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SIGNIFICANCE FOR INTERNATIONAL CORRELATION OF THE PERAPERTÚ FORMATION IN NORTHERN PALENCIA, CANTABRIAN MOUNTAINS. TECTONIC/STRATIGRAPHIC CONTEXT AND DESCRIPTION OF MISSISSIPPIAN AND UPPER BASHKIRIAN GONIATITES

Autor: Robert Herman Wagner, Cornelis F. Winkler Prins, Jürgen Kullmann

Publikováno v: Spanish Journal of Palaeontology, Vol 22, Iss 2, Pp 127-145 (2021)

Small ammonoid assemblages are recorded from the Perapertú Formation in northern Palencia. This is a mudstone unit with local platform limestones characterised by carbonate debris flows on the limestone margins. This unit, of Late Bashkirian to Earl

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::633b89b12261b6b0ed0cbaf2f5516551
https://ojs.uv.es/index.php/sjpalaeontology/article/view/20419

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Quantitative palynological analysis of the E2a and E2b goniatite biozones (Arnsbergian, Mississippian) in mudstones from the Southern Pennine Basin (U.K.)

Autor: Jan A.I. Hennissen, G. Montesi

We performed a quantitative palynological analysis of Arnsbergian (Namurian, Late Mississippian) mudstone intervals, potentially prospective for unconventional hydrocarbons. While many palynological studies exist on these stratigraphic intervals in t

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::779921baa7456db592dde8193b5f8143

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Testing the limits of chronostratigraphic resolution in the Appalachian Basin, Late Devonian (middle Frasnian), eastern North America: New U-Pb zircon dates for the Belpre Tephra suite

Autor: D. Jeffrey Over, William T. Kirchgasser, Amanda Lanik, Mark D. Schmitz

Publikováno v: Geological Society of America Bulletin. 128:1813-1821

The Belpre Tephra suite from the Chattanooga Shale in eastern Tennessee and the lower Rhinestreet Shale in western New York has yielded high-precision chemical abrasion−thermal ionization mass spectrometry (CA-TIMS) U-Pb zircon dates of 375.55 ± 0

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::9c97679162f2de35d93c22d39dc86f36
https://doi.org/10.1130/b31408.1

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Permian ammonoids of the Okhotsk Region, Northeast Asia

Autor: Alexander S. Biakov, R. V. Kutygin

Publikováno v: Paleontological Journal. 49:1275-1281

Beds with ammonoids are recognized as a result of the study of goniatitids and prolecanitids from the Nyut, Khuren, and Ayan-Yuryakh in the Okhotsk Region. Beds with Neopronorites tenkensis, assigned to the Upper Artinskian Substage, correspond to th

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::3dba0d364bf0b9fdc910eb3637d42e56
https://doi.org/10.1134/s0031030115120084

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The Late Devonian ammonoid Mimimitoceras in the Anti-Atlas of Morocco

Autor: Volker Ebbighausen, Jürgen Bockwinkel, Dieter Korn

Publikováno v: Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen. 275:125-150

Mimimitoceras is the most abundant late Famennian goniatite genus in the Anti-Atlas of Morocco and the Saoura Valley of Algeria. Based on conch morphology, conch ontogeny, suture line and ornament, six new species can be separated, which occur in thr

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::462328f7119712a39caf7fb700678ff4
https://doi.org/10.1127/njgpa/2015/0455

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THE NATURE AND TIMING OF THE MIDDLE DEVONIAN KA AK BIOEVENTS IN THE MARCELLUS SUBGROUP OF THE APPALACHIAN BASIN

Autor: Thomas J. Schramm, Alexander J. Bartholomew

Publikováno v: PALAIOS. 28:825-836

Intervals of faunal turnover in the fossil record are often preserved at unconformities, suggesting that their apparent abruptness is an artifact of geologic discontinuities. A detailed investigation of the Middle Devonian Kacak Bioevents of the Appa

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::9a6d6131b57ca244bdded271634be7b1
https://doi.org/10.2110/palo.2014.021

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The Malvinokaffric Realm in the Early-Middle Devonian of South Africa

Autor: Cameron R. Penn-Clarke

Publikováno v: Journal of African Earth Sciences. 158:103549

The Devonian palaeontological record of South Africa is essential in understanding plant and animal evolution as well as global palaeobiogeography and palaeoecology at high subpolar-polar (60–90°) southern palaeolatitudes. As early as the mid-nine

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::e2b9837f03f97065a69b1db01af23052
https://doi.org/10.1016/j.jafrearsci.2019.103549

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