Siluro-Devonian miospore biostratigraphy of the Urubu River area, western Amazon Basin, northern Brazil.

STEEMANS, P.; RUBINSTEIN, CLAUDIA V.; MELO, J. H. G.

GEOBIOS

Elsevier

Lugar: Amsterdam; Año: 2008 vol. 41 p. 263 - 282

0016-6995

Well preserved miospores have been observed in the Urubu River area from the western part of the Amazon Basin, northern Brazil, in rocks belonging to the uppermost Pitinga and Manacapuru Formations. A previous palynological work based on chitinozoans has dated these strata as late Ludlow, early Pridoli and early Lochkovian. Although samples are relatively poor in miospores, the present study reveals the most diversified Silurian-earliest Lochkovian palynoflora ever reported from South America, an interval where miospore information is still very rare. Sixty four species have been identified, of which two are new (Artemopyra urubuense and Retusotriletesamazonensis). One single specimen attributed to the genus Grandispora, identical to unpublished forms identified by one of us (P.S.) in Lochkovian sections of Saudi Arabia, has been found in a Lochkovian sample from the Urubu River. These constitute the oldest geological record of Grandispora. Among the abundant acritarchs, specimens of the genus Schizocystia have been observed for the first time in pre-Devonian rocks.Although the late Silurian ? early Lochkovian miospore biostratigraphy is still in its infancy in South America, it seems that Amazon Basin assemblages do not show significant differences in composition in comparison to coeval palynofloras from other areas of northwestern Gondwana. This is surprising since the miospore localities under consideration are widely distributed over high to low paleolatitudes, i.e. from cool temperate to dry subtropical belts. Conversely, Siluro-Devonian Gondwanan assemblages differ considerably from the contemporary palynofloras of the Old Red Sandstone Continent and adjacent areas, thus contradicting recent phytogeographic interpretations based on megafloras.