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Lesleya Lesquereux from the Late Carboniferous of the Iberian Massif: an upland macroflora from the Variscan orogen

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F16%3A00000052" target="_blank" >RIV/00025798:_____/16:00000052 - isvavai.cz</a>

  • Result on the web

    <a href="http://dx.doi.org/10.1139/cjes-2015-0213" target="_blank" >http://dx.doi.org/10.1139/cjes-2015-0213</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1139/cjes-2015-0213" target="_blank" >10.1139/cjes-2015-0213</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Lesleya Lesquereux from the Late Carboniferous of the Iberian Massif: an upland macroflora from the Variscan orogen

  • Original language description

    The Carboniferous – early Permian plant genus Lesleya is a characteristic component of “dryland floras” that occupied a wide range of moisture-stressed, well-drained environments in tropical regions of Euramerica. Fossil records of Lesleya are almost exclusively found in basinal lowlands. For example, occurrences in Early Pennsylvanian-age, seasonally dry, parautochthonous deposits in basinal lowlands of North America (e.g., Illinois Basin, USA) indicate that Lesleya lived in that region in low-altitude (lowland) paleoenvironments during dry climatic intervals. In this paper, we document the first occurrence of Lesleya during the Carboniferous on the Iberian Massif, in lower Gzhelian (Upper Pennsylvanian) strata of the Douro Carboniferous Basin, in northwestern Portugal. This newly discovered occurrence includes a new species, Lesleya iberiensis sp. nov., recognized on the basis of natural molds of leaves. The Portuguese Lesleya fossils are from upland intramontane deposits and occur between coal beds. Their fossil remains are preserved in mica-rich shales that were deposited between sandstone-dominated fluvial and shale-dominated lacustrine deposits, suggesting that this megaflora was deposited near freshwater bodies. These new data provide evidence that this megaflora grew in mountain riparian environments within the Variscan orogen, either in localized, well-drained areas or during drier climatic intervals in the Late Pennsylvanian.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)

  • CEP classification

    DB - Geology and mineralogy

  • OECD FORD branch

Result continuities

  • Project

    <a href="/en/project/GAP210%2F10%2F0232" target="_blank" >GAP210/10/0232: Cordaitalean and pteridosperm cuticular analysis and their "in situ" prepollen</a><br>

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2016

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Canadian Journal of Earth Sciences

  • ISSN

    0008-4077

  • e-ISSN

  • Volume of the periodical

    53

  • Issue of the periodical within the volume

    9

  • Country of publishing house

    CA - CANADA

  • Number of pages

    13

  • Pages from-to

    883-895

  • UT code for WoS article

    000382753100002

  • EID of the result in the Scopus database