-
Event II were
dysoxic (2.0 - 0.2 mL of O2/L of H2O[with oxic
being > 2.0 mL of O2/L])
rather than
anoxic (< 0.2 mL of O2/L of H2O).
Dysoxic water can be...
- concentration—in the
range between 1 and 30% saturation—is
called hypoxic or
dysoxic. Most fish
cannot live
below 30%
saturation since they rely on
oxygen to...
- Formation),
which are
interpreted as the
products of an oxygen-depleted ("
dysoxic")
marine bottom water habitat of a
possibly offs****
seashelf at depths...
- the
Tethys Ocean jumped to 32–36 °C, and
Tethyan seawater became more
dysoxic. A
decline in
carbonate ac****ulation at
ocean depths of
greater than three...
- Bernhard, Joan M.; Bowser,
Samuel S. (1999). "Benthic
foraminifera of
dysoxic sediments:
chloroplast sequestration and
functional morphology". Earth-Science...
- .trilobite
occupied the
exaerobic zone, at the
boundary of
anoxic and
dysoxic bottom waters. E.
kingii consistently occur in
settings below the oxygen...
- ISBN 978-1-4684-7612-5. Bernhard, J. M.; Bowser, S.M. (1999). "Benthic
Foraminifera of
dysoxic sediments:
chloroplast sequestration and
functional morphology". Earth-Science...
-
marine konzentrat-lagerstätte
deposited in a
hemipelagic mud
bottom during dysoxic conditions.
Talbragar fossil site 151 Ma New
South Wales,
Australia This...
-
Sally E. (2016-01-01). "Testing
symbiotic morphology in
trilobites under dysoxic and oxic
conditions from
Cambrian to
Early Ordovician Lagerstätten". Palaeogeography...
-
Coastal Plain, well
oxygenated during the Late Palaeocene,
became highly dysoxic during the PETM. The
tropical surface oceans, in contrast,
remained oxygenated...
