Results 31 to 40 of about 3,280 (273)
Maintenance of the great late Ediacaran ice age [PDF]
Geological records witness extensive glaciations in the late Ediacaran, ranging from ~580 to 560 Ma or younger. However, the explanation of maintenance for this regionally diachronous and globally continuous glacial epoch is still unclear.
Peng Liu +6 more
doaj +2 more sources
Large equatorial seasonal cycle during Marinoan snowball Earth. [PDF]
© 2020 The Authors. In the equatorial regions on Earth today, the seasonal cycle of the monthly mean surface air temperature is 1 m) sand wedges were found near the paleoequator in the Marinoan glaciogenic deposits at ∼635 million years ago, indicating a
Liu Y, Yang J, Bao H, Shen B, Hu Y.
europepmc +2 more sources
Initiation of a Marinoan Snowball Earth in a state-of-the-art atmosphere-ocean general circulation model [PDF]
We study the initiation of a Marinoan Snowball Earth (~635 million years before present) with the state-of-the-art atmosphere-ocean general circulation model ECHAM5/MPI-OM. This is the most sophisticated model ever applied to Snowball initiation.
A. Voigt +3 more
doaj +1 more source
When the Earth goes white: the Snowball Earth attractor [PDF]
Using an intermediate complexity climate model we investigate the so-called snowball Earth transition. For certain values (including its current value) of the solar constant, the climate system allows two different stable states: one of them is the ...
Kaszás, Bálint +2 more
core +1 more source
A conceptual model of oceanic heat transport in the Snowball Earth scenario [PDF]
Geologic evidence suggests that the Earth may have been completely covered in ice in the distant past, a state known as Snowball Earth. This is still the subject of controversy, and has been the focus of modeling work from low-dimensional models up to ...
D. Comeau, D. A. Kurtze, J. M. Restrepo
doaj +1 more source
Climate and ocean circulation in the aftermath of a Marinoan snowball Earth [PDF]
When a snowball Earth deglaciates through a very high atmospheric CO2 concentration, the resulting inflow of freshwater leads to a stably stratified ocean, and the strong greenhouse conditions drive the climate into a very warm state.
L. Ramme +3 more
doaj +1 more source
Climate and ocean circulation changes toward a modern snowball Earth [PDF]
It has been hypothesized that the Earth may have experienced snowball events in the past, during which its surface became completely covered with ice. Previous studies used general circulation models to investigate the onset and climate of such snowball ...
T. Obase +8 more
doaj +1 more source
Evidence based on molecular clocks, together with molecular evidence/biomarkers and putative body fossils, points to major evolutionary events prior to and during the intense Cryogenian and Ediacaran glaciations. The glaciations themselves were of global
Daniel Paul Le Heron
doaj +1 more source
Tonian Low‐Latitude Marine Ecosystems Were Cold Before Snowball Earth
Precambrian marine carbonate strata are commonly assumed to have formed in warm‐water carbonate factories due to the temperature dependence of non‐skeletal carbonate precipitation rates.
Elizabeth J. Trower +4 more
doaj +1 more source
Eurypsychrophilic acidophiles: From (meta)genomes to low-temperature biotechnologies
Low temperature and acidic environments encompass natural milieus such as acid rock drainage in Antarctica and anthropogenic sites including drained sulfidic sediments in Scandinavia.
Mark Dopson +5 more
doaj +1 more source

