Results 11 to 20 of about 5,075 (214)
The use of soil palynomorphs in forensics [PDF]
Journal of Applied Sciences and Environmental Management, 2018 The aim was to establish the forensic value of using palynomorphs in soil samples to link people or objects to crime scenes in order to establish or strengthen an association.
A.A. Abdulrahaman +2 more
doaj +4 more sources
Why a new volume on non-pollen palynomorphs? [PDF]
Geological Society, London, Special Publications, 2021 Abstract Here we introduce the volume Applications of Non-Pollen Palynomorphs: from Palaeoenvironmental Reconstructions to Biostratigraphy . The study of non-pollen palynomorphs (NPPs) has a long and rich history that is interwoven with that of pollen-based studies.
Jennifer M. K. O'Keefe +4 more
openaire +4 more sources
Early Cretaceous (Neocomian-Cenomanian) Palynomorphs [PDF]
Journal of Micropalaeontology, 1985 Abstract. INTRODUCTIONThis study is primarily concerned with the Neocomian to Aptian palynomorphs recorded in selected exploration wells (See Fig. 9). In order to document a complete Early Cretaceous microfloral succession in the studied wells, a reconnaissance of Aptian to Early Cenomanian palynomorphs was also undertaken.
Thusu, B., Van Der Eem, J. G. L. A.
openaire +3 more sources
Identifying and naming non-pollen palynomorphs [PDF]
Review of Palaeobotany and PalynologyPalynological slides usually contain numerous remains of fungi, algae, plants, and animals, collectively referred to as non-pollen palynomorphs (NPPs). Even experienced palynologists often struggle to identify all of these palynomorphs or decide how they should be labelled in a way that ensures clarity and comparability across studies.
Shumilovskikh, Lyudmila +29 more
core +6 more sources
Geophysical Monograph Series, Page 263-304., 2021 Exploring the links between Large Igneous Provinces and dramatic environmental impact
An emerging consensus suggests that Large Igneous Provinces (LIPs) and Silicic LIPs (SLIPs) are a significant driver of dramatic global environmental and biological changes, including mass extinctions.
Jessica H. Whiteside +3 more
wiley +2 more sources
Journal of Micropalaeontology, 1985 Abstract. The data obtained from an independent study of acritarchs, chitinozoans and miospores enables the determination of maximum age ranges of samples taken from three wells. These are shown in Fig. 8.ACRITARCHSAt present, samples have been examined from six wells – A1-46, Core 2; E1-81, Cores 3, 4; F1-46, Core 3; D-31, Core 1; A1-81, Core 3 and C1-
Hill, P. J. +2 more
openaire +2 more sources
Devonian (Emsian-Famennian) Palynomorphs [PDF]
Journal of Micropalaeontology, 1985 Abstract. EMSIANMiospore assemblages which can be positively assigned to the Early Devonian have, to date, only been recorded from core material from Well A1-33. Assemblages of Emsian age were recorded from the interval 8079 to 8091 ft. whilst assemblages from 8055 to 8076 ft.
Paris, F. +4 more
openaire +3 more sources
High-resolution palynological analysis in Lake Sapanca as a tool to detect recent earthquakes on the North Anatolian Fault [PDF]
, 2009 High-resolution palynological analysis of a 38-cm-long core collected from Lake Sapanca, northwest Turkey, reveals large earthquakes that occurred during the second half of the 20th century along the North Anatolian Fault Zone. Four events have disturbed
Boyraz, S, Gürbüz, A, Leroy, SAG
core +3 more sources
Late Ordovician Palynomorphs [PDF]
Journal of Micropalaeontology, 1985 Abstract. ACRITARCHSOrdovician acritarchs have been recorded in five core samples collected between 2520 ft. and 3000 ft. in Well E1-81, and ten cutting samples taken between 12150 ft. and 13240 ft. in Well J1-81A. All the assemblages recovered are of Late Ordovician age; no Early Ordovician or Middle Ordovician assemblages have been identified ...
Molyneux, S. G., Paris, F.
openaire +2 more sources