Microboring organisms — an overlooked Early-Mid Palaeozoic marine ecosystem: Case study from the Prague Basin (Czech Republic)

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F24%3A00598711" target="_blank" >RIV/67985831:_____/24:00598711 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/67985831:_____/23:00570597 RIV/00023272:_____/24:10136055 RIV/00216208:11310/24:10492058 RIV/49777513:23420/24:43969009 RIV/00025798:_____/24:10169106

Výsledek na webu

<a href="https://www.sciencedirect.com/science/article/pii/S1871174X23000100?via%3Dihub" target="_blank" >https://www.sciencedirect.com/science/article/pii/S1871174X23000100?via%3Dihub</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1016/j.palwor.2023.01.010" target="_blank" >10.1016/j.palwor.2023.01.010</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Microboring organisms — an overlooked Early-Mid Palaeozoic marine ecosystem: Case study from the Prague Basin (Czech Republic)

Popis výsledku v původním jazyce

Nearly 800 of Ordovician to Middle Devonian petrographic slides from the Prague Basin (Barrandian area, Czech Republic) have been inspected for the presence of microboring structures in bioclasts. Traces of microbioerosion are rare in the Ordovician to Lower Devonian of the studied area and are produced almost exclusively by bacteria and fungi on bioclast surfaces. However, a gradual increase in the abundance of microboring structures and their shift into bioclast interior is observed during the Silurian to the Early Devonian interval. This coincides with a generally ascending quantity of tunnels possibly produced by phototrophic microboring organisms (Cyanobacteria and Algae). Subsequently, the abundance of microendolithic structures notably increased from the Emsian onwards. They are not randomly distributed in relation to their palaeoenvironments, with most abundant occurrences in low-energy hemipelagic red carbonates. Although this may partially reflect the global marine evolutionary trends, the changes in microbioeroder ecosystems were more likely driven by local factors such as the drift of the Prague Basin from temperate to tropical climate zone, increased oxygen content near the sea floor or to a larger extent, the preserved shallow littoral facies.

Název v anglickém jazyce

Microboring organisms — an overlooked Early-Mid Palaeozoic marine ecosystem: Case study from the Prague Basin (Czech Republic)

Popis výsledku anglicky

Nearly 800 of Ordovician to Middle Devonian petrographic slides from the Prague Basin (Barrandian area, Czech Republic) have been inspected for the presence of microboring structures in bioclasts. Traces of microbioerosion are rare in the Ordovician to Lower Devonian of the studied area and are produced almost exclusively by bacteria and fungi on bioclast surfaces. However, a gradual increase in the abundance of microboring structures and their shift into bioclast interior is observed during the Silurian to the Early Devonian interval. This coincides with a generally ascending quantity of tunnels possibly produced by phototrophic microboring organisms (Cyanobacteria and Algae). Subsequently, the abundance of microendolithic structures notably increased from the Emsian onwards. They are not randomly distributed in relation to their palaeoenvironments, with most abundant occurrences in low-energy hemipelagic red carbonates. Although this may partially reflect the global marine evolutionary trends, the changes in microbioeroder ecosystems were more likely driven by local factors such as the drift of the Prague Basin from temperate to tropical climate zone, increased oxygen content near the sea floor or to a larger extent, the preserved shallow littoral facies.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10506 - Paleontology

Projekt

—

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2024

Kód důvěrnosti údajů

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

Název periodika

Palaeoworld

ISSN

1871-174X

e-ISSN

1875-5887

Svazek periodika

33

Číslo periodika v rámci svazku

1

Stát vydavatele periodika

NL - Nizozemsko

Počet stran výsledku

18

Strana od-do

39-56

Kód UT WoS článku

001170245100001

EID výsledku v databázi Scopus

2-s2.0-85148892183