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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
seeds
Pollen morphology and reproductive biology of Calophyllum brasiliense Cambess. (Calophyllaceae) Available to Purchase
THE SOUTH DOES ALSO EXIST: THE CONTINENTAL DRIFT DEBATE IN THE ACCOUNT OF THE SOUTH-AFRICAN PALEOBOTANIST EDNA PLUMSTEAD Available to Purchase
EARLY DIAGENESIS OF SEEDS ASSOCIATED WITH LIMESTONES SOILS Available to Purchase
Inconsistent Hydroclimate Responses in Different Parts of the Asian Monsoon Region during Heinrich Stadials Open Access
Contribution of archaeobotany to understand taphonomic phenomena. The case of a Preboreal palaeochannel of Autrecourt-et-Pourron (Ardennes, France) Open Access
FIRST EVIDENCE OF SEED PREDATION BY ARTHROPODS FROM GONDWANA AND ITS EARLY PALEOZOIC HISTORY (RIO BONITO FORMATION, PARANÁ BASIN, BRAZIL) Available to Purchase
Position of the base of the Quaternary in West Siberia (based on paleobotanical and paleomagnetic evidence) Available to Purchase
Biota and palaeoenvironment of a high middle-latitude Late Triassic peat-forming ecosystem from Hopen, Svalbard archipelago Available to Purchase
Abstract A siliceous permineralized peat block recovered from Hopen in the Svalbard archipelago hosts a low-diversity Late Triassic flora dominated by autochthonous roots and stems of bennettitaleans and lycophytes, and parautochthonous leaves, sporangia, spores and pollen from a small range of pteridophytes and gymnosperms. Some parenchymatous bennettitalean root cells show interactions with chytrid fungi and bacteria; the remains of other fungi and fungi-like organisms are dispersed within the peat’s detrital matrix. Cavities excavated through some roots and compacted detritus contain abundant coprolites probably derived from sapro-xylophagous oribatid mites, although no body fossils have yet been identified. Sparse larger coprolites containing leaf fragments attest to the presence of invertebrate folivores in the ancient ecosystem. The low-diversity flora, relatively few trophic levels and simple nutritional web, together with sedimentological aspects of the host formation and the peat structure, collectively favour accumulation of the organic mass as a fibric (root-dominated) peat within a temperate (high middle-latitude), well-aerated mire.