Zobrazeno 1 - 10
of 10
pro vyhledávání: '"Lucyna Leda"'
Publikováno v:
European Journal of Taxonomy, Vol 776, Iss 1 (2021)
The Changhsingian (Late Permian) Hambast Formation of sections at Baghuk Mountain (Central Iran) has yielded diverse ammonoid assemblages composed of the genera Pseudogastrioceras, Shevyrevites, Arasella, Dzhulfites, Paratirolites, Clivotirolites gen
Externí odkaz:
https://doaj.org/article/0401f1a0f4534572b0cfc5e0ba56ed8b
Publikováno v:
European Journal of Taxonomy, Vol 776, Iss 1 (2021)
The Changhsingian (Late Permian) Hambast Formation of sections at Baghuk Mountain (Central Iran) has yielded diverse ammonoid assemblages composed of the genera Pseudogastrioceras, Shevyrevites, Arasella, Dzhulfites, Paratirolites, Clivotirolites gen
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6a42a4ff3413899c70572ffc90250481
https://europeanjournaloftaxonomy.eu/index.php/ejt/article/view/1559
https://europeanjournaloftaxonomy.eu/index.php/ejt/article/view/1559
Autor:
Lucyna Leda, Dieter Korn, Wolfgang Kiessling, Martin Schobben, Vachik Hairapetian, Abbas Ghaderi
Publikováno v:
Geology, 46(3), 283. Geological Society of America
The devastating end-Permian mass extinction is widely considered to have been caused by large-scale and rapid greenhouse gas release by Siberian magmatism. Although the proximate extinction mechanisms are disputed, there is widespread agreement that
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::344bb7369a5822320da276024c595583
https://doi.org/10.1130/g39866.1
https://doi.org/10.1130/g39866.1
Autor:
Martin Schobben, Lucyna Leda, Ulrich Struck, Thomas J. Algeo, Dieter Korn, Christoph Korte, Wolf Uwe Reimold, Clemens V. Ullmann, Abbas Ghaderi
Publikováno v:
Chemical Geology. 422:94-107
Sedimentary successions across the Permian–Triassic boundary (PTB) are marked by a prominent negative carbon isotope excursion. This excursion, found in both fossil (e.g., brachiopod) and bulk carbonate at many sites around the world, is generally
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ef4f9e84e7dcec88f98302a3c2e6bf91
Publikováno v:
Journal of Systematic Palaeontology. 14:841-890
The Changhsingian (Late Permian), 4 to 5 m thick Paratirolites Limestone has yielded diverse ammonoid assemblages composed of the genera Neoaganides, Pseudogastrioceras, Dzhulfites, Paratirolites, Julfotirolites, Alibashites, Abichites, Stoyanowites
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::baa0fb2b8e7904efa431ca69e72adcf8
https://doi.org/10.1080/14772019.2015.1119211
https://doi.org/10.1080/14772019.2015.1119211
Publikováno v:
Fossil Record 17(1): 41-57
Fossil record, 17(1): 41-57
Fossil Record, Vol 17, Iss 1, Pp 41-57 (2014)
Fossil record, 17(1): 41-57
Fossil Record, Vol 17, Iss 1, Pp 41-57 (2014)
The Permian–Triassic boundary sections in north-western Iran belong to the most complete successions, in which the largest mass extinction event in the history of the Earth can be studied. We investigated the Changhsingian stage in six sections in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c1a8782bd1810eb9060dc3de00341bac
https://www.foss-rec.net/17/41/2014/
https://www.foss-rec.net/17/41/2014/
Autor:
Martin Schobben, Sebastiaan van de Velde, Jana Suchocka, Lucyna Leda, Dieter Korn, Ulrich Struck, Clemens Vinzenz Ullmann, Vachik Hairapetian, Abbas Ghaderi, Christoph Korte, Robert J. Newton, Simon W. Poulton, Paul B. Wignall
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1d0cb5eba346d1ebff98b0036d176db5
https://doi.org/10.5194/cp-2017-66-supplement
https://doi.org/10.5194/cp-2017-66-supplement
Publikováno v:
Gondwana Research. 26:675-683
The end-Permian mass extinction has been associated with severe global warming. Main stage volcanism of the Siberian Traps occurred at or near the extinction interval and has been proposed as a likely greenhouse catalyst. In this study, a high-resolu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::011dba56a05c6f3669a699214ded2c57
https://doi.org/10.1016/j.gr.2013.07.019
https://doi.org/10.1016/j.gr.2013.07.019
Publikováno v:
Facies. 60:295-325
Permian–Triassic boundary sections in the Julfa (NW Iran) and Abadeh (Central Iran) regions display a succession of three characteristic rock units, (1) the Paratirolites Limestone with the mass extinction horizon at its top, (2) the ‘Boundary Cl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8d07e50cf7bcb9d6dc03aaa05c386c02
https://doi.org/10.1007/s10347-013-0366-0
https://doi.org/10.1007/s10347-013-0366-0
Autor:
Thomas J. Algeo, Lucyna Leda, Martin Schobben, Ulrich Struck, János Haas, Harald Strauss, Alan Stebbins, Dieter Korn, Christoph Korte
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology, 486, 74. Elsevier Saunders
Marine biodiversity decreases and ecosystem destruction during the end-Permian mass extinction (EPME) have been linked to widespread marine euxinic conditions. Changes in the biogeochemical sulfur cycle, microbial sulfate reduction (MSR), and marine
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6241f60a80d04eeeb8b6746b52f96594
https://doi.org/10.1016/j.palaeo.2017.02.025
https://doi.org/10.1016/j.palaeo.2017.02.025