Herpetologická společenstva pliocénu až středního pleistocénu střední Evropy: paleoekologický význam

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F07%3A00022759" target="_blank" >RIV/00216224:14310/07:00022759 - isvavai.cz</a>

Výsledek na webu

—

DOI - Digital Object Identifier

—

Jazyk výsledku

angličtina

Název v původním jazyce

Herpetological assemblages from the Pliocene to middle Pleistocene in Central Europe: palaeoecological significance

Popis výsledku v původním jazyce

The extinction event at the Early/Late Pliocene boundary (MN 15/MN 16) distinctively affected especially the southern part of Central Europe (the last occurrences of Albanerpeton pannonicus, Mertensiella mera, and Latonia gigantea). Several other taxa died out during MN 16 zone. This Pliocene extinction is a result of deterioration of climatic conditions with the process of aridization playing, most probably, the key role. Because numerous taxa became extinct long before the beginning of the Pleistoceneduring the MN 15 and MN 16 zones, the Pliocene/Pleistocene transition (ca 1.8 Ma) is not reflected in the evolution of Central European herpetological assemblages. Herpetological assemblages fundamentally changed during the terminal part of the Early Biharian (Early Pleistocene) when several Pliocene and Early Biharian representatives became extinct. In the Late Biharian herpetological assemblages no extant mediterranean taxa have been reported from Central European localities situated

Název v anglickém jazyce

Herpetological assemblages from the Pliocene to middle Pleistocene in Central Europe: palaeoecological significance

Popis výsledku anglicky

The extinction event at the Early/Late Pliocene boundary (MN 15/MN 16) distinctively affected especially the southern part of Central Europe (the last occurrences of Albanerpeton pannonicus, Mertensiella mera, and Latonia gigantea). Several other taxa died out during MN 16 zone. This Pliocene extinction is a result of deterioration of climatic conditions with the process of aridization playing, most probably, the key role. Because numerous taxa became extinct long before the beginning of the Pleistoceneduring the MN 15 and MN 16 zones, the Pliocene/Pleistocene transition (ca 1.8 Ma) is not reflected in the evolution of Central European herpetological assemblages. Herpetological assemblages fundamentally changed during the terminal part of the Early Biharian (Early Pleistocene) when several Pliocene and Early Biharian representatives became extinct. In the Late Biharian herpetological assemblages no extant mediterranean taxa have been reported from Central European localities situated

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

EH - Ekologie – společenstva

OECD FORD obor

—

Projekt

—

Návaznosti

Z - Vyzkumny zamer (s odkazem do CEZ)

Rok uplatnění

2007

Kód důvěrnosti údajů

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

Název periodika

Geodiversitas

ISSN

1280-9659

e-ISSN

—

Svazek periodika

29

Číslo periodika v rámci svazku

2

Stát vydavatele periodika

FR - Francouzská republika

Počet stran výsledku

24

Strana od-do

297-320

Kód UT WoS článku

—

EID výsledku v databázi Scopus

—