MACNBR   00242
MUSEO ARGENTINO DE CIENCIAS NATURALES "BERNARDINO RIVADAVIA"
Unidad Ejecutora - UE
artículos
Título:
Fossil bee cells from the Canary Islands. Ichnotaxonomy, palaeobiology and palaeoenvironments of Palmiraichnus castellanosi
Autor/es:
FRANCISCO LA ROCHE; JORGE F. GENISE; CAROLINA CASTILLO; MARIA LUISA QUESADA; CRISTO GARCÍA GOTERA; JULIO DE LA NUEZ
Revista:
PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
Editorial:
ELSEVIER SCIENCE BV
Referencias:
Lugar: Amsterdam; Año: 2014 vol. 409 p. 249 - 249
ISSN:
0031-0182
Resumen:
Fossil bee cells, attributable to the ichnospecies Palmiraichnus castellanosi, are recorded from the Pleistocene and Holocene of the easternmost Canary Islands. Cells bear a chamberwith internal smooth lining, spiral closure, andan antechamber. They have a discretewall that surrounds both the chamber and antechamber. The antechamber shows an internal smooth surface and a structureless filling of palaeosol material. These features enable this materialto be assigned to the ichnospecies P. castellanosi, originally described fromthe Palaeogene of Uruguay. This record constitutes the first documented evidence for bees, and Hymenoptera, in the Quaternary of the Canaries and the first for this ichnospecies fromAfrica. By comparisonwith extant cells, the potential constructors are bees of the genus Andrena (Andrenidae). Palaeoecological and statistical data suggest that five species may have produced P. castellanosi in the Canary Islands. One on Lanzarote in the Holocene, another in south Fuerteventura in the Upper Pleistocene, two on Gran Canaria and another onMontaña Clara islet during theMiddle Pleistocene. A high level of breeding success was probably favoured by the lack of predators or parasites and optimal environmental conditions, at least in the Pleistocene. During the Pleistocene, the abundance of P. castellanosi in the lowlands suggests a rich endemic shrubby flora and palaeoclimatic conditions similar to the present, but probablywith a higher humidity. The land-snail assemblage associatedwith lowdensities of P. castellanosi in the Holocene mid-altitude belt suggests a cool moist palaeoenvironment, less favourable for P. castellanosi producers.