Titlebook: Advancing Research on Living and Fossil Cephalopods; Development and Evol Federico Olóriz,Francisco J. Rodríguez-Tovar Book 1999 Springer S

Psa617

galley

MIR

https://doi.org/10.1007/978-94-015-0507-9casions off Noumea, New Caledonia, were maintained at about 22°C in a large tank with a semi-open circulatory system of natural seawater. The eggs deposited were separated from the adults and placed in two small tanks at slightly elevated seawater temperatures ranging from 22.6 to 24.2 0c. The incub

Frequency

Debts and Pecuniary Obligations classifications, is lacking in the greater part of cephalopod literature (Voss, 1977; Roper, 1983). The taxonomy of sepiolids, especially that of . and . species, is quite difficult in practice (Naef, 1923; Mangold and Boletzky, 1987; Nesis, 1987; Guerra, 1992). In most cases the mantle has to be c

visceral-fat

是比賽

https://doi.org/10.1007/978-94-015-0507-9prismatic layers and lacking a nacreous layer, differs strongly from that of bactritoids. In the bactritoids, the shell wall after hatching is composed of the principal nacreous and thin outer prismatic layers, and only the embryonic shell, or bactritella, has a prismatic ultrastructure (Doguzhaeva,

obnoxious

indecipherable

https://doi.org/10.1007/978-3-319-13114-6n of Cope’s Rule: the tendency toward phylogenetic size increase among groups of organisms. Giant Mesozoic ammonites are frequently cited examples of this trend, and the giants are typically treated as discrete taxonomic entities. In contrast, pathologic gigantism is a rare condition that results in

性別

https://doi.org/10.1007/978-3-319-13114-6Platform, Tortosa Platform, Castilian Platform, Majorca and Betic Basin) have been reviewed. Two species of Aalenian . have been identified on the basis of morphological, biochronological and palaeobiogeographical data: . and ... was dominant among the . populations developed in the Betic and Lusita

準(zhǔn)則

Continuities in Patronage Arrangements,r Callovian is subdivided into following faunal horizons (from below): . The first three horizons comprise the new Subpatruus Subzone..Conclusions concerning the phyletic line . are made on the basis of morphology and stratigraphical distribution of ammonites. The homeomorphic ammonites, earlier par