Re: Mediterranean flood

mortongr@flash.net
Fri, 29 Oct 1999 22:12:56 +0000

The other day, I was challenged concerning the paleodepths of the lowermost
section at Alba, Italy where the eel was found and the site that I used to
show that life could exist in a desciccated Mediterranean. The suggestion
was made that the area had not been more than 500 feet deep (150 m). I did
some more research and found this for the strata in an area just south of
Alba. Group C describes the Tortonian strata. For those who don't know the
Tortonian strat is where the lampfish were found and it confirms the depths
I was speaking of.

"Benthic foraminifers were also considered, mostely as bathymetric
indicators. In the upper part of Group and in group B, the most common
forms are: Cibicidoides, Anomalinoides, Gyroidinoides, Lenticulina,
Stilostomella, Heterolepa, Uvigerina, Planulina and Karreriella. The
plankton/benthos ratio varies between 2 and 6. IN the mudstones of Group C,
Lenticulinae are very common with a great number of species, followed by
NOdosariids and Uvigerinae, with a mean plankton/benthos ratio of 8.
"Similar associations are considered indicative of the upper bathyal zone
with depth range between 200 and 600 m. The presence of differentiated
species of Uvigerina in the whole succession is particularly important
because it may exclude depths shallower than 200 m." M. Gnaccolini et al,
"Sequence Stratigraphy of the Langhe Oligo-Miocene Succession, Tertiary
Piedmont BAsin, NOrthern Italy," in Mesozoic and Cenozoic Sequence
Stratigraphy of European BAsins, SEPM Special PUblications No 60, p.
233-244, p. 242

200-600 m is a range of 650-1950 feet. the center of that range is in the
neighborhood of 1300 feet deep
glenn

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