Danube loess stratigraphy - Towards a pan-European loess stratigraphic model
The Danube River drainage basin is the second largest river catchment in Europe and contains a significant and extensive region of thick loess deposits that preserve a record of a wide variety of recent and past environments. Indeed, the Danube River and tributaries may themselves be responsible for...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Slobodan B Markovic [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2015 |
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| Systematik: |
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| Übergeordnetes Werk: |
Enthalten in: Earth science reviews - Amsterdam [u.a.] : Elsevier, 1966, 148(2015), Seite 228 |
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| Übergeordnetes Werk: |
volume:148 ; year:2015 ; pages:228 |
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| 520 | |a The Danube River drainage basin is the second largest river catchment in Europe and contains a significant and extensive region of thick loess deposits that preserve a record of a wide variety of recent and past environments. Indeed, the Danube River and tributaries may themselves be responsible for the transportation of large volumes of silt that ultimately drive loess formation in the middle and lower reaches of this large catchment. However, this vast loess province lacks a unified stratigraphic scheme. European loess research started in the late 17th century in the Danube Basin with the work of Count Luigi Ferdinand Marsigli. Since that time numerous investigations provided the basis for the pioneering stratigraphic framework proposed initially by Kukla (1970, 1977) in his correlations of loess with deep-sea sediments. Loess-palaeosol sequences in the middle and lower reaches of the Danube River basin were a key part of this framework and contain some of the longest and most complete continental climate records in Europe, covering more than the last million years. However, the very size of the Danube loess belt and the large number of countries it covers presents a major limiting factor in developing a unified approach that enables continental scale analysis of the deposits. Local loess-palaeosol stratigraphic schemes have been defined separately in different countries and the difficulties in correlating such schemes, which often change significantly with advances in age-dating, have limited the number of basin-wide studies. A unified basin-wide stratigraphic model would greatly alleviate these difficulties and facilitate research into the wider significance of these loess records. Therefore we review the existing stratigraphic schemes and define a new Danube Basin wide loess stratigraphy based around a synthetic type section of the Mosorin and Stari Slankamen sites in Serbia. We present a detailed comparison with the sedimentological and palaeoclimatic records preserved in sediments of the Chinese Loess Plateau, with the oxygen isotope records from deep-sea sediments, and with classic European Pleistocene stratigraphic subdivisions. The hierarchy of Danubian stratigraphic units is determined by climatically controlled environmental shifts, in a similar way to the Chinese loess stratigraphic scheme. A new unified Danube loess stratigraphic model has a number of advantages, including preventing confusion resulting from the use of multiple national schemes, a more transparent basis, and the potential to set Pleistocene palaeoenvironmental changes recorded in the Danube catchment area into a global context. The use of a very simple labelling system based on the well-established Chinese loess scheme facilitates interpretation of palaeoenvironmental information reported from the Danube Basin loess sites in a wider more accessible context that can be readily correlated world-wide. This stratigraphic approach also provides, for the first time, an appropriate framework for the development of an integrated, pan-European and potentially pan-Eurasian loess stratigraphic scheme. | ||
| 650 | 4 | |a Stratigraphy | |
| 650 | 4 | |a Sedimentary geology | |
| 650 | 4 | |a River basins | |
| 650 | 4 | |a Paleoclimate science | |
| 700 | 0 | |a Thomas Stevens |4 oth | |
| 700 | 0 | |a George J Kukla |4 oth | |
| 700 | 0 | |a Ulrich Hambach |4 oth | |
| 700 | 0 | |a Kathryn E Fitzsimmons |4 oth | |
| 700 | 0 | |a Phil Gibbard |4 oth | |
| 700 | 0 | |a Björn Buggle |4 oth | |
| 700 | 0 | |a Michael Zech |4 oth | |
| 700 | 0 | |a Zhengtang Guo |4 oth | |
| 700 | 0 | |a Qingzhen Hao |4 oth | |
| 700 | 0 | |a Haibin Wu |4 oth | |
| 700 | 0 | |a Ken O'Hara Dhand |4 oth | |
| 700 | 0 | |a Ian J Smalley |4 oth | |
| 700 | 0 | |a Gábor Újvári |4 oth | |
| 700 | 0 | |a Pál Sümegi |4 oth | |
| 700 | 0 | |a Alida Timar-Gabor |4 oth | |
| 700 | 0 | |a Daniel Veres |4 oth | |
| 700 | 0 | |a Frank Sirocko |4 oth | |
| 700 | 0 | |a Djordjije A Vasiljevic |4 oth | |
| 700 | 0 | |a Zdzislaw Jary |4 oth | |
| 700 | 0 | |a Anderss Svensson |4 oth | |
| 700 | 0 | |a Vidojko Jovic |4 oth | |
| 700 | 0 | |a Frank Lehmkuhl |4 oth | |
| 700 | 0 | |a János Kovács |4 oth | |
| 700 | 0 | |a Zorica Svircev |4 oth | |
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PQ20160617 (DE-627)OLC196785808X (DE-599)GBVOLC196785808X (PRQ)p1483-62c8ac9ef5f9c5d0c745cef7c05e60767ac169ee49c15745245b0af4999cb05f0 (KEY)0080876820150000148000000228danubeloessstratigraphytowardsapaneuropeanloessstr DE-627 ger DE-627 rakwb eng 070 550 DNB RA 1000 AVZ rvk Slobodan B Markovic verfasserin aut Danube loess stratigraphy - Towards a pan-European loess stratigraphic model 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier The Danube River drainage basin is the second largest river catchment in Europe and contains a significant and extensive region of thick loess deposits that preserve a record of a wide variety of recent and past environments. Indeed, the Danube River and tributaries may themselves be responsible for the transportation of large volumes of silt that ultimately drive loess formation in the middle and lower reaches of this large catchment. However, this vast loess province lacks a unified stratigraphic scheme. European loess research started in the late 17th century in the Danube Basin with the work of Count Luigi Ferdinand Marsigli. Since that time numerous investigations provided the basis for the pioneering stratigraphic framework proposed initially by Kukla (1970, 1977) in his correlations of loess with deep-sea sediments. Loess-palaeosol sequences in the middle and lower reaches of the Danube River basin were a key part of this framework and contain some of the longest and most complete continental climate records in Europe, covering more than the last million years. However, the very size of the Danube loess belt and the large number of countries it covers presents a major limiting factor in developing a unified approach that enables continental scale analysis of the deposits. Local loess-palaeosol stratigraphic schemes have been defined separately in different countries and the difficulties in correlating such schemes, which often change significantly with advances in age-dating, have limited the number of basin-wide studies. A unified basin-wide stratigraphic model would greatly alleviate these difficulties and facilitate research into the wider significance of these loess records. Therefore we review the existing stratigraphic schemes and define a new Danube Basin wide loess stratigraphy based around a synthetic type section of the Mosorin and Stari Slankamen sites in Serbia. We present a detailed comparison with the sedimentological and palaeoclimatic records preserved in sediments of the Chinese Loess Plateau, with the oxygen isotope records from deep-sea sediments, and with classic European Pleistocene stratigraphic subdivisions. The hierarchy of Danubian stratigraphic units is determined by climatically controlled environmental shifts, in a similar way to the Chinese loess stratigraphic scheme. A new unified Danube loess stratigraphic model has a number of advantages, including preventing confusion resulting from the use of multiple national schemes, a more transparent basis, and the potential to set Pleistocene palaeoenvironmental changes recorded in the Danube catchment area into a global context. The use of a very simple labelling system based on the well-established Chinese loess scheme facilitates interpretation of palaeoenvironmental information reported from the Danube Basin loess sites in a wider more accessible context that can be readily correlated world-wide. This stratigraphic approach also provides, for the first time, an appropriate framework for the development of an integrated, pan-European and potentially pan-Eurasian loess stratigraphic scheme. Stratigraphy Sedimentary geology River basins Paleoclimate science Thomas Stevens oth George J Kukla oth Ulrich Hambach oth Kathryn E Fitzsimmons oth Phil Gibbard oth Björn Buggle oth Michael Zech oth Zhengtang Guo oth Qingzhen Hao oth Haibin Wu oth Ken O'Hara Dhand oth Ian J Smalley oth Gábor Újvári oth Pál Sümegi oth Alida Timar-Gabor oth Daniel Veres oth Frank Sirocko oth Djordjije A Vasiljevic oth Zdzislaw Jary oth Anderss Svensson oth Vidojko Jovic oth Frank Lehmkuhl oth János Kovács oth Zorica Svircev oth Enthalten in Earth science reviews Amsterdam [u.a.] : Elsevier, 1966 148(2015), Seite 228 (DE-627)129069752 (DE-600)1792-9 (DE-576)014401525 0012-8252 nnns volume:148 year:2015 pages:228 http://search.proquest.com/docview/1697517655 http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-261220 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_21 GBV_ILN_70 GBV_ILN_2027 GBV_ILN_4028 RA 1000 AR 148 2015 228 |
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PQ20160617 (DE-627)OLC196785808X (DE-599)GBVOLC196785808X (PRQ)p1483-62c8ac9ef5f9c5d0c745cef7c05e60767ac169ee49c15745245b0af4999cb05f0 (KEY)0080876820150000148000000228danubeloessstratigraphytowardsapaneuropeanloessstr DE-627 ger DE-627 rakwb eng 070 550 DNB RA 1000 AVZ rvk Slobodan B Markovic verfasserin aut Danube loess stratigraphy - Towards a pan-European loess stratigraphic model 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier The Danube River drainage basin is the second largest river catchment in Europe and contains a significant and extensive region of thick loess deposits that preserve a record of a wide variety of recent and past environments. Indeed, the Danube River and tributaries may themselves be responsible for the transportation of large volumes of silt that ultimately drive loess formation in the middle and lower reaches of this large catchment. However, this vast loess province lacks a unified stratigraphic scheme. European loess research started in the late 17th century in the Danube Basin with the work of Count Luigi Ferdinand Marsigli. Since that time numerous investigations provided the basis for the pioneering stratigraphic framework proposed initially by Kukla (1970, 1977) in his correlations of loess with deep-sea sediments. Loess-palaeosol sequences in the middle and lower reaches of the Danube River basin were a key part of this framework and contain some of the longest and most complete continental climate records in Europe, covering more than the last million years. However, the very size of the Danube loess belt and the large number of countries it covers presents a major limiting factor in developing a unified approach that enables continental scale analysis of the deposits. Local loess-palaeosol stratigraphic schemes have been defined separately in different countries and the difficulties in correlating such schemes, which often change significantly with advances in age-dating, have limited the number of basin-wide studies. A unified basin-wide stratigraphic model would greatly alleviate these difficulties and facilitate research into the wider significance of these loess records. Therefore we review the existing stratigraphic schemes and define a new Danube Basin wide loess stratigraphy based around a synthetic type section of the Mosorin and Stari Slankamen sites in Serbia. We present a detailed comparison with the sedimentological and palaeoclimatic records preserved in sediments of the Chinese Loess Plateau, with the oxygen isotope records from deep-sea sediments, and with classic European Pleistocene stratigraphic subdivisions. The hierarchy of Danubian stratigraphic units is determined by climatically controlled environmental shifts, in a similar way to the Chinese loess stratigraphic scheme. A new unified Danube loess stratigraphic model has a number of advantages, including preventing confusion resulting from the use of multiple national schemes, a more transparent basis, and the potential to set Pleistocene palaeoenvironmental changes recorded in the Danube catchment area into a global context. The use of a very simple labelling system based on the well-established Chinese loess scheme facilitates interpretation of palaeoenvironmental information reported from the Danube Basin loess sites in a wider more accessible context that can be readily correlated world-wide. This stratigraphic approach also provides, for the first time, an appropriate framework for the development of an integrated, pan-European and potentially pan-Eurasian loess stratigraphic scheme. Stratigraphy Sedimentary geology River basins Paleoclimate science Thomas Stevens oth George J Kukla oth Ulrich Hambach oth Kathryn E Fitzsimmons oth Phil Gibbard oth Björn Buggle oth Michael Zech oth Zhengtang Guo oth Qingzhen Hao oth Haibin Wu oth Ken O'Hara Dhand oth Ian J Smalley oth Gábor Újvári oth Pál Sümegi oth Alida Timar-Gabor oth Daniel Veres oth Frank Sirocko oth Djordjije A Vasiljevic oth Zdzislaw Jary oth Anderss Svensson oth Vidojko Jovic oth Frank Lehmkuhl oth János Kovács oth Zorica Svircev oth Enthalten in Earth science reviews Amsterdam [u.a.] : Elsevier, 1966 148(2015), Seite 228 (DE-627)129069752 (DE-600)1792-9 (DE-576)014401525 0012-8252 nnns volume:148 year:2015 pages:228 http://search.proquest.com/docview/1697517655 http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-261220 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_21 GBV_ILN_70 GBV_ILN_2027 GBV_ILN_4028 RA 1000 AR 148 2015 228 |
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PQ20160617 (DE-627)OLC196785808X (DE-599)GBVOLC196785808X (PRQ)p1483-62c8ac9ef5f9c5d0c745cef7c05e60767ac169ee49c15745245b0af4999cb05f0 (KEY)0080876820150000148000000228danubeloessstratigraphytowardsapaneuropeanloessstr DE-627 ger DE-627 rakwb eng 070 550 DNB RA 1000 AVZ rvk Slobodan B Markovic verfasserin aut Danube loess stratigraphy - Towards a pan-European loess stratigraphic model 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier The Danube River drainage basin is the second largest river catchment in Europe and contains a significant and extensive region of thick loess deposits that preserve a record of a wide variety of recent and past environments. Indeed, the Danube River and tributaries may themselves be responsible for the transportation of large volumes of silt that ultimately drive loess formation in the middle and lower reaches of this large catchment. However, this vast loess province lacks a unified stratigraphic scheme. European loess research started in the late 17th century in the Danube Basin with the work of Count Luigi Ferdinand Marsigli. Since that time numerous investigations provided the basis for the pioneering stratigraphic framework proposed initially by Kukla (1970, 1977) in his correlations of loess with deep-sea sediments. Loess-palaeosol sequences in the middle and lower reaches of the Danube River basin were a key part of this framework and contain some of the longest and most complete continental climate records in Europe, covering more than the last million years. However, the very size of the Danube loess belt and the large number of countries it covers presents a major limiting factor in developing a unified approach that enables continental scale analysis of the deposits. Local loess-palaeosol stratigraphic schemes have been defined separately in different countries and the difficulties in correlating such schemes, which often change significantly with advances in age-dating, have limited the number of basin-wide studies. A unified basin-wide stratigraphic model would greatly alleviate these difficulties and facilitate research into the wider significance of these loess records. Therefore we review the existing stratigraphic schemes and define a new Danube Basin wide loess stratigraphy based around a synthetic type section of the Mosorin and Stari Slankamen sites in Serbia. We present a detailed comparison with the sedimentological and palaeoclimatic records preserved in sediments of the Chinese Loess Plateau, with the oxygen isotope records from deep-sea sediments, and with classic European Pleistocene stratigraphic subdivisions. The hierarchy of Danubian stratigraphic units is determined by climatically controlled environmental shifts, in a similar way to the Chinese loess stratigraphic scheme. A new unified Danube loess stratigraphic model has a number of advantages, including preventing confusion resulting from the use of multiple national schemes, a more transparent basis, and the potential to set Pleistocene palaeoenvironmental changes recorded in the Danube catchment area into a global context. The use of a very simple labelling system based on the well-established Chinese loess scheme facilitates interpretation of palaeoenvironmental information reported from the Danube Basin loess sites in a wider more accessible context that can be readily correlated world-wide. This stratigraphic approach also provides, for the first time, an appropriate framework for the development of an integrated, pan-European and potentially pan-Eurasian loess stratigraphic scheme. Stratigraphy Sedimentary geology River basins Paleoclimate science Thomas Stevens oth George J Kukla oth Ulrich Hambach oth Kathryn E Fitzsimmons oth Phil Gibbard oth Björn Buggle oth Michael Zech oth Zhengtang Guo oth Qingzhen Hao oth Haibin Wu oth Ken O'Hara Dhand oth Ian J Smalley oth Gábor Újvári oth Pál Sümegi oth Alida Timar-Gabor oth Daniel Veres oth Frank Sirocko oth Djordjije A Vasiljevic oth Zdzislaw Jary oth Anderss Svensson oth Vidojko Jovic oth Frank Lehmkuhl oth János Kovács oth Zorica Svircev oth Enthalten in Earth science reviews Amsterdam [u.a.] : Elsevier, 1966 148(2015), Seite 228 (DE-627)129069752 (DE-600)1792-9 (DE-576)014401525 0012-8252 nnns volume:148 year:2015 pages:228 http://search.proquest.com/docview/1697517655 http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-261220 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_21 GBV_ILN_70 GBV_ILN_2027 GBV_ILN_4028 RA 1000 AR 148 2015 228 |
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PQ20160617 (DE-627)OLC196785808X (DE-599)GBVOLC196785808X (PRQ)p1483-62c8ac9ef5f9c5d0c745cef7c05e60767ac169ee49c15745245b0af4999cb05f0 (KEY)0080876820150000148000000228danubeloessstratigraphytowardsapaneuropeanloessstr DE-627 ger DE-627 rakwb eng 070 550 DNB RA 1000 AVZ rvk Slobodan B Markovic verfasserin aut Danube loess stratigraphy - Towards a pan-European loess stratigraphic model 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier The Danube River drainage basin is the second largest river catchment in Europe and contains a significant and extensive region of thick loess deposits that preserve a record of a wide variety of recent and past environments. Indeed, the Danube River and tributaries may themselves be responsible for the transportation of large volumes of silt that ultimately drive loess formation in the middle and lower reaches of this large catchment. However, this vast loess province lacks a unified stratigraphic scheme. European loess research started in the late 17th century in the Danube Basin with the work of Count Luigi Ferdinand Marsigli. Since that time numerous investigations provided the basis for the pioneering stratigraphic framework proposed initially by Kukla (1970, 1977) in his correlations of loess with deep-sea sediments. Loess-palaeosol sequences in the middle and lower reaches of the Danube River basin were a key part of this framework and contain some of the longest and most complete continental climate records in Europe, covering more than the last million years. However, the very size of the Danube loess belt and the large number of countries it covers presents a major limiting factor in developing a unified approach that enables continental scale analysis of the deposits. Local loess-palaeosol stratigraphic schemes have been defined separately in different countries and the difficulties in correlating such schemes, which often change significantly with advances in age-dating, have limited the number of basin-wide studies. A unified basin-wide stratigraphic model would greatly alleviate these difficulties and facilitate research into the wider significance of these loess records. Therefore we review the existing stratigraphic schemes and define a new Danube Basin wide loess stratigraphy based around a synthetic type section of the Mosorin and Stari Slankamen sites in Serbia. We present a detailed comparison with the sedimentological and palaeoclimatic records preserved in sediments of the Chinese Loess Plateau, with the oxygen isotope records from deep-sea sediments, and with classic European Pleistocene stratigraphic subdivisions. The hierarchy of Danubian stratigraphic units is determined by climatically controlled environmental shifts, in a similar way to the Chinese loess stratigraphic scheme. A new unified Danube loess stratigraphic model has a number of advantages, including preventing confusion resulting from the use of multiple national schemes, a more transparent basis, and the potential to set Pleistocene palaeoenvironmental changes recorded in the Danube catchment area into a global context. The use of a very simple labelling system based on the well-established Chinese loess scheme facilitates interpretation of palaeoenvironmental information reported from the Danube Basin loess sites in a wider more accessible context that can be readily correlated world-wide. This stratigraphic approach also provides, for the first time, an appropriate framework for the development of an integrated, pan-European and potentially pan-Eurasian loess stratigraphic scheme. Stratigraphy Sedimentary geology River basins Paleoclimate science Thomas Stevens oth George J Kukla oth Ulrich Hambach oth Kathryn E Fitzsimmons oth Phil Gibbard oth Björn Buggle oth Michael Zech oth Zhengtang Guo oth Qingzhen Hao oth Haibin Wu oth Ken O'Hara Dhand oth Ian J Smalley oth Gábor Újvári oth Pál Sümegi oth Alida Timar-Gabor oth Daniel Veres oth Frank Sirocko oth Djordjije A Vasiljevic oth Zdzislaw Jary oth Anderss Svensson oth Vidojko Jovic oth Frank Lehmkuhl oth János Kovács oth Zorica Svircev oth Enthalten in Earth science reviews Amsterdam [u.a.] : Elsevier, 1966 148(2015), Seite 228 (DE-627)129069752 (DE-600)1792-9 (DE-576)014401525 0012-8252 nnns volume:148 year:2015 pages:228 http://search.proquest.com/docview/1697517655 http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-261220 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_21 GBV_ILN_70 GBV_ILN_2027 GBV_ILN_4028 RA 1000 AR 148 2015 228 |
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The Danube River drainage basin is the second largest river catchment in Europe and contains a significant and extensive region of thick loess deposits that preserve a record of a wide variety of recent and past environments. Indeed, the Danube River and tributaries may themselves be responsible for the transportation of large volumes of silt that ultimately drive loess formation in the middle and lower reaches of this large catchment. However, this vast loess province lacks a unified stratigraphic scheme. European loess research started in the late 17th century in the Danube Basin with the work of Count Luigi Ferdinand Marsigli. Since that time numerous investigations provided the basis for the pioneering stratigraphic framework proposed initially by Kukla (1970, 1977) in his correlations of loess with deep-sea sediments. Loess-palaeosol sequences in the middle and lower reaches of the Danube River basin were a key part of this framework and contain some of the longest and most complete continental climate records in Europe, covering more than the last million years. However, the very size of the Danube loess belt and the large number of countries it covers presents a major limiting factor in developing a unified approach that enables continental scale analysis of the deposits. Local loess-palaeosol stratigraphic schemes have been defined separately in different countries and the difficulties in correlating such schemes, which often change significantly with advances in age-dating, have limited the number of basin-wide studies. A unified basin-wide stratigraphic model would greatly alleviate these difficulties and facilitate research into the wider significance of these loess records. Therefore we review the existing stratigraphic schemes and define a new Danube Basin wide loess stratigraphy based around a synthetic type section of the Mosorin and Stari Slankamen sites in Serbia. We present a detailed comparison with the sedimentological and palaeoclimatic records preserved in sediments of the Chinese Loess Plateau, with the oxygen isotope records from deep-sea sediments, and with classic European Pleistocene stratigraphic subdivisions. The hierarchy of Danubian stratigraphic units is determined by climatically controlled environmental shifts, in a similar way to the Chinese loess stratigraphic scheme. A new unified Danube loess stratigraphic model has a number of advantages, including preventing confusion resulting from the use of multiple national schemes, a more transparent basis, and the potential to set Pleistocene palaeoenvironmental changes recorded in the Danube catchment area into a global context. The use of a very simple labelling system based on the well-established Chinese loess scheme facilitates interpretation of palaeoenvironmental information reported from the Danube Basin loess sites in a wider more accessible context that can be readily correlated world-wide. This stratigraphic approach also provides, for the first time, an appropriate framework for the development of an integrated, pan-European and potentially pan-Eurasian loess stratigraphic scheme. |
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The Danube River drainage basin is the second largest river catchment in Europe and contains a significant and extensive region of thick loess deposits that preserve a record of a wide variety of recent and past environments. Indeed, the Danube River and tributaries may themselves be responsible for the transportation of large volumes of silt that ultimately drive loess formation in the middle and lower reaches of this large catchment. However, this vast loess province lacks a unified stratigraphic scheme. European loess research started in the late 17th century in the Danube Basin with the work of Count Luigi Ferdinand Marsigli. Since that time numerous investigations provided the basis for the pioneering stratigraphic framework proposed initially by Kukla (1970, 1977) in his correlations of loess with deep-sea sediments. Loess-palaeosol sequences in the middle and lower reaches of the Danube River basin were a key part of this framework and contain some of the longest and most complete continental climate records in Europe, covering more than the last million years. However, the very size of the Danube loess belt and the large number of countries it covers presents a major limiting factor in developing a unified approach that enables continental scale analysis of the deposits. Local loess-palaeosol stratigraphic schemes have been defined separately in different countries and the difficulties in correlating such schemes, which often change significantly with advances in age-dating, have limited the number of basin-wide studies. A unified basin-wide stratigraphic model would greatly alleviate these difficulties and facilitate research into the wider significance of these loess records. Therefore we review the existing stratigraphic schemes and define a new Danube Basin wide loess stratigraphy based around a synthetic type section of the Mosorin and Stari Slankamen sites in Serbia. We present a detailed comparison with the sedimentological and palaeoclimatic records preserved in sediments of the Chinese Loess Plateau, with the oxygen isotope records from deep-sea sediments, and with classic European Pleistocene stratigraphic subdivisions. The hierarchy of Danubian stratigraphic units is determined by climatically controlled environmental shifts, in a similar way to the Chinese loess stratigraphic scheme. A new unified Danube loess stratigraphic model has a number of advantages, including preventing confusion resulting from the use of multiple national schemes, a more transparent basis, and the potential to set Pleistocene palaeoenvironmental changes recorded in the Danube catchment area into a global context. The use of a very simple labelling system based on the well-established Chinese loess scheme facilitates interpretation of palaeoenvironmental information reported from the Danube Basin loess sites in a wider more accessible context that can be readily correlated world-wide. This stratigraphic approach also provides, for the first time, an appropriate framework for the development of an integrated, pan-European and potentially pan-Eurasian loess stratigraphic scheme. |
| abstract_unstemmed |
The Danube River drainage basin is the second largest river catchment in Europe and contains a significant and extensive region of thick loess deposits that preserve a record of a wide variety of recent and past environments. Indeed, the Danube River and tributaries may themselves be responsible for the transportation of large volumes of silt that ultimately drive loess formation in the middle and lower reaches of this large catchment. However, this vast loess province lacks a unified stratigraphic scheme. European loess research started in the late 17th century in the Danube Basin with the work of Count Luigi Ferdinand Marsigli. Since that time numerous investigations provided the basis for the pioneering stratigraphic framework proposed initially by Kukla (1970, 1977) in his correlations of loess with deep-sea sediments. Loess-palaeosol sequences in the middle and lower reaches of the Danube River basin were a key part of this framework and contain some of the longest and most complete continental climate records in Europe, covering more than the last million years. However, the very size of the Danube loess belt and the large number of countries it covers presents a major limiting factor in developing a unified approach that enables continental scale analysis of the deposits. Local loess-palaeosol stratigraphic schemes have been defined separately in different countries and the difficulties in correlating such schemes, which often change significantly with advances in age-dating, have limited the number of basin-wide studies. A unified basin-wide stratigraphic model would greatly alleviate these difficulties and facilitate research into the wider significance of these loess records. Therefore we review the existing stratigraphic schemes and define a new Danube Basin wide loess stratigraphy based around a synthetic type section of the Mosorin and Stari Slankamen sites in Serbia. We present a detailed comparison with the sedimentological and palaeoclimatic records preserved in sediments of the Chinese Loess Plateau, with the oxygen isotope records from deep-sea sediments, and with classic European Pleistocene stratigraphic subdivisions. The hierarchy of Danubian stratigraphic units is determined by climatically controlled environmental shifts, in a similar way to the Chinese loess stratigraphic scheme. A new unified Danube loess stratigraphic model has a number of advantages, including preventing confusion resulting from the use of multiple national schemes, a more transparent basis, and the potential to set Pleistocene palaeoenvironmental changes recorded in the Danube catchment area into a global context. The use of a very simple labelling system based on the well-established Chinese loess scheme facilitates interpretation of palaeoenvironmental information reported from the Danube Basin loess sites in a wider more accessible context that can be readily correlated world-wide. This stratigraphic approach also provides, for the first time, an appropriate framework for the development of an integrated, pan-European and potentially pan-Eurasian loess stratigraphic scheme. |
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Danube loess stratigraphy - Towards a pan-European loess stratigraphic model |
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Thomas Stevens George J Kukla Ulrich Hambach Kathryn E Fitzsimmons Phil Gibbard Björn Buggle Michael Zech Zhengtang Guo Qingzhen Hao Haibin Wu Ken O'Hara Dhand Ian J Smalley Gábor Újvári Pál Sümegi Alida Timar-Gabor Daniel Veres Frank Sirocko Djordjije A Vasiljevic Zdzislaw Jary Anderss Svensson Vidojko Jovic Frank Lehmkuhl János Kovács Zorica Svircev |
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Thomas Stevens George J Kukla Ulrich Hambach Kathryn E Fitzsimmons Phil Gibbard Björn Buggle Michael Zech Zhengtang Guo Qingzhen Hao Haibin Wu Ken O'Hara Dhand Ian J Smalley Gábor Újvári Pál Sümegi Alida Timar-Gabor Daniel Veres Frank Sirocko Djordjije A Vasiljevic Zdzislaw Jary Anderss Svensson Vidojko Jovic Frank Lehmkuhl János Kovács Zorica Svircev |
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