The osmium isotope evidence found
in black shales correlates with higher continental weathering as a result of oxygen in the atmosphere.
Not exact matches
The Marcellus
Shale, also referred to as the Marcellus Formation, is a Middle Devonian - age
black, low density, carbonaceous (organic rich)
shale that occurs
in the subsurface beneath much of Ohio, West Virginia, Pennsylvania and New York.
Originally constructed
in the 1820's, the earliest settlers of Le Roy built the Creekside from
black Marcellus
shale dug from the Oatka Creek bed.
Permian - Triassic boundary
in shallow marine sediments, characterised by a significant sedimentation gap between the
black shales of Permian and dolomites of Triassic age.
In keeping with the naming of its living relative (after an Eastern Cape river), the species name of the new fossil form, kowiensis, is after the Kowie River which rises among the hills where it was found, and the genus name, Serenichthys, honours Serena Gess, who provided land for the storage of more than 70 tons of black shale rescued from roadworks for ongoing research — in which all the new material was foun
In keeping with the naming of its living relative (after an Eastern Cape river), the species name of the new fossil form, kowiensis, is after the Kowie River which rises among the hills where it was found, and the genus name, Serenichthys, honours Serena Gess, who provided land for the storage of more than 70 tons of
black shale rescued from roadworks for ongoing research —
in which all the new material was foun
in which all the new material was found.
Interspersed
in the red stone were narrow bands of
black shale containing petrified fish, from a time when a deep lake covered the area.
In the new paper, researchers analyzed the same
black shales for the relative abundance of an additional element: osmium.
To find out whether acid rain was indeed the problem, the team focused on one problematic sliding layer
in the Jiweishan avalanche: a thin bed of
black shale, which contains slippery clay minerals such as talc,
in addition to fine organic material and calcite, which helps cement the
shale together.
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The model also shows that the presence of seafloor anoxia, as suggested by
black -
shale deposition
in the proto - North Atlantic Ocean before the event, might be the result of the silled shape and lack of deep - water formation of this basin at the Late Cretaceous.
Lumpus must first reveal how Spookydontid albedo and
black carbon optical depth footprints have evolved since his debut alongside Hallucigenia sparsa
in the Burgess
shale
But, as would be expected from their origins
in the earth's orbital cycles, the Milankovitch rhythms were present long before that, and can be seen as cycles of deep - sea anoxia: T. D. Herbert and A. G. Fischer, «Milankovitch climatic origin of mid-Cretaceous
black shale rhythms
in central Italy.»
He was especially interested
in learning why
black shales, including the Marcellus, had a natural fracture pattern different from that of any other rock.
He said health hazard protocols can provide information on what the safe level of
black shale particles can be present
in well water.