MACNBR   00242
MUSEO ARGENTINO DE CIENCIAS NATURALES "BERNARDINO RIVADAVIA"
Unidad Ejecutora - UE
artículos
Título:
New fossil record of the Lactoridaceae in southern South America: a paleobiogeographic approach.
Autor/es:
GAMERRO, J.C.; BARREDA, V.
Revista:
BOTANICAL JOURNAL OF THE LINNEAN SOCIETY
Referencias:
Año: 2008 vol. 158 p. 41 - 50
ISSN:
0024-4074
Resumen:
Lactoridaceae is a monotypic family confined to the Masatierra Island, Juan Fernández
archipelago, in the Pacific Ocean. It grows in the understorey of a subtropical montane
rain forest. Lactoridaceae most likely originated in southern South Africa in the
Cretaceous, with the oldest records in the Turonian-Campanian, and reached its widest
paleogeographic distribution by the Maastrichtian, extending into Australia, India,
Antarctica and North and South America. Here we report a new fossil find of
lactoridaceous tetrads from the Early Miocene of eastern Patagonia, southern South
America. This record is the youngest, and geographically one of the closest to the extant
Lactoris distribution area. Patagonian fossil material shows greater similarities to extantdistribution area. Patagonian fossil material shows greater similarities to extant
L. fernandeziana Phil. than any other described morphotaxon. The family may have
migrated into South America either via Africa (through the Atlantic Ocean) or
Antarctica by the Maastrichtian, growing in eastern Patagonia up to the Early Miocene.
Arid conditions established in this region by the Middle-Late Miocene onwards would
have determined the restriction of forests to the western lands. Lactoridaceae may have
followed a similar migration pattern towards the Pacific coast of South America. The
shifting of Lactoridaceae towards the Masatierra Island would have occurred in the last
4 Myr, by long distance dispersal episodes (perhaps by birds).
Phil. than any other described morphotaxon. The family may have
migrated into South America either via Africa (through the Atlantic Ocean) or
Antarctica by the Maastrichtian, growing in eastern Patagonia up to the Early Miocene.
Arid conditions established in this region by the Middle-Late Miocene onwards would
have determined the restriction of forests to the western lands. Lactoridaceae may have
followed a similar migration pattern towards the Pacific coast of South America. The
shifting of Lactoridaceae towards the Masatierra Island would have occurred in the last
4 Myr, by long distance dispersal episodes (perhaps by birds).