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
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Czech description
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Classification
Type
J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)
CEP classification
DB - Geology and mineralogy
OECD FORD branch
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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
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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
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