THE ULTRASTRUCTURE OF IN-SITU CLAVATIPOLLENITES POLLEN FROM THE EARLY CRETACEOUS OF PATAGONIA

Small dispersed anther contents of Clavatipollenites grains are reported from the Early Cretaceous (early Aptian) of Patagonia. This report represents the first documentation of in situ grains of this type from the Southern Hemisphere. The anthers are small (0.6 mm long x 0.25 mm wide); no tissues of the androecium are preserved nor is there any indication of how the sacs were attached. Some grains are still in tetrads and closely associated with numerous orbicules and tapetal membranes. Grains are 18-22 mum long and up to 15 mum wide. The exine consists of an inner homogeneous nexine that supports narrow columellae below a perforate tectum. The mature pollen wall includes uniform microgranules that ornament the muri. The chloranthaceous affinities of these Gondwana pollen sacs are established and the grains are compared with specimens recovered from slightly older or coeval sediments from the Northern Hemisphere. The discovery of these pollen sacs from Patagonia expands our understanding of early angiosperm biogeography.