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  • 1
    Monograph available for loan
    Monograph available for loan
    The carboniferous timescale; Part B (2022)
    London : The Geological Society
    Associated volumes
    Details Availability
    Call number: 9/M 07.0421(512/B)
    In: Special publications / the Geological Society, London, No. 512
    Description / Table of Contents: The Carboniferous chronostratigraphic scale consists of two subsystems, six series and seven stages. Precise numerical age control within the Carboniferous is uneven, and a global magnetic polarity timescale for the Carboniferous is far from established. Isotope stratigraphy based on Sr, C and O isotopes is at an early stage but has already identified a few Sr and C isotope events of use to global correlation. Cyclostratigraphy has created a workable astrochronology for part of Pennsylvanian time that needs better calibration. Chronostratigraphic definitions of most of the seven Carboniferous stages remain unfinished. Future research on the Carboniferous timescale should focus on Global Stratotype Section and Point (GSSP) selection for the remaining, undefined stage bases, definition and characterization of substages, and further development and integration of the Carboniferous chronostratigraphic scale with radioisotopic, magnetostratigraphic, chemostratigraphic and cyclostratigraphic tools for calibration and correlation, and the cross-correlation of non-marine and marine chronologies.
    Type of Medium: Monograph available for loan
    Pages: vi, 696-1016 Seiten , Illustrationen, Diagramme, Karten
    ISBN: 9781786205421 , 978-1-78620-542-1
    ISSN: 0305-8719
    Series Statement: Special publications / the Geological Society, London No. 512
    URL: Fulltext @ Lyell Collection (GFZ only)
    DOI: 10.1144/SP512-2021-160
    Language: English
    Note: Contents PART A Lucas, S. G., Schneider, J. W., Nikolaeva, S. and Wang, X. / The Carboniferous timescale: an introduction Carboniferous chronostratigraphy Lucas, S. G., Schneider, J. W., Nikolaeva, S. and Wang, X. / The Carboniferous chronostratigraphic scale: history, status and prospectus Alekseev, A. S., Nikolaeva, S. V., Goreva, N. V., Donova, N. B., Kossovaya, O. L., Kulagina, E. I., Kucheva, N. A., Kurilenko, A. V., Kutygin, R. V., Popeko, L. I. and Stepanova, T. I. / Russian regional Carboniferous stratigraphy González, C. R. and Díaz Saravia, P. / Proposed chronostratigraphic units for the Carboniferous and early Permian of the southwestern Gondwana margin Magnetostratigraphy Hounslow, M. W. / A geomagnetic polarity timescale for the Carboniferous Isotope stratigraphy Chen, J., Chen, B. and Montañez, I. P. 7 Carboniferous isotope stratigraphy Cyclostratigraphy Montañez, I. P. 7 Current synthesis of the penultimate icehouse and its imprint on the Upper Devonian through Permian stratigraphic record Marine biostratigraphy Vachard, D. and Le Coze, F. 7 Carboniferous smaller Foraminifera: convergences and divergences Ueno, K. 7 Carboniferous fusuline Foraminifera: taxonomy, regional biostratigraphy, and palaeobiogeographic faunal development Angiolini, L., Cisterna, G. A., Mottequin, B., Shen, S.-Z. and Muttoni, G. 7 Global Carboniferous brachiopod biostratigraphy Ausich, W. I., Kammer, T. W. and Mirantsev, G. V. 7 Carboniferous crinoids Wang, X.-D., Yang, S.-R., Yao, L., Sugiyama, T. and Hu, K.-yi 7 Carboniferous biostratigraphy of rugose corals Nikolaeva, S. V. / Carboniferous ammonoid genozones PART B Barrick, J. E., Alekseev, A. S., Blanco-Ferrera, S., Goreva, N. V., Hu, K., Lambert, L. L., Nemyrovska, T. I., Qi, Y., Ritter, S. M. and Sanz-López, J. 7 Carboniferous conodont biostratigraphy Ginter, M. / The biostratigraphy of Carboniferous chondrichthyans Non-marine biostratigraphy Eble, C. F. / Appalachian coal bed palynofloras: changes in composition through time and comparison with other areas Opluštil, S., Cleal, C. J., Wang, J. and Wan, M. / Carboniferous macrofloral biostratigraphy: an overview Schneider, J. W., Scholze, F., Ross, A. J., Blake, B. M. Jr and Lucas, S. G. / Improved blattoid insect and conchostracan zonation for the Late Carboniferous, Pennsylvanian, of Euramerica Amler, M. R. W. and Silantiev, V. V. / A global review of Carboniferous marine and non-marine bivalve biostratigraphy Lucas, S. G., Stimson, M. R., King, O. A., Calder, J. H., Mansky, C. F., Hebert, B. L. and Hunt, A. P. / Carboniferous tetrapod footprint biostratigraphy, biochronology and evolutionary events Lucas, S. G. / Carboniferous tetrapod biostratigraphy, biochronology and evolutionary events Index
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  • 2
    Monograph available for loan
    Monograph available for loan
    The carboniferous timescale; Part A (2022)
    London : The Geological Society
    Associated volumes
    Details Availability
    Call number: 9/M 07.0421(512/A)
    In: Special publications / the Geological Society, London, No. 512
    Description / Table of Contents: The Carboniferous chronostratigraphic scale consists of two subsystems, six series and seven stages. Precise numerical age control within the Carboniferous is uneven, and a global magnetic polarity timescale for the Carboniferous is far from established. Isotope stratigraphy based on Sr, C and O isotopes is at an early stage but has already identified a few Sr and C isotope events of use to global correlation. Cyclostratigraphy has created a workable astrochronology for part of Pennsylvanian time that needs better calibration. Chronostratigraphic definitions of most of the seven Carboniferous stages remain unfinished. Future research on the Carboniferous timescale should focus on Global Stratotype Section and Point (GSSP) selection for the remaining, undefined stage bases, definition and characterization of substages, and further development and integration of the Carboniferous chronostratigraphic scale with radioisotopic, magnetostratigraphic, chemostratigraphic and cyclostratigraphic tools for calibration and correlation, and the cross-correlation of non-marine and marine chronologies.
    Type of Medium: Monograph available for loan
    Pages: vi, 693 Seiten , Illustrationen, Diagramme, Karten , 26 cm
    ISBN: 9781786205421 , 978-1-78620-542-1
    ISSN: 0305-8719
    Series Statement: Special publications / the Geological Society, London No. 512
    URL: Fulltext @ Lyell Collection (GFZ only)
    DOI: 10.1144/SP512-2021-160
    Language: English
    Note: Contents PART A Lucas, S. G., Schneider, J. W., Nikolaeva, S. and Wang, X. / The Carboniferous timescale: an introduction Carboniferous chronostratigraphy Lucas, S. G., Schneider, J. W., Nikolaeva, S. and Wang, X. / The Carboniferous chronostratigraphic scale: history, status and prospectus Alekseev, A. S., Nikolaeva, S. V., Goreva, N. V., Donova, N. B., Kossovaya, O. L., Kulagina, E. I., Kucheva, N. A., Kurilenko, A. V., Kutygin, R. V., Popeko, L. I. and Stepanova, T. I. / Russian regional Carboniferous stratigraphy González, C. R. and Díaz Saravia, P. / Proposed chronostratigraphic units for the Carboniferous and early Permian of the southwestern Gondwana margin Magnetostratigraphy Hounslow, M. W. / A geomagnetic polarity timescale for the Carboniferous Isotope stratigraphy Chen, J., Chen, B. and Montañez, I. P. 7 Carboniferous isotope stratigraphy Cyclostratigraphy Montañez, I. P. 7 Current synthesis of the penultimate icehouse and its imprint on the Upper Devonian through Permian stratigraphic record Marine biostratigraphy Vachard, D. and Le Coze, F. 7 Carboniferous smaller Foraminifera: convergences and divergences Ueno, K. 7 Carboniferous fusuline Foraminifera: taxonomy, regional biostratigraphy, and palaeobiogeographic faunal development Angiolini, L., Cisterna, G. A., Mottequin, B., Shen, S.-Z. and Muttoni, G. 7 Global Carboniferous brachiopod biostratigraphy Ausich, W. I., Kammer, T. W. and Mirantsev, G. V. 7 Carboniferous crinoids Wang, X.-D., Yang, S.-R., Yao, L., Sugiyama, T. and Hu, K.-yi 7 Carboniferous biostratigraphy of rugose corals Nikolaeva, S. V. / Carboniferous ammonoid genozones PART B Barrick, J. E., Alekseev, A. S., Blanco-Ferrera, S., Goreva, N. V., Hu, K., Lambert, L. L., Nemyrovska, T. I., Qi, Y., Ritter, S. M. and Sanz-López, J. 7 Carboniferous conodont biostratigraphy Ginter, M. / The biostratigraphy of Carboniferous chondrichthyans Non-marine biostratigraphy Eble, C. F. / Appalachian coal bed palynofloras: changes in composition through time and comparison with other areas Opluštil, S., Cleal, C. J., Wang, J. and Wan, M. / Carboniferous macrofloral biostratigraphy: an overview Schneider, J. W., Scholze, F., Ross, A. J., Blake, B. M. Jr and Lucas, S. G. / Improved blattoid insect and conchostracan zonation for the Late Carboniferous, Pennsylvanian, of Euramerica Amler, M. R. W. and Silantiev, V. V. / A global review of Carboniferous marine and non-marine bivalve biostratigraphy Lucas, S. G., Stimson, M. R., King, O. A., Calder, J. H., Mansky, C. F., Hebert, B. L. and Hunt, A. P. / Carboniferous tetrapod footprint biostratigraphy, biochronology and evolutionary events Lucas, S. G. / Carboniferous tetrapod biostratigraphy, biochronology and evolutionary events Index
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  • 3
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    The carboniferous timescale (2022)
    London : The Geological Society
    Associated volumes
    Details
    Call number: 10.1144/SP512-2021-160 (e-book)
    In: Special publications / the Geological Society, London, No. 512
    Description / Table of Contents: The Carboniferous chronostratigraphic scale consists of two subsystems, six series and seven stages. Precise numerical age control within the Carboniferous is uneven, and a global magnetic polarity timescale for the Carboniferous is far from established. Isotope stratigraphy based on Sr, C and O isotopes is at an early stage but has already identified a few Sr and C isotope events of use to global correlation. Cyclostratigraphy has created a workable astrochronology for part of Pennsylvanian time that needs better calibration. Chronostratigraphic definitions of most of the seven Carboniferous stages remain unfinished. Future research on the Carboniferous timescale should focus on Global Stratotype Section and Point (GSSP) selection for the remaining, undefined stage bases, definition and characterization of substages, and further development and integration of the Carboniferous chronostratigraphic scale with radioisotopic, magnetostratigraphic, chemostratigraphic and cyclostratigraphic tools for calibration and correlation, and the cross-correlation of non-marine and marine chronologies.
    Type of Medium: 12
    Pages: 1 Online-Ressource (vi, 1016 Seiten) , Illustrationen, Diagramme, Karten
    ISBN: 9781786205421 , 978-1-78620-542-1
    ISSN: 0305-8719
    Series Statement: Special publications / the Geological Society, London No. 512
    URL: Fulltext @ Lyell Collection (GFZ only)
    DOI: 10.1144/SP512-2021-160
    Language: English
    Note: Contents PART A Lucas, S. G., Schneider, J. W., Nikolaeva, S. and Wang, X. / The Carboniferous timescale: an introduction Carboniferous chronostratigraphy Lucas, S. G., Schneider, J. W., Nikolaeva, S. and Wang, X. / The Carboniferous chronostratigraphic scale: history, status and prospectus Alekseev, A. S., Nikolaeva, S. V., Goreva, N. V., Donova, N. B., Kossovaya, O. L., Kulagina, E. I., Kucheva, N. A., Kurilenko, A. V., Kutygin, R. V., Popeko, L. I. and Stepanova, T. I. / Russian regional Carboniferous stratigraphy González, C. R. and Díaz Saravia, P. / Proposed chronostratigraphic units for the Carboniferous and early Permian of the southwestern Gondwana margin Magnetostratigraphy Hounslow, M. W. / A geomagnetic polarity timescale for the Carboniferous Isotope stratigraphy Chen, J., Chen, B. and Montañez, I. P. 7 Carboniferous isotope stratigraphy Cyclostratigraphy Montañez, I. P. 7 Current synthesis of the penultimate icehouse and its imprint on the Upper Devonian through Permian stratigraphic record Marine biostratigraphy Vachard, D. and Le Coze, F. 7 Carboniferous smaller Foraminifera: convergences and divergences Ueno, K. 7 Carboniferous fusuline Foraminifera: taxonomy, regional biostratigraphy, and palaeobiogeographic faunal development Angiolini, L., Cisterna, G. A., Mottequin, B., Shen, S.-Z. and Muttoni, G. 7 Global Carboniferous brachiopod biostratigraphy Ausich, W. I., Kammer, T. W. and Mirantsev, G. V. 7 Carboniferous crinoids Wang, X.-D., Yang, S.-R., Yao, L., Sugiyama, T. and Hu, K.-yi 7 Carboniferous biostratigraphy of rugose corals Nikolaeva, S. V. / Carboniferous ammonoid genozones PART B Barrick, J. E., Alekseev, A. S., Blanco-Ferrera, S., Goreva, N. V., Hu, K., Lambert, L. L., Nemyrovska, T. I., Qi, Y., Ritter, S. M. and Sanz-López, J. 7 Carboniferous conodont biostratigraphy Ginter, M. / The biostratigraphy of Carboniferous chondrichthyans Non-marine biostratigraphy Eble, C. F. / Appalachian coal bed palynofloras: changes in composition through time and comparison with other areas Opluštil, S., Cleal, C. J., Wang, J. and Wan, M. / Carboniferous macrofloral biostratigraphy: an overview Schneider, J. W., Scholze, F., Ross, A. J., Blake, B. M. Jr and Lucas, S. G. / Improved blattoid insect and conchostracan zonation for the Late Carboniferous, Pennsylvanian, of Euramerica Amler, M. R. W. and Silantiev, V. V. / A global review of Carboniferous marine and non-marine bivalve biostratigraphy Lucas, S. G., Stimson, M. R., King, O. A., Calder, J. H., Mansky, C. F., Hebert, B. L. and Hunt, A. P. / Carboniferous tetrapod footprint biostratigraphy, biochronology and evolutionary events Lucas, S. G. / Carboniferous tetrapod biostratigraphy, biochronology and evolutionary events Index
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  • 4
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    Non-Marine Permian Biostratigraphy and Biochronology (2006)
    London : The Geological Society
    Details
    Description / Table of Contents: During the Permian, the single supercontinent Pangaea stretched from pole to pole. Early Permian glacial deposits are found in southern Gondwana. Along the sutures of Pangaea, mountain ranges towered over vast tropical lowlands. Interior areas included dry deserts where dune sands accumulated. Gypsum and halite beds document the evaporation of hot, shallow seas that formed the most extensive salt deposits in the geological record. The Permian period (251 to 299 Ma) encompasses nine ages (stages) arranged into three epochs (series). Most of the Permian marine timescale has been defined by global stratotype sections and points for the stage boundaries. This volume presents new data regarding the biostratigraphy and biochronology of the non-marine Permian and provides a basis for temporally ordering Permian geological and biotic history on land, and correlating that history to events in the marine realm.
    Pages: Online-Ressource (344 Seiten)
    ISBN: 9781862392069
    URL: http://sp.lyellcollection.org/content/vol265/issue1/
    Language: English
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  • 5
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    An andesitic sill complex in the Southern Permian Basin: volcanogenetic model and stratigraphic implications (2020)
    Luthardt, Ludwig ; Breitkreuz, Christoph ; Schneider, Joerg W. ; [et al.]
    Springer Berlin Heidelberg
    Details
    Publication Date: 2023-06-19
    Description: Subvolcanic intrusions are highly variable in shape and structure, and occur in nearly all parts of the upper crust, as a result of extensive volcanic activity. Processes of subvolcanics interacting with the host rock are insufficiently understood, as they are rarely exposed. In the southernmost part of the Flechtingen-Altmark Subprovince, (sub)volcanic rocks of the Flechtingen Volcanic Complex (FVC) are exposed in several quarries. It is built up of silicic tuffs, ignimbrites and lava flows, but also of intermediate lavas and extended sill sheets. Additionally, major granitic intrusions exposed by drillings are associated with the FVC. In the Mammendorf quarry, a sill intruded in between lithified turbiditic series of early Carboniferous (Visean–Serphukovian) age at the base, and widely consolidated volcanoclastic deposits of late Carboniferous (late Pennsylvanian) age at the top. Various magma-host rock interactions were found indicating brittle and ductile deformation patterns occurring at the basal contact, and secondary fluidal mixing predominantly occurring at the top contact, most probably caused by fluids accompanying the intruding magma. We present an extended volcanogenetic model for the FVC. Volcanic activity initiated at 302 ± 3 Ma with fallout deposits represented by mostly re-deposited silicic ashfall deposits of the Flechtingen Formation, and cumulated in depositing major ignimbrite series, most likely forming a caldera. Later, the sills intruded at the rheological boundary of the lithified Mississippian turbiditic series and the partly consolidated volcanoclastic series. Finally, major granitic intrusions emplaced in the basement rocks at around 298 ± 4 Ma. The study contributes to clarify stratigraphic constraints of late Carboniferous to early Permian continental deposits and sheds light on stratigraphy of significant late Paleozoic volcanic deposits of the Flechtingen-Altmark Subprovince in the Southern Permian Basin.
    Keywords: ddc:554.3 ; Southern Permian Basin ; Late Paleozoic volcanism ; Andesite ; Sill ; Peperite ; Caldera
    Language: English
    Type: doc-type:article
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  • 6
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    Amphibian biostratigraphy of the European Permo-Carboniferous (2007)
    In:  Geological Society Special Publication 265: 201-215.
    Details
    Publication Date: 2007-10-08
    Description: A revised amphibian zonation for the European Pennsylvanian and Cisuralian (Upper Carboniferous to Lower Permian) with nine amphibian zones is presented. The index fossils belong to species-chronoclines with two or three closely related species. The time resolution of these amphibian zones is about 1.5-3.0 Ma. Biostratigraphical correlations with amphibian zones are applicable to 16 basins in the Czech Republic, Poland, France, Italy and Germany. The biostratigraphical potential of other tetrapods is discussed.
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  • 7
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    Insect biostratigraphy of the Euramerican continental Late Pennsylvanian and Early Permian (2007)
    In:  Geological Society Special Publication 265: 325-336.
    Details
    Publication Date: 2007-10-08
    Description: An insect zonation with a time resolution of 1.5-2 Ma for Late Pennsylvanian to Early Permian (Kasimovian to Artinskian) non-marine deposits is presented. The zonation is based on the directed morphogenetic evolution of colour pattern in the forewings of the blattid (cockroach) family Spiloblattinidae. This evolution is observed in lineages of succeeding species of three genera. All three genera are widely distributed in the palaeo-equatorial zone from Europe to North America, that is, in the Euramerican biota province. Increasing reports of spiloblattinid zone species in condont-bearing, interfingered marine/continental strata of North American Appalachian, Mid-Continent and West Texas basins could be the key to direct biostratigraphical correlations of pure continental profiles, as are present in the most parts of the Hercynides, to the global marine scale.
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  • 8
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    Non-marine Permian biostratigraphy and biochronology: an introduction (2007)
    In:  Geological Society Special Publication 265: 1-14.
    Details
    Publication Date: 2007-10-08
    Description: The Permian time scale based on marine rocks and fossils is well defined and of global utility, but non-marine Permian biostratigraphy and chronology is in an early phase of development. Non-marine Permian strata are best known from western Europe and the western United States, but significant records are also known from Russia, South Africa, China and Brazil. Global time terms based on non-marine Permian strata, such as Rotliegend, Zechstein, Autunian, Saxonian and Thuringian, are either inadequately defined or poorly characterized and should only be used as lithostratigraphic terms. Macro- and microfloras have long been important in non-marine Permian correlations, but are subject to limitations based on palaeoprovinciality and facies/climatic controls. Charophytes, conchostracans, ostracodes and freshwater bivalves have a potential use in non-marine Permian biostratigraphy but are limited by their over-split taxonomy and lack of well-established stratigraphic distributions of low-level taxa. Tetrapod footprints provide poor biostratigraphic resolution during the Permian, but tetrapod body fossils and insects provide more detailed biostratigraphic zonations, especially in the Lower Permian. Numerous radioisotopic ages are available from non-marine Permian sections and need to be more precisely correlated to the global time scale. The Middle Permian Illawarra reversal and subsequent magnetic polarity shifts are also of value to correlation. There needs to be a concerted effort to develop non-marine Permian biostratigraphy, to correlate it to radio-isotopic and magnetostratigraphic data, and to cross-correlate it to the marine time scale.
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  • 9
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    Permo-Carboniferous climate: Early Pennsylvanian to Late Permian climate development of central Europe in a regional and global context (2007)
    In:  Geological Society Special Publication 265: 95-136.
    Details
    Publication Date: 2007-10-08
    Description: A well-justified stratigraphical correlation of continental successions and new palaeogeographic reconstruction of Pangaea reveal new insights into the northern Pangaean climate development influenced by palaeogeography, palaeotopography, glacio-eustatic sealevel changes and ocean currents. The overall Permo-Carboniferous aridization trend was interrupted by five wet phases. These are linked to the Gondwana icecap. The aridization and weakening of wet phases over time were not only caused by the drift of northern Pangaea to the arid climatic belt, but also by the successive closure of the Rheic Ocean, which caused the expansion of arid/semi-arid environments in the Lower/Middle Permian. The end of the Gondwana glaciation rearranged ocean circulation, leading to a cold, coast-parallel ocean current west of northern Pangaea, blocking moisture coming with westerly winds. The maximum of aridity was reached during the Roadian/Wordian. The Trans-Pangaean Mountain Belt was non-existent. Its single diachronous parts never exceeded an average elevation of 2000 m. The maximum elevation shifted during time from east to west. The Hercynian orogen never acted as an orographic east-west barrier, and the Inter-Tropical Convergence Zone was widely displaced, causing four seasons (dry summer/winter, wet spring/autumn) at the equator and a strong monsoon system.
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  • 10
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    Late Triassic ichnoassemblage from a playa-lake system of the Coastal Meseta, Morocco: Palaeoenvironmental and palaeoecological implications (2020)
    Elsevier
    Details
    Publication Date: 2020-12-01
    Print ISSN: 1464-343X
    Electronic ISSN: 1879-1956
    Topics: Geosciences
    Published by Elsevier
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