Results 31 to 40 of about 2,147 (148)

Transient marine euxinia at the end of the terminal Cryogenian glaciation

open access: yesNature Communications, 2018
The termination of the Marinoan snowball Earth event marks one of the most drastic transitions in Earth history, but the oceanic response remains unclear.
Xianguo Lang   +11 more
doaj   +1 more source

Snowball Earth Under the Microscope [PDF]

open access: yesJournal of Sedimentary Research, 2018
Abstract Micromorphology is a well-established technique adopted by Quaternary scientists which has received wide application in the study of glacial sediments and in soil science. One area where the approach is far less developed is in the analysis of ancient successions and, in particular, rocks of Cryogenian age that are purported ...
Busfield, Marie Elen   +1 more
openaire   +2 more sources

Climate and ocean circulation changes toward a modern snowball Earth [PDF]

open access: yesClimate of the Past
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

Tonian Low‐Latitude Marine Ecosystems Were Cold Before Snowball Earth

open access: yesGeophysical Research Letters, 2023
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

Life, geology and snowball Earth [PDF]

open access: yesNature, 2001
According to the 'snowball Earth' hypothesis, a series of global glaciations occurred 750–580 million years ago, each lasting for millions of years and ending in a scorching heat caused by an extreme enrichment of atmospheric greenhouse gases. Hyde et al.1 have used climate models to simulate this global glaciation, finding in one case an alternative ...
D P, Schrag, P F, Hoffman
openaire   +2 more sources

The dynamics of the Snowball Earth Hadley circulation for off-equatorial and seasonally varying insolation [PDF]

open access: yesEarth System Dynamics, 2013
I study the Hadley circulation of a completely ice-covered Snowball Earth through simulations with a comprehensive atmosphere general circulation model.
A. Voigt
doaj   +1 more source

Eurypsychrophilic acidophiles: From (meta)genomes to low-temperature biotechnologies

open access: yesFrontiers in Microbiology, 2023
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

Radiative effects of ozone on the climate of a Snowball Earth [PDF]

open access: yesClimate of the Past, 2012
Some geochemical and geological evidence has been interpreted to suggest that the concentration of atmospheric oxygen was only 1–10 % of the present level in the time interval from 750 to 580 million years ago when several nearly global glaciations or
J. Yang, Y. Hu, W. R. Peltier
doaj   +1 more source

Tracing the Snowball bifurcation of aquaplanets through time reveals a fundamental shift in critical-state dynamics [PDF]

open access: yesEarth System Dynamics, 2023
The instability with respect to global glaciation is a fundamental property of the climate system caused by the positive ice-albedo feedback. The atmospheric concentration of carbon dioxide (CO2) at which this Snowball bifurcation occurs changes through ...
G. Feulner   +3 more
doaj   +1 more source

Snowball Earth transitions from Last Glacial Maximum conditions provide an independent upper limit on Earth's climate sensitivity [PDF]

open access: yesEarth System Dynamics
Geological evidence of a snowball Earth state indicate persistent tropical sea ice cover during the Neoproterozoic (>635 million years ago). Current theory is that a strengthening of the positive surface albedo feedback with cooling temperatures ...
M. Renoult   +6 more
doaj   +1 more source

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