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60  Articles
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New Anisian to Ladinian palynology, palynofacies and stable carbon isotope records are reported for the Middle Triassic from deep Swiss wells (Weiach, Benken, Leuggern), well B3/13 (Weizen, S-Germany) and the type area of the Freudenstadt Formation in sou... see more

The vegetation of the Po Plain has long been modified by natural and human factors. The present plant landscape is almost entirely anthropogenic. Many hydro-hygrophilous species, quite common until a few decades ago, are now very rare and in danger of ext... see more

Givetian sediments are widely distributed within the Volyn-Podillia margin of the East-European platform (VPO EEP). These are terrigenous-carbonate cyclically constructed formations with a thickness of 102 to 165 m, the stratification of which is complica... see more

Pollen is the reproductive agent of flowering plants; palynology is utilized by archaeologists because sporopollenin, a major component in the exine of pollen grains, is resistant to decay and morphologically distinctive. Wine, beer, and mead have been id... see more

Local source rock potential of ANL-1 and E-12 well sediments in offshore, NigerDelta have been evaluated based on organic matter maturation studies to provideleads for hydrocarbon exploration. The studied wells display diverse palynoflora atdifferent stra... see more

The Garigliano Plain (between Latium and Campania) is characterized by the presence of wetlands behind the most recent beach ridge. Although modern cartography displays small lakes and the Greek and Latin authors describe a marshy environment close to the... see more

Pollen is the reproductive agent of flowering plants; palynology is utilized by archaeologists because sporopollenin, a major component in the exine of pollen grains, is resistant to decay and morphologically distinctive. Wine, beer, and mead have been id... see more

Well 11 is located near the village of Velika Lanna, Krasnograd District, Kharkiv Region, and at the current stage of research is the most representative section of the continental Upper Cenozoic deposits of the Dnieper-Donets depression. For the first ti... see more

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