WebFeb 4, 2024 · On average Nothofagidites pollen accounts for 79.0 % of all non-reworked taxa and 95.0 % of all angiosperm taxa. Taxa belonging to the Nothofagidites lachlaniae complex (subgenus: Fuscospora) are the most abundant followed by undifferentiated Nothofagus spp. sporomorphs and N. rocanensis (subgenus: Nothofagus ). WebAug 15, 2014 · Nothofagidites senectus Dettmann and Playford 1968 [Fig. 3-33] Nothofagidites Erdtman 1947 ex Potonié 1960 spp. [Cluster of adherent grains, Fig. 3-41] Taxonomic note — The morphological variety and commonly folded nature of Nothofagidites spp. grains restricted identification of most specimens to generic level …
CiteSeerX — Revista Brasileira de Paleontologia 9(1):101-108, …
WebMar 23, 2010 · Nothofagidites matawaensis is the most abundant palynomorph throughout, first appearing in the lower Waikato Coal Measures. Several palynomorphs become extinct near the Eocene/Oligocene boundary, where there appears to be a significant turnover in species, similar to that documented for the marine realm. WebIt was associated with one of the most catastrophic events in the history of life, involving mass mortality in both terrestrial and marine ecosystems globally; vast amounts of dead biomass covered the Earth’s surface. Of prime importance are … sign in dexcom clarity
Paleogeography of Late Eocene to earliest Miocene Te Kuiti …
WebMar 22, 2024 · In the angiosperm group, Nothofagidites is further divided into subgenera. These are Brassospora (B), Fuscospora (F), and Lophozonia (L) types. CONISS ordination constrains our late Eocene–early Oligocene sporomorph assemblages into four distinct pollen zones (PZ 1–PZ 4) or vegetation and climate phases. WebDownload Table Species of Nothofagidites recovered from Site 274 from publication: Evidence of Pliocene Nothofagus in Antarctica from Pliocene marine sedimentary … WebA detailed examination of the brown coal facies preserved in the Latrobe Valley Morwell 1B seam indicates that the type of peat-forming environment and the associated hydrological regime are the main factors influencing the development of lithotypes sign in department of education one school