Quaternary stratigraphy: Recent changes

Corrections to the Quaternary stratigraphic division of Serbia was updated/renewed by lowering limit of the Pleistocene / Quaternary to the beginning of the Gelasian that is at approximately 2.588 million years. Rather than the officially rejected Penck & Brückner Alpine stratigraphic model,...

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Main Authors: Gaudenji Tivadar, Jovanović Mlađen
Format: Article
Language:English
Published: Serbian Geographical Society 2012-01-01
Series:Glasnik Srpskog Geografskog Društva
Subjects:
Online Access:http://www.doiserbia.nb.rs/img/doi/0350-3593/2012/0350-35931204001G.pdf
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author Gaudenji Tivadar
Jovanović Mlađen
author_facet Gaudenji Tivadar
Jovanović Mlađen
author_sort Gaudenji Tivadar
collection DOAJ
description Corrections to the Quaternary stratigraphic division of Serbia was updated/renewed by lowering limit of the Pleistocene / Quaternary to the beginning of the Gelasian that is at approximately 2.588 million years. Rather than the officially rejected Penck & Brückner Alpine stratigraphic model, the use of oxygen isotope stages (OIS / MIS) is recommended. Climatostratigraphic terms glacial and interglacial have a regional applicability and their use is recommended only in areas where there are traces of glaciation, while the terms cold and warm stage (or moderate) stages should be used within the global context. Eopleistocene is a regional term for the former Soviet Union and due to its uniqueness it can hardly be applied in the stratigraphical scheme of the Quaternary depostis in Serbia. With the latest extension of the Lower Pleistocene, further use of Eopleistocene would lead to further confusion in stratigraphic correlation as such the use of the Lower / Early Pleistocene or other appropriate stratigraphic units is recommended. [Projekat Ministarstva nauke Republike Srbije, br. 47007]
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spelling doaj.art-1325b22023ba46a9a46e5acbf286ddca2022-12-21T19:25:45ZengSerbian Geographical SocietyGlasnik Srpskog Geografskog Društva0350-35932012-01-0192411610.2298/GSGD1204001GQuaternary stratigraphy: Recent changesGaudenji TivadarJovanović MlađenCorrections to the Quaternary stratigraphic division of Serbia was updated/renewed by lowering limit of the Pleistocene / Quaternary to the beginning of the Gelasian that is at approximately 2.588 million years. Rather than the officially rejected Penck & Brückner Alpine stratigraphic model, the use of oxygen isotope stages (OIS / MIS) is recommended. Climatostratigraphic terms glacial and interglacial have a regional applicability and their use is recommended only in areas where there are traces of glaciation, while the terms cold and warm stage (or moderate) stages should be used within the global context. Eopleistocene is a regional term for the former Soviet Union and due to its uniqueness it can hardly be applied in the stratigraphical scheme of the Quaternary depostis in Serbia. With the latest extension of the Lower Pleistocene, further use of Eopleistocene would lead to further confusion in stratigraphic correlation as such the use of the Lower / Early Pleistocene or other appropriate stratigraphic units is recommended. [Projekat Ministarstva nauke Republike Srbije, br. 47007]http://www.doiserbia.nb.rs/img/doi/0350-3593/2012/0350-35931204001G.pdfquaternarystratigraphyterminologySerbia
spellingShingle Gaudenji Tivadar
Jovanović Mlađen
Quaternary stratigraphy: Recent changes
Glasnik Srpskog Geografskog Društva
quaternary
stratigraphy
terminology
Serbia
title Quaternary stratigraphy: Recent changes
title_full Quaternary stratigraphy: Recent changes
title_fullStr Quaternary stratigraphy: Recent changes
title_full_unstemmed Quaternary stratigraphy: Recent changes
title_short Quaternary stratigraphy: Recent changes
title_sort quaternary stratigraphy recent changes
topic quaternary
stratigraphy
terminology
Serbia
url http://www.doiserbia.nb.rs/img/doi/0350-3593/2012/0350-35931204001G.pdf
work_keys_str_mv AT gaudenjitivadar quaternarystratigraphyrecentchanges
AT jovanovicmlađen quaternarystratigraphyrecentchanges