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== Classification ==
== Classification ==
The Gunz-Haslach interglacial is defined as that [[erosion (geology)|erosion]] phase which follows the [[Günz Glacial Stage|Günz]] and precedes the [[Haslach Glacial Stage]]. It thus corresponds to the stratigraphic gap between the Zeil gravels (''Zeiler Schotter'') in [[Swabia]] and Haslach gravels (''Haslacher Schotter'') northeast of the [[Rhine Glacier]].<ref>{{citation/core|Surname1=A. Schreiner & R. Ebel|Periodical=Geologisches Jahrbuch|Title=Quartärgeologische Untersuchungen in der Umgebung von Interglazialvorkommen im östlichen Rheingletschergebiet (Baden-Württemberg) |Volume=A 59|PublicationPlace=Hannover|Year=1981|At=pp.&nbsp;3–64|Date= 1981|language=German}}</ref><ref>{{citation/core|Surname1=W. Fesseler & W. Goos|Title=Geologische Karte 1:25,000 von Baden-Württemberg. Erläuterungen zu Blatt 8026 Aitrach |PublicationPlace=Stuttgart|Year=1988|Date= 1988|language=German}}</ref> Depositions from the time of the Gunz-Haslach interglacial have hitherto only been detected as [[weathering]] formations ([[soil]]s) on the Zeil gravels. The erosion during the interglacial is very marked and there are different views on the assignment of the gravels (''Schotter'') before and afterwards.
The Gunz-Haslach interglacial is defined as that [[erosion (geology)|erosion]] phase which follows the [[Günz Glacial Stage|Günz]] and precedes the [[Haslach Glacial Stage]]. It thus corresponds to the stratigraphic gap between the Zeil gravels (''Zeiler Schotter'') in [[Swabia]] and Haslach gravels (''Haslacher Schotter'') northeast of the [[Rhine Glacier]].<ref>{{cite journal|surname1=A. Schreiner & R. Ebel|periodical=Geologisches Jahrbuch|title=Quartärgeologische Untersuchungen in der Umgebung von Interglazialvorkommen im östlichen Rheingletschergebiet (Baden-Württemberg) |volume=A 59|publicationplace=Hannover|year=1981|at=pp.&nbsp;3–64|date=1981|language=German}}</ref><ref>{{cite journal|surname1=W. Fesseler & W. Goos|title=Geologische Karte 1:25,000 von Baden-Württemberg. Erläuterungen zu Blatt 8026 Aitrach |publicationplace=Stuttgart|year=1988|date=1988|language=German}}</ref> Depositions from the time of the Gunz-Haslach interglacial have hitherto only been detected as [[weathering]] formations ([[soil]]s) on the Zeil gravels. The erosion during the interglacial is very marked and there are different views on the assignment of the gravels (''Schotter'') before and afterwards.


The interglacial may possible correlated to [[marine isotope stage|MIS]] 15. In this case it would be about 540,000 to 600,000 years old.<ref>{{citation/core|Surname1=Lorraine E. Lisiecki|Surname2=Maureen E. Raymo|Periodical=Paleoceanography|Title=A Plio-Pleistocene Stack of 57 Globally Distributed Benthic δ<sup>18</sup>O Records |Volume=20|Year=2005|Date= 2005|language=German|URL={{cite web |url=http://web.pdx.edu/~chulbe/COURSES/QCLIM/reprints/LisieckiRaymo_preprint.pdf |title=pdf file; 1.1 MB |accessdate=2011-06-16 |deadurl=yes |archiveurl=https://web.archive.org/web/20110616130840/http://web.pdx.edu/~chulbe/COURSES/QCLIM/reprints/LisieckiRaymo_preprint.pdf |archivedate=June 16, 2011 |df= }}}}</ref> There are, however, clues that the interglacial could be older than MIS 15.<ref>[[#Literatur|Habbe 2007]], p. 75</ref>
The interglacial may possible correlated to [[marine isotope stage|MIS]] 15. In this case it would be about 540,000 to 600,000 years old.<ref>{{cite journal|surname1=Lorraine E. Lisiecki|surname2=Maureen E. Raymo|periodical=Paleoceanography|title=A Plio-Pleistocene Stack of 57 Globally Distributed Benthic δ<sup>18</sup>O Records |volume=20|year=2005|date=2005|language=German|url=http://web.pdx.edu/~chulbe/COURSES/QCLIM/reprints/LisieckiRaymo_preprint.pdf |archiveurl=https://web.archive.org/web/20110616130840/http://web.pdx.edu/~chulbe/COURSES/QCLIM/reprints/LisieckiRaymo_preprint.pdf |archivedate=2011-06-16 |deadurl=yes}}</ref> There are, however, clues that the interglacial could be older than MIS 15.<ref>[[#Literatur|Habbe 2007]], p. 75</ref>


The Günz-Haslach interglacial definitely corresponds in part to the Swiss Deckenschotter glaciations.<ref>{{citation/core|Surname1=Ueli Reinmann|Periodical=Jahrbuch des Oberaargaus|Title=Auf den Spuren der Eiszeit im Raum Wangen a. A. : Neue Erkenntnisse auf Grund von bodenkundlichen Untersuchungen im Endmoränengebiet des Rhonegletschers|Volume=47|Year=2004|At=pp.&nbsp;135–152|Date= 2004|language=German|URL=http://www.digibern.ch/jahrbuch_oberaargau/jahrbuch_2004/JBOAG_2004_135_152_eiszeit_wangen.pdf|Format= pdf file; 850 kB}}</ref>
The Günz-Haslach interglacial definitely corresponds in part to the Swiss Deckenschotter glaciations.<ref>{{cite journal|surname1=Ueli Reinmann|periodical=Jahrbuch des Oberaargaus|title=Auf den Spuren der Eiszeit im Raum Wangen a. A. : Neue Erkenntnisse auf Grund von bodenkundlichen Untersuchungen im Endmoränengebiet des Rhonegletschers|volume=47|year=2004|at=pp.&nbsp;135–152|date=2004|language=German|url=http://www.digibern.ch/jahrbuch_oberaargau/jahrbuch_2004/JBOAG_2004_135_152_eiszeit_wangen.pdf|format=pdf file; 850 kB}}</ref>


== Literature ==
== Literature ==
* {{citation/core|Surname1=K.A. Habbe|Surname2=in cooperation with D. Ellwanger|Surname3=R. Becker-Haumann|EditorSurname1=T. Litt im Auftrag der Deutschen Stratigraphischen Kommission 2007|Periodical=Eiszeitalter und Gegenwart/Quaternary Science Journal|Title=Stratigraphische Begriffe für das Quartär des süddeutschen Alpenvorlandes |Volume=56, No. 1/2|Publisher=E. Schweizerbart’sche Verlagsbuchhandlung (Nägele und Obermiller)|PublicationPlace=Stuttgart|At=pp.&nbsp;66–83|ISSN=0424-7116|language=German|DOI=10.3285/eg.56.1-2.03}}
* {{cite journal|surname1=K.A. Habbe|surname2=in cooperation with D. Ellwanger|surname3=R. Becker-Haumann|periodical=Eiszeitalter und Gegenwart/Quaternary Science Journal|title=Stratigraphische Begriffe für das Quartär des süddeutschen Alpenvorlandes |volume=56, No. 1/2|publisher=E. Schweizerbart’sche Verlagsbuchhandlung (Nägele und Obermiller)|publicationplace=Stuttgart|at=pp.&nbsp;66–83|issn=0424-7116|language=German|doi=10.3285/eg.56.1-2.03}}
* {{citation/core|Surname1=T. Litt et al.|Periodical=Newsletters in Stratigraphie|Title=Das Quartär in der Stratigraphischen Tabelle von Deutschland 2002 |Volume=41|Issue=1-3|PublicationPlace=Berlin, Stuttgart|At=pp.&nbsp;385-399|language=German|URL=http://www.deuqua.de/strat/dokumente/Erlaeuterungen_STD02.pdf|Format= Explanation; pdf file, 124 kB and [http://www.deuqua.de/strat/dokumente/website_STD2002_Quartaer.pdf table; pdf file, 182 kB]}}
* {{cite journal|surname1=T. Litt et al.|periodical=Newsletters in Stratigraphie|title=Das Quartär in der Stratigraphischen Tabelle von Deutschland 2002 |volume=41|issue=1-3|publicationplace=Berlin, Stuttgart|at=pp.&nbsp;385-399|language=German|url=http://www.deuqua.de/strat/dokumente/Erlaeuterungen_STD02.pdf|format= Explanation; pdf file, 124 kB and [http://www.deuqua.de/strat/dokumente/website_STD2002_Quartaer.pdf table; pdf file, 182 kB]}}


== References ==
== References ==

Revision as of 16:04, 1 December 2017

The Gunz-Haslach interglacial (German: Günz-Haslach-Interglazial), also Gunz-Haslach warm period (Günz-Haslach-Warmzeit), is one of the warm periods of the Pleistocene in the Alpine region. It lies between the Gunz and Haslach glaciations.

Classification

The Gunz-Haslach interglacial is defined as that erosion phase which follows the Günz and precedes the Haslach Glacial Stage. It thus corresponds to the stratigraphic gap between the Zeil gravels (Zeiler Schotter) in Swabia and Haslach gravels (Haslacher Schotter) northeast of the Rhine Glacier.[1][2] Depositions from the time of the Gunz-Haslach interglacial have hitherto only been detected as weathering formations (soils) on the Zeil gravels. The erosion during the interglacial is very marked and there are different views on the assignment of the gravels (Schotter) before and afterwards.

The interglacial may possible correlated to MIS 15. In this case it would be about 540,000 to 600,000 years old.[3] There are, however, clues that the interglacial could be older than MIS 15.[4]

The Günz-Haslach interglacial definitely corresponds in part to the Swiss Deckenschotter glaciations.[5]

Literature

  • K.A. Habbe; in cooperation with D. Ellwanger; R. Becker-Haumann. "Stratigraphische Begriffe für das Quartär des süddeutschen Alpenvorlandes". Eiszeitalter und Gegenwart/Quaternary Science Journal (in German). 56, No. 1/2. Stuttgart: E. Schweizerbart’sche Verlagsbuchhandlung (Nägele und Obermiller). pp. 66–83. doi:10.3285/eg.56.1-2.03. ISSN 0424-7116. {{cite journal}}: Unknown parameter |publicationplace= ignored (|publication-place= suggested) (help)CS1 maint: unflagged free DOI (link)
  • T. Litt; et al. "Das Quartär in der Stratigraphischen Tabelle von Deutschland 2002" (Explanation; pdf file, 124 kB and table; pdf file, 182 kB). Newsletters in Stratigraphie (in German). 41 (1–3). Berlin, Stuttgart. pp. 385-399. {{cite journal}}: Explicit use of et al. in: |surname1= (help); External link in |format= (help); Unknown parameter |publicationplace= ignored (|publication-place= suggested) (help)

References

  1. ^ A. Schreiner & R. Ebel (1981). "Quartärgeologische Untersuchungen in der Umgebung von Interglazialvorkommen im östlichen Rheingletschergebiet (Baden-Württemberg)". Geologisches Jahrbuch (in German). A 59. Hannover. pp. 3–64. {{cite journal}}: Unknown parameter |publicationplace= ignored (|publication-place= suggested) (help)CS1 maint: date and year (link)
  2. ^ W. Fesseler & W. Goos (1988). "Geologische Karte 1:25,000 von Baden-Württemberg. Erläuterungen zu Blatt 8026 Aitrach" (in German). Stuttgart. {{cite journal}}: Cite journal requires |journal= (help); Unknown parameter |publicationplace= ignored (|publication-place= suggested) (help)CS1 maint: date and year (link)
  3. ^ Lorraine E. Lisiecki; Maureen E. Raymo (2005). "A Plio-Pleistocene Stack of 57 Globally Distributed Benthic δ18O Records" (PDF). Paleoceanography (in German). 20. Archived from the original (PDF) on 2011-06-16. {{cite journal}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)CS1 maint: date and year (link)
  4. ^ Habbe 2007, p. 75
  5. ^ Ueli Reinmann (2004). "Auf den Spuren der Eiszeit im Raum Wangen a. A. : Neue Erkenntnisse auf Grund von bodenkundlichen Untersuchungen im Endmoränengebiet des Rhonegletschers" (pdf file; 850 kB). Jahrbuch des Oberaargaus (in German). 47. pp. 135–152.{{cite journal}}: CS1 maint: date and year (link)

External links

Retrieved from "https://en.wikipedia.org/w/index.php?title=Gunz-Haslach_interglacial&oldid=813071495"