LATE APTIAN RADIOLITIDAE (RUDIST BIVALVES) FROM THE MEDITERRANEAN ANDSOUTHWEST ASIATIC REGIONS - TAXONOMIC, BIOSTRATIGRAPHIC AND PALEOBIOGEOGRAPHIC ASPECTS
Jp. Masse et Mg. Maresca, LATE APTIAN RADIOLITIDAE (RUDIST BIVALVES) FROM THE MEDITERRANEAN ANDSOUTHWEST ASIATIC REGIONS - TAXONOMIC, BIOSTRATIGRAPHIC AND PALEOBIOGEOGRAPHIC ASPECTS, Palaeogeography, palaeoclimatology, palaeoecology, 128(1-4), 1997, pp. 101-110
The onset of the Radiolitidae in the mid-Aptian was subsequently follo
wed by a diversification and a geographic spreading of the group durin
g the late Aptian. From the Mediterranean and Southwest Asian regions
are recorded four species of Eoradiolites and one species of Praeradio
lites, all well defined. Moreover at least two species of Eoradiolites
and two species of Praeradiolites, with a poorly defined taxonomic st
atus, are also present. The geographic distribution of the Mediterrane
an faunas runs from Southern France, Spain, Italy, Bosnia, East Serbia
, Lebanon to Algeria. The southwest Asian faunas are documented from W
estern China, North India, Pakistan, Afghanistan and Iran. The age of
the radiolitid-bearing localities is discussed and/or documented after
micropalaeontological assemblages. Mediterranean and Southwest Asian
faunas are remarkably different: the former group is dominated by typi
cal cellular shelled forms (Eoradiolites katzeri-E. plicatus being the
cardinal taxa) whereas the latter is dominated by acellular forms (Eo
radiolites gilgitensis being the cardinal taxon). Palaeogeographic rec
onstruction of the late Aptian palaeoenvironments place the Mediterran
ean fauna on the northern and the southern margin of the ''Mediterrane
an Seuil'' without any significant dissimilarities in composition, whi
le the southwest Asian faunas are restricted to the northern margin of
Tethys. These two bioprovinces are both located in the tropical domai
n of the northern hemisphere. The existence in southern Russia of a wi
de marine embayment connected to high latitude cool waters suggests a
possible thermal barrier between the Southwest Asian and Mediterranean
faunas, close to the Caucasus. The corresponding faunal groups, with
common origin, could have derived from isolation of founder population
s coupled with some adaptive divergence during the rapid dispersion of
the family at an early stage of evolutionary maturity.