http://www.cnr.it/ontology/cnr/individuo/prodotto/ID186202
Environmental factors influencing skeletal grain sediment associations: a critical review of Miocene examples from the western Mediterranean (Articolo in rivista)
- Type
- Label
- Environmental factors influencing skeletal grain sediment associations: a critical review of Miocene examples from the western Mediterranean (Articolo in rivista) (literal)
- Anno
- 2004-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.1111/j.1365-3091.2004.00640.x (literal)
- Alternative label
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- POMAR L; M. BRANDANO; WESTPHAL H (literal)
- Pagina inizio
- Pagina fine
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
- Rivista
- Note
- ISI Web of Science (WOS) (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- IGAG-Cnr, La Sapienza Università di Roma, UIB, Institut fu¨ r Geologie und Pala¨ ontologie, Hannover, (literal)
- Titolo
- Environmental factors influencing skeletal grain sediment associations: a critical review of Miocene examples from the western Mediterranean (literal)
- Abstract
- The presence of foramol, rhodalgal and bryomol skeletal grain associations in
ancient shallow-marine limestones is commonly interpreted as evidence for
non-tropical palaeoclimate, despite temperature being only one of several
factors influencing skeletal grain associations. Such interpretations neglect
the multitude of factors other than temperature that influence carbonateproducing
biota. These include nutrients, water energy, water transparency,
depth of the sea floor, salinity, oxygen, Ca2+ and CO2 concentrations, Mg/Ca
ratio, alkalinity, substrate requirements, competitive displacement as well as
biological and evolutionary trends. This uniformitarian approach also
disregards the probability that conditions of present-day biological systems
may not be representative of past conditions of analogous systems. Here, the
importance of considering these other factors is illustrated through two
examples of carbonate platforms in the western Mediterranean. These
platforms are dominated by foramol, rhodalgal and bryomol associations of
Miocene age in spite of having formed in tropical conditions. The platforms
discussed are: (1) the Lower Tortonian ramp on Menorca, Balearic Islands;
and (2) the Lower-Middle Miocene ramps of the central Apennines, Italy.
Evidence for tropical conditions in the Mediterranean during the period of
growth of these platforms is provided by species of red algae and larger
foraminifera, by data from coeval continental basins and by global oxygen
isotope data. (literal)
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- Autore CNR
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