Search Results - Serpukhov*

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  1. 1

    Conodonts of the genus Lochriea in Ireland and the recognition of the Viséan–Serpukhovian (Carboniferous) boundary by Barham, Milo, Murray, J., Sevastopulo, G., Williams, D.

    Published 2014
    “…In particular, L. ziegleri is regarded as the most suitable index taxon for recognition of a revised Viséan-Serpukhovian boundary and selection of a Global Stratotype Section and Point. …”
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  2. 2

    Correlation of the base of the Serpukhovian Stage (Mississippian) in NW Europe by Sevastopulo, G., Barham, Milo

    Published 2013
    “…Although there is some discrepancy in the recorded levels of the FOD of L. ziegleri in NW Europe, this may be as a result of collection failure. The base of the Serpukhovian based on the FAD of Lochriea ziegleri will be in the middle of the Brigantian regional Substage.…”
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  3. 3

    The prospectivity of a potential shale gas play: An example from the southern Pennine Basin (central England, UK) by Hennissen, Jan A.I., Hough, Edward, Vane, Christopher H., Leng, Melanie J., Kemp, Simon J., Stephenson, Michael H.

    Published 2017
    “…During the Serpukhovian (late Mississippian) Stage, the Pennine Basin, now underlying much of northern England, consisted of a series of interlinked sub-basins that developed in response to the crustal extension north of the Hercynic orogenic zone. …”
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  4. 4

    The onset of the permo-carboniferous glaciation: Reconciling global stratigraphic evidence with biogenic apatite δ18O records in the late Visean by Barham, Milo, Murray, J., Joachimski, M., Williams, D.

    Published 2012
    “…Both conodont and microfossil fish δ18Oapatite indicate stabilization of an ‘icehouse’ climate during the Brigantian and into the Serpukhovian. Substantial late Visean cooling identified herein is in good agreement with global glacioeustatic records.…”
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  5. 5

    Posidonomya (Bivalvia) from Northwest Peninsular Malaysia and its significance by Basir Jasin

    Published 2015
    “…The age of Posidonomya from Peninsular Malaysia is comparable to those of Europe, Morocco, Turkey and South China which range from Tournaisian to Serpukhovian, Early Carboniferous. The fossil specimens exhibit morphological features closely related to Posidonomya becheri Bronn. …”
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