Extremely high temperatures and paleoclimate trends recorded in Permian ephemeral lake halite

@article{Zambito2013ExtremelyHT,
  title={Extremely high temperatures and paleoclimate trends recorded in Permian ephemeral lake halite},
  author={James J. Zambito and Kathleen Counter Benison},
  journal={Geology},
  year={2013},
  volume={41},
  pages={587-590}
}
Although the late Paleozoic deglaciation is arguably one of the best deep-time analogs for current and predicted climate change, quantitative paleotemperature data from this interval are generally lacking. We reconstruct extreme paleoweather conditions and paleoclimate changes from Permian Nippewalla Group (probably uppermost Leonardian/Kungurian; North America) ephemeral lake halite by using fluid inclusion homogenization temperatures to directly measure the water temperature when the halite… 

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References

SHOWING 1-10 OF 29 REFERENCES
Paleobrine Temperatures, Chemistries, and Paleoenvironments of Silurian Salina Formation F-1 Salt, Michigan Basin, U.S.A., from Petrography and Fluid Inclusions in Halite
Abstract A 3.7 m stratigraphic section of the Silurian Salina Group F-1 Salt, Detroit Salt Company mine, Michigan Basin, was studied to document the paleodepositional conditions, including brine
Silurian paleoclimate data from fluid inclusions in the Salina Group halite Michigan Basin
The Silurian Salina Group of the Michigan Basin consists of halite, carbonates, and shales. The halite was probably deposited when seawater became restricted over what is now southern Michigan. The
From Wetlands to Wet Spots: Environmental Tracking and the Fate of Carboniferous Elements in Early Permian Tropical Floras
Diverse wetland vegetation flourished at the margins of the Midland Basin in north-central Texas during the Pennsylvanian Period. Extensive coastal swamps and an ever-wet, tropical climate supported
...
...