INVESTIGADORES
IGLESIAS Ari
congresos y reuniones científicas
Título:
Cretaceous seeds from the Austral Basin, Argentina, their context in the angiosperm dispersal and evolution.
Autor/es:
ARI IGLESIAS; ZAMUNER ALBA B.; POIRE DANIEL
Lugar:
La Plata
Reunión:
Congreso; X Congreso Argentino de Paleontología y Bioestratigrafía y VII Congreso Latinoamericano de Paleontología; 2010
Institución organizadora:
Universidad Nacional de La Plata
Resumen:
With angiosperm radiation and diversification during the Upper Cretaceous, deep floristic changes occurred thatdrove into modern ecosystems. Little is known about plant ecology and seed dispersal during the Cretaceous. Richcompression floras found in Piedra Clavada (Albian), Mata Amarilla (Cenomanian), and La Anita (Campanian?)formations in the northern Austral Basin, Santa Cruz province, allow the recognition of diverse angiosperm florasof leaves, flowers, fruits, and seeds. Up to now there were identified seven new seed types, all of them very small insize (0.4-5mm maximum length), coinciding with global Cretaceous records. Some seeds preserve woody envelopewith rugulate ornamentation and two lateral wings, similar to Albian records from North America. Spherical seedswith pedunculate hilum show in some cases a pair of wings meanwhile in others three longitudinal keels. Someof them, exceptionally preserved, have endosperm cells. The biggest seeds were found inside small dry fruits.Presence of winged seeds and general small seed size in these floras seem to indicate both fast growing seedlingand anemochory as the most common seed dispersal mechanism. The Cretaceous is critical in the evolution of seeddisperser as mammals and birds; several dispersal theories have been proposed based on Cretaceous seeds shapeand size for the North Hemisphere. The Austral Basin fossil records plus several other Patagonian macrofloras understudy could give light in the understanding of the plant-disperser evolution in southern South America based on afairly continuous fossil record from middle Cretaceous to Paleogene.