Microspinosporites, a new genus of Palaeozoic pseudosaccate miospores of flemingitalean affinity

Result code in IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F13%3A00394259" target="_blank" >RIV/67985831:_____/13:00394259 - isvavai.cz</a>

Result on the web

<a href="http://dx.doi.org/10.3140/bull.geosci.1365" target="_blank" >http://dx.doi.org/10.3140/bull.geosci.1365</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.3140/bull.geosci.1365" target="_blank" >10.3140/bull.geosci.1365</a>

Result language

angličtina

Original language name

Microspinosporites, a new genus of Palaeozoic pseudosaccate miospores of flemingitalean affinity

Original language description

Pennsylvanian microspinate/spinate mio- and microspores are formerly assigned to cingulate species of Lycospora (Schopf et al.), which were described by Potonie & Kremp. In the present paper, from the three existing species of distally microspinate miospores of this type [L. granulata Kosanke, L. orbicula (Potonie & Kremp) Smith & Butterworth and L. chaloneri Scott & Hemsley] two of them, L. orbicula and L. chaloneri are assigned to new pseudosaccate miospore genus Microspinosporites gen. nov. Miosporesof this genus are characterized by inner body and distal and proximal microspinae/spinae, except for the contact area.Acingulum is not developed. The fructifications that produced Microspinosporites were bisporangiate cones of the genera Flemingites Carruthers and probably Moscvostrobus Naugolnykh & Orlova, and were born on arborescent lycopsids of the genus Paralycopodites (Moorey & Moorey) DiMichele. The morphology of Microspinosporites is similar to that of e.g., Geminospora (Balme)

Czech name

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Czech description

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Type

J_x - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)

CEP classification

DB - Geology and mineralogy

OECD FORD branch

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Project

<a href="/en/project/GAP210%2F12%2F2053" target="_blank" >GAP210/12/2053: High-resolution floristic changes as a response to climatic dynamics during the Late Palaeozoic ice age recorded in the basins of the Bohemian Massif</a><br>

Continuities

Z - Vyzkumny zamer (s odkazem do CEZ)<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Publication year

2013

Confidentiality

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

Name of the periodical

Bulletin of Geosciences

ISSN

1214-1119

e-ISSN

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Volume of the periodical

88

Issue of the periodical within the volume

3

Country of publishing house

CZ - CZECH REPUBLIC

Number of pages

9

Pages from-to

573-581

UT code for WoS article

000321252500007

EID of the result in the Scopus database

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