Late Carboniferous to Late Permian carbon isotope stratigraphy: A new record from post-Variscan carbonates from the Southern Alps (Austria and Italy)

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Late Carboniferous to Late Permian carbon isotope stratigraphy : A new record from post-Variscan carbonates from the Southern Alps (Austria and Italy). / Buggisch, Werner ; Krainer, Karl; Schaffhauser, Maria; Joachimskia, Michael ; Korte, Christoph.

In: Palaeogeography, Palaeoclimatology, Palaeoecology - An International Journal for the Geo-Sciences, Vol. 433, 2015, p. 174–190.

Research output: Contribution to journal › Journal article › Research › peer-review

Harvard

Buggisch, W, Krainer, K, Schaffhauser, M, Joachimskia, M & Korte, C 2015, 'Late Carboniferous to Late Permian carbon isotope stratigraphy: A new record from post-Variscan carbonates from the Southern Alps (Austria and Italy)', Palaeogeography, Palaeoclimatology, Palaeoecology - An International Journal for the Geo-Sciences, vol. 433, pp. 174–190. https://doi.org/10.1016/j.palaeo.2015.05.012

APA

Buggisch, W., Krainer, K., Schaffhauser, M., Joachimskia, M., & Korte, C. (2015). Late Carboniferous to Late Permian carbon isotope stratigraphy: A new record from post-Variscan carbonates from the Southern Alps (Austria and Italy). Palaeogeography, Palaeoclimatology, Palaeoecology - An International Journal for the Geo-Sciences, 433, 174–190. https://doi.org/10.1016/j.palaeo.2015.05.012

Vancouver

Buggisch W, Krainer K, Schaffhauser M, Joachimskia M, Korte C. Late Carboniferous to Late Permian carbon isotope stratigraphy: A new record from post-Variscan carbonates from the Southern Alps (Austria and Italy). Palaeogeography, Palaeoclimatology, Palaeoecology - An International Journal for the Geo-Sciences. 2015;433:174–190. https://doi.org/10.1016/j.palaeo.2015.05.012

Author

Buggisch, Werner ; Krainer, Karl ; Schaffhauser, Maria ; Joachimskia, Michael ; Korte, Christoph. / Late Carboniferous to Late Permian carbon isotope stratigraphy : A new record from post-Variscan carbonates from the Southern Alps (Austria and Italy). In: Palaeogeography, Palaeoclimatology, Palaeoecology - An International Journal for the Geo-Sciences. 2015 ; Vol. 433. pp. 174–190.

Bibtex

@article{a64dcf3446d746df80039e651505a7b1,
title = "Late Carboniferous to Late Permian carbon isotope stratigraphy: A new record from post-Variscan carbonates from the Southern Alps (Austria and Italy)",
abstract = "An integrated study of the litho-, bio-, and isotope stratigraphy of carbonates in the Southern Alps was undertaken in order to better constrain δ13C variations during the Late Carboniferous to Late Permian. The presented high resolution isotope curves are based on 1299 δ13Ccarb and 396 δ13Corg analyses. The carbon isotope record of diagenetically unaltered samples from the Carnic Alps (Austria) and Karavanke Mountains (Slovenia) shows generally high δ13C values, but Late Carboniferous and Early Permian successions are affected by a diagenetic alteration as consequence of glacio-eustatic sea level changes. Negative δ13C excursions are related to low-stand deposits and caused by diagenetic processes during subaerial exposure. The comparison with δ13C records from other parts of the world demonstrate that δ13C values are high in most unaltered samples, an overall negative trend during the Permian, as recently published, is not obvious and negative excursions related to changes in the carbon isotope composition of the global oceanic carbon pool cannot be confirmed, except for the Permian–Triassic boundary interval.",
author = "Werner Buggisch and Karl Krainer and Maria Schaffhauser and Michael Joachimskia and Christoph Korte",
year = "2015",
doi = "10.1016/j.palaeo.2015.05.012",
language = "English",
volume = "433",
pages = "174–190",
journal = "Palaeogeography, Palaeoclimatology, Palaeoecology - An International Journal for the Geo-Sciences",
issn = "0031-0182",
publisher = "Elsevier",

}

RIS

TY - JOUR

T1 - Late Carboniferous to Late Permian carbon isotope stratigraphy

T2 - A new record from post-Variscan carbonates from the Southern Alps (Austria and Italy)

AU - Buggisch, Werner

AU - Krainer, Karl

AU - Schaffhauser, Maria

AU - Joachimskia, Michael

AU - Korte, Christoph

PY - 2015

Y1 - 2015

N2 - An integrated study of the litho-, bio-, and isotope stratigraphy of carbonates in the Southern Alps was undertaken in order to better constrain δ13C variations during the Late Carboniferous to Late Permian. The presented high resolution isotope curves are based on 1299 δ13Ccarb and 396 δ13Corg analyses. The carbon isotope record of diagenetically unaltered samples from the Carnic Alps (Austria) and Karavanke Mountains (Slovenia) shows generally high δ13C values, but Late Carboniferous and Early Permian successions are affected by a diagenetic alteration as consequence of glacio-eustatic sea level changes. Negative δ13C excursions are related to low-stand deposits and caused by diagenetic processes during subaerial exposure. The comparison with δ13C records from other parts of the world demonstrate that δ13C values are high in most unaltered samples, an overall negative trend during the Permian, as recently published, is not obvious and negative excursions related to changes in the carbon isotope composition of the global oceanic carbon pool cannot be confirmed, except for the Permian–Triassic boundary interval.

AB - An integrated study of the litho-, bio-, and isotope stratigraphy of carbonates in the Southern Alps was undertaken in order to better constrain δ13C variations during the Late Carboniferous to Late Permian. The presented high resolution isotope curves are based on 1299 δ13Ccarb and 396 δ13Corg analyses. The carbon isotope record of diagenetically unaltered samples from the Carnic Alps (Austria) and Karavanke Mountains (Slovenia) shows generally high δ13C values, but Late Carboniferous and Early Permian successions are affected by a diagenetic alteration as consequence of glacio-eustatic sea level changes. Negative δ13C excursions are related to low-stand deposits and caused by diagenetic processes during subaerial exposure. The comparison with δ13C records from other parts of the world demonstrate that δ13C values are high in most unaltered samples, an overall negative trend during the Permian, as recently published, is not obvious and negative excursions related to changes in the carbon isotope composition of the global oceanic carbon pool cannot be confirmed, except for the Permian–Triassic boundary interval.

U2 - 10.1016/j.palaeo.2015.05.012

DO - 10.1016/j.palaeo.2015.05.012

M3 - Journal article

VL - 433

SP - 174

EP - 190

JO - Palaeogeography, Palaeoclimatology, Palaeoecology - An International Journal for the Geo-Sciences

JF - Palaeogeography, Palaeoclimatology, Palaeoecology - An International Journal for the Geo-Sciences

SN - 0031-0182

ER -

ID: 154219409