Results 81 to 90 of about 8,694 (221)

A new psammosteid (Agnatha, Heterostraci) from the Amata Regional Stage of the Main Devonian Field and morpho-histological types of discrete micromeric elements in the family Psammosteidae [PDF]

open access: yesEstonian Journal of Earth Sciences, 2017
In memory of an outstanding palaeoichthyologist Elga Mark-Kurik The range of diversity of psammosteids from the family Psammosteidae is still poorly known. Here a new species, Psammosteus ramosus sp. nov.
Vadim N. Glinskiy, Sergey P. Nilov
doaj   +1 more source

Araguainha Dome, Brazil: A polygonal impact structure due to a complex pre‐impact regional structural framework

open access: yesMeteoritics &Planetary Science, EarlyView.
Abstract We investigated the structural framework of the north–northwestern Paraná Basin in Brazil to test whether the pre‐impact structures in this region may have had any influence on the first‐order formation and morphostructure of the Araguainha impact structure (AIS).
Renato B. Bernardes   +5 more
wiley   +1 more source

Late Devonian shear zone reactivation in the Canadian Appalachian orogen: Supplementary material

open access: yes, 2023
Supplementary material for the manuscript named Late Devonian shear zone reactivation in the Canadian Appalachian ...
Nicolas Piette-Lauziere
core   +1 more source

Revisiting the Hummeln structure, Sweden—A shallow marine Cambrian impact structure

open access: yesMeteoritics &Planetary Science, EarlyView.
Abstract Hummeln is a simple impact structure located in south‐eastern Sweden. It is approximately 1.2 km in diameter and almost completely covered by a lake. Here, we present the first detailed investigation of impactites and mapping of the 164.25 m deep drill core Hummeln‐1 with a focus on impact metamorphism and the impact process.
S. Alwmark   +8 more
wiley   +1 more source

Eifelian (Middle Devonian) to Early Frasnian (Late Devonian) conodonts and strata in the Spanish Central Pyrenees: Global correlations and effects of climatic fluctuations in the biota

open access: yes
The interval between the late Eifelian and early Frasnian was marked by significant paleoenvironmental instability, including major evolutionary, eustatic, and biotic events.
Valenzuela Ríos, José Ignacio   +1 more
core   +1 more source

Late Mid Devonian Sawdonia (Zosterophyllopsida) from Venezuela [PDF]

open access: yes, 2019
Premise of research. Fossil plants from the Late Middle to early Late Devonian age Campo Chico Formation, Sierra de Perijá, western Venezuela, are determined to represent a new species of the zosterophyll genus Sawdonia.
Berry, Christopher M.   +1 more
core   +1 more source

Palaeoecological reconstruction of the Late Devonian Lebedjan biota

open access: yes, 2022
Palaeozoic fossil-bearing deposits in Russia record important and rare insights into pre-Mesozoic palaeoecological systems. Among the known formations, the Late Devonian (Famennian) deposits exposed in the central part of Russian platform have been under-
D C Bicknell, Russell   +1 more
core   +1 more source

Evidence for regulation of transpiration in nonstomatal plants: insights from bryophyte gametophytes

open access: yesNew Phytologist, EarlyView.
Kinetics of cell wall water vapor potential (Ψcw) and resistance of cell wall and plasmatic membrane to water flux in response to cytoplasmic water potential (Ψcyt) during dehydration. Ψcyt was calculated from the WC at any moment of the dehydration curve by using the relationship between −1/Ψw and WC of pressure volume curves and assuming Ψw = Ψcyt ...
Alicia V. Perera‐Castro   +3 more
wiley   +1 more source

Simple mass balance model for the Mo inventory of Late Devonian seawater

open access: yes, 2022
Simple mass balance model for the Mo inventory of Late Devonian ...
Swapan Sahoo
core   +1 more source

Recognition of fossil keratose sponges in carbonates using petrographic and machine‐learning classification

open access: yesSedimentology, EarlyView.
ABSTRACT Filamentous, anastomosing spar‐filled networks in Phanerozoic carbonates have been interpreted as the mineralised remains of keratose (non‐spiculate) sponges, yet their recognition remains contested because fabrics of broadly similar appearance may arise from microbial, diagenetic or physical processes. This study combines direct fossil–modern
Jeong‐Hyun Lee   +2 more
wiley   +1 more source

Home - About - Disclaimer - Privacy