Amber and the Cretaceous Resinous Interval
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00023272%3A_____%2F23%3A10136065" target="_blank" >RIV/00023272:_____/23:10136065 - isvavai.cz</a>
Výsledek na webu
<a href="https://www.sciencedirect.com/science/article/pii/S0012825223001757?via%3Dihub" target="_blank" >https://www.sciencedirect.com/science/article/pii/S0012825223001757?via%3Dihub</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1016/j.earscirev.2023.104486" target="_blank" >10.1016/j.earscirev.2023.104486</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Amber and the Cretaceous Resinous Interval
Popis výsledku v původním jazyce
Amber is fossilized resin that preserves biological remains in exceptional detail, study of which has revolutionized understanding of past terrestrial organisms and habitats from the Early Cretaceous to the present day. Cretaceous amber outcrops are more abundant in the Northern Hemisphere and during an interval of about 54 million years, from the Barremian to the Campanian. The extensive resin production that generated this remarkable amber record may be attributed to the biology of coniferous resin producers, the growth of resiniferous forests in proximity to transitional sedimentary environments, and the dynamics of climate during the Cretaceous. Here we discuss the set of interrelated abiotic and biotic factors potentially involved in resin production during that time. We name this period of mass resin production by conifers during the late Mesozoic fundamental as an archive of terrestrial life, the 'Cretaceous Resinous Interval' (CREI).
Název v anglickém jazyce
Amber and the Cretaceous Resinous Interval
Popis výsledku anglicky
Amber is fossilized resin that preserves biological remains in exceptional detail, study of which has revolutionized understanding of past terrestrial organisms and habitats from the Early Cretaceous to the present day. Cretaceous amber outcrops are more abundant in the Northern Hemisphere and during an interval of about 54 million years, from the Barremian to the Campanian. The extensive resin production that generated this remarkable amber record may be attributed to the biology of coniferous resin producers, the growth of resiniferous forests in proximity to transitional sedimentary environments, and the dynamics of climate during the Cretaceous. Here we discuss the set of interrelated abiotic and biotic factors potentially involved in resin production during that time. We name this period of mass resin production by conifers during the late Mesozoic fundamental as an archive of terrestrial life, the 'Cretaceous Resinous Interval' (CREI).
Klasifikace
Druh
J<sub>imp</sub> - Článek v periodiku v databázi Web of Science
CEP obor
—
OECD FORD obor
10506 - Paleontology
Návaznosti výsledku
Projekt
—
Návaznosti
V - Vyzkumna aktivita podporovana z jinych verejnych zdroju
Ostatní
Rok uplatnění
2023
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Earth-Science Reviews
ISSN
0012-8252
e-ISSN
—
Svazek periodika
2023
Číslo periodika v rámci svazku
243
Stát vydavatele periodika
NL - Nizozemsko
Počet stran výsledku
15
Strana od-do
1-15
Kód UT WoS článku
001035782100001
EID výsledku v databázi Scopus
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