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Contributions to Zoology, 72 (2/3) (2003)

Macrurans (Crustacea, Decapoda) from the Lower Triassic (Olenekian) of the Ambilobé area (NW Madagascar)

Alessandro Garassino , Giovanni Pasini , Giorgio Teruzzi

Dipartimento di Paleontologia degli Invertebrati, Museo civico di Storia naturale, C.so Venezia 55, I-20121 Milano, Italy

Museo Civico dei Fossili di Besano, Via Prestini 5, I-21050 Besano (Varese), Italy

Keywords: Crustacea, Decapoda, Triassic, Madagascar

Abstract


Fossil decapods of the Lower Triassic marine strata of Madagascar are reviewed. These display affiliation to the dendrobranchiates. These include Antrimpos madagascariensis, two species of Ifasya (I. madagascariensis and I. straeleni) and Ambilobeia karojoi.

Introduction


Fossiliferous levels within Lower Triassic marine strata to the south/south-west of the village of Ambilobé, c. 150 km SW of Diego Suarez (Antsiranana, Madagascar) have long been known (Besairie, 1932). Beltan (1996) proposed a Dienerian (Early Triassic) age for the fossil-bearing beds in the Ambilobé area, based on correlation with the Lystrosaurus and Cynognathus zones of the Beaufort Group (Battail et al., 1987). Recently, Yanbin et al. (2002) have studied some conchostracans from this area, and assigned them to Euestheria (Magniestheria) truempyi (Kozur & Seidel, 1983). In view of the fact that this species has previously been recorded also from the Bernburg Formation (lowermost Olenekian) in the German Basin, we may date the Ambilobé faunal assemblage as Olenekian rather than Induan (Dienerian).

This famous faunal assemblage, which comprises invertebrates (ammonites, nautiloids, bivalves, serpulids, decapod crustaceans, thylacocephalans, cycloids, limulids and conchostracans) and vertebrates (mostly fish and rare amphibians), is found in the westernmost outcrops of a band of sedimentary rocks, roughly between the small villages of Anaborano Ifasy in the south west and of Bobasatrana in the northeast.

Results


The first description of decapod crustaceans from the Lower Triassic of Madagascar is that by van Straelen (1933), who recorded two incomplete specimens from the Ambilobé area, referring both to a new species, Antrimpos madagascariensis. Garassino & Teruzzi (1995) carried on this study, having available a sample of 400 specimens, in part collected during a field trip in 1989 organised by the Dipartimento di Paleontologia degli Invertebrati del Museo civico di Storia naturale di Milano and in part collected earlier by one of us (GP). In this assemblage, the genus Ifasya Garassino & Teruzzi, 1995 was recognised, with the species I. madagascariensis (van Straelen, 1933) and I. straeleni Garassino & Teruzzi, 1995 (Fig. 1).

FIG2

Fig. 1. Macruran decapod crustaceans from the Lower Triassic of the Ambilobé area, NW Madagascar (from to top to bottom): Ifasya madagascariensis (van Straelen, 1933), I. straeleni Garassino & Teruzzi, 1995, and Ambilobeia karojoi Garassino & Pasini, 2002.

Recently, Garassino & Pasini (2002) have studied a single specimen collected from a new outcrop near the village of Bobasatrana. This show certain morphological features, e.g., elongate rostrum without supra- and sub-rostral teeth, strong tooth at base of rostrum, pereiopods I-III with short and stout chelae) that set it apart from species of Ifasya. To contain this species, the genus Ambilobeia Garassino & Pasini, 2002, was erected (type species: A. karojoi Garassino & Pasini, 2002; see Fig. 1). Only the Late Triassic genus Antrimpos von Münster, 1839 might show certain morphological affinities in the shape of rostrum and body with the new genus. However, a rostrum with supra- and sub-rostral teeth, the presence of one strong antennal spine and of hepatic, orbito-antennal and gastro-frontal grooves distinguish Antrimpos from Ambilobeia.

References


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