-steppe habitats characterised the Carpathian Basin, the woodlands mostly consisting of Picea trees in the North and Pinus sylvestris in the South, as well as six other arboreal species. By reference to the subsequent charcoal layers, reforestation occurred every 2000–5000 years with the same composition, although their density may have varied. These forests thus recur in the same places, after extensive forest fires. How often and why these reforestation events took place, and how much time was needed for the forests-steppes to redevelop needs further clarification.</abstract>
<note type="content">Fig. 1: Map of the Carpathian Basin, showing location of the analysed sites.</note>
<note type="content">Fig. 2: Map of the Tokaj region with the analysed sites around Kopasz-hill: (A) Analysed sites with macro-charcoal and Molluscs; (B) sites with only macro-charcoal; (C) road or track; (D) railway; (1) Bodrogkeresztúr brickyard; (3) Kereszthegy-II; (4) Kereszthegy-I; (5) Csorgókút-I; (6) Csorgókút-II; (7) Patkóbánya; (9) Terem-tető; (10) Tarcal; (11) Bodrogkeresztúr-Henye hill.</note>
<note type="content">Fig. 3: Climatic zones of the Carpathian Basin: (1) Distribution of Cf Köppen zone; (2) forest-steppe (Bs) climatic zone of Köppen; (3) sub-Carpathian and Carpathian (Df) climatic zone; (4) transition zone; (5) frequency of sub-Mediterranean climatic effects.</note>
<note type="content">Fig. 4: Vegetation zones in the Carpathian Basin: (1) Pannonian forest steppe; (2) sub-Mediterranean oak forest; (3) Central European and sub-Mediterranean mixed oak forest; (4) Balcanic oak forest; (5) Central European oak forest; (6) beech and needle-leaved forest; (7) northern limit of Tilia tomentosa distribution.</note>
<note type="content">Fig. 5: Base rocks of the soils in the Carpathian Basin: (1) sandy with gravel; (2) loessic; (3) alluvial, clayey sediment; (4) consolidate sediment, volcanic and metamorphic rocks.</note>
<note type="content">Fig. 6: SEM photomicrographs of charcoal of (1) Picea sp., longitudinal radial fracture surface, (2) Larix sp., longitudinal radial fracture surface, (3) Pinus sylvestris, longitudinal radial fracture surface, (4) Pinus cembra, longitudinal radial fracture surface, (5) Carpinus betulus, transversal fracture surface, (6) Salix sp., transversal fracture surface.</note>
<note type="content">Fig. 7: Loess sections around Kopasz-hill at Tokaj. tszfm=metres above sea level: (I) Bodrogkeresztúr I; (II) Bodrogkeresztúr II; (III) Kereszthegy-I; (IV) Kereszthegy-II; (V) Csorgókút-I; (VI) Csorgókút-II; (VII) Patkóbánya; (VIII) Terem-tető; (IX) railway-station profile; (X) Tarcal; (1) soil; (2) Tokaj upper aeolian loess layer; (3) charcoal layer; (4) Tokaj upper palaeosol; (5) Tokaj intermediate loess layer; (6) Tokaj lower palaeosol; (7) Tokaj lower loess layer.</note>
<note type="content">Table 1: Modified radiocarbon data after Willis et al. (2000), with additionsa</note>
<note type="content">Table 2: </note>
<note type="content">Table 3: Dominance of different palaeoecological Mollusca groups in the Late Pleistocene time intervals from 21 radiocarbon-dated Hungarian loess profiles. The shaded columns are the palaeosol layers</note>
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Recurring Taiga forest-steppe habitats in the Carpathian Basin in the Upper Weichselian

Recurring Taiga forest-steppe habitats in the Carpathian Basin in the Upper Weichselian

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