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[HTML][HTML] The enduring Ediacaran paleomagnetic enigma
M Domeier, B Robert, JG Meert, EV Kulakov… - Earth-Science …, 2023 - Elsevier
Abstract The Ediacaran Period was an interval of significant global transformation, marked
by major changes in the biosphere, cryosphere, hydrosphere and atmosphere, and possibly …
by major changes in the biosphere, cryosphere, hydrosphere and atmosphere, and possibly …
A Great late Ediacaran ice age
The emergence of the Ediacara biota soon after the Gaskiers glaciation ca. 580 million years
ago (Ma) implies a possible glacial fuse for the evolution of animals. However, the timing of …
ago (Ma) implies a possible glacial fuse for the evolution of animals. However, the timing of …
Pannotia: to be or not to be?
Following a decade during which its presence was widely accepted, the existence of the
putative Ediacaran supercontinent Pannotia has come into question since the turn of the …
putative Ediacaran supercontinent Pannotia has come into question since the turn of the …
Environmental drivers of the first major animal extinction across the Ediacaran White Sea-Nama transition
SD Evans, C Tu, A Rizzo, RL Surprenant… - Proceedings of the …, 2022 - pnas.org
The Ediacara Biota—the oldest communities of complex, macroscopic fossils—consists of
three temporally distinct assemblages: the Avalon (ca. 575–560 Ma), White Sea (ca. 560 …
three temporally distinct assemblages: the Avalon (ca. 575–560 Ma), White Sea (ca. 560 …
The origin of cap carbonate after the Ediacaran glaciations
R Wang, C **ng, B Wen, X Wang, K Liu… - Global and Planetary …, 2023 - Elsevier
Abstracts Cap carbonate is the most unique component of a Snowball Earth glaciation, ie,
two Cryogenian global glaciations. In the canonical model, cap carbonate precipitation …
two Cryogenian global glaciations. In the canonical model, cap carbonate precipitation …
Pannotia: in defence of its existence and geodynamic significance
JB Murphy, RD Nance, PA Cawood, WJ Collins, W Dan… - 2021 - pubs.geoscienceworld.org
The status of Pannotia as an Ediacaran supercontinent, or even its mere existence as a
coherent large landmass, is controversial. The effect of its hypothesized amalgamation is …
coherent large landmass, is controversial. The effect of its hypothesized amalgamation is …
The provenance of Avalonia and its tectonic implications: a critical reappraisal
Abstract The late Neoproterozoic–Cambrian interval is characterized by global-scale
orogenesis, rapid continental growth and profound changes in Earth systems. Orogenic …
orogenesis, rapid continental growth and profound changes in Earth systems. Orogenic …
Inverted South China: A novel configuration for Rodinia and its breakup
Disentangling records of Rodinia fragmentation and true polar wander remains a challenge
for understanding late Tonian plate tectonics. The ca. 760 Ma lower member of the Liántuó …
for understanding late Tonian plate tectonics. The ca. 760 Ma lower member of the Liántuó …
Iapetan Oceans: an analog of Tethys?
Abstract The Iapetus Ocean opened during the breakup of Rodinia by the separation of the
major continental blocks of Laurentia (LA), Baltica, and Amazonia (AM). Relics of protracted …
major continental blocks of Laurentia (LA), Baltica, and Amazonia (AM). Relics of protracted …
Late Cambrian geomagnetic instability after the onset of inner core nucleation
Abstract The Ediacaran Period marks a pivotal time in geodynamo evolution when the
geomagnetic field is thought to approach the weak state where kinetic energy exceeds …
geomagnetic field is thought to approach the weak state where kinetic energy exceeds …