Sie befinden Sich nicht im Netzwerk der Universität Paderborn. Der Zugriff auf elektronische Ressourcen ist gegebenenfalls nur via VPN oder Shibboleth (DFN-AAI) möglich. mehr Informationen...
Ergebnis 2 von 93

Details

Autor(en) / Beteiligte
Titel
The Messinian stromatolites of the Sierra del Colmenar (Western Mediterranean): facies characterization and sedimentological interpretation
Ist Teil von
  • PeerJ (San Francisco, CA), 2018-10, Vol.6, p.e5766-e5766, Article e5766
Ort / Verlag
United States: PeerJ. Ltd
Erscheinungsjahr
2018
Link zum Volltext
Quelle
Electronic Journals Library
Beschreibungen/Notizen
  • A representative outcrop of the Messinian stromatolites belonging to the Terminal Carbonate Complex unit, from the northern sector of the Bajo Segura basin ( section, Sierra del Colmenar, SE Spain) has been studied. Here, we present a detailed analysis of the architecture, external morphology, and internal morphology in order to reconstruct the environmental and palaeoecological conditions for their growth. The stromatolites macrostructure consists of a continuously doming type morphology (build up and sheets areas). These developed close to the coast and acted as a palaeogeographic barrier, reducing physical stress, channeling the erosive effect of water and favoring restricted conditions. This stromatolitic macrostructure exhibits variations in its internal morphology, giving rise to seven subfacies, which are a product of the environmental changes experienced during the growth of the microbial mats. Although broadly suggesting a coastal environment, restricted and shallow during formation, the variation in internal morphology (mesostructure and microstructure) is evidence of minor changes in the physical environment that indicate a progressive shallowing.
Sprache
Englisch
Identifikatoren
ISSN: 2167-8359
eISSN: 2167-8359
DOI: 10.7717/peerj.5766
Titel-ID: cdi_doaj_primary_oai_doaj_org_article_2232c1aef50343f1bc55dfbd541dfcec

Weiterführende Literatur

Empfehlungen zum selben Thema automatisch vorgeschlagen von bX