title: The magnitude and duration of Late Ordovician-Early Silurian glaciation.
abstract: Understanding ancient climate changes is hampered by the inability to disentangle trends in ocean temperature from trends in continental ice volume. We used carbonate "clumped" isotope paleothermometry to constrain ocean temperatures, and thereby estimate ice volumes, through the Late Ordovician-Early Silurian glaciation. We find tropical ocean temperatures of 32° to 37°C except for short-lived cooling by ~5°C during the final Ordovician stage. Evidence for ice sheets spans much of the study interval, but the cooling pulse coincided with a glacial maximum during which ice volumes likely equaled or exceeded those of the last (Pleistocene) glacial maximum. This cooling also coincided with a large perturbation of the carbon cycle and the Late Ordovician mass extinction.
authors.affiliation: Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, USA. sethf@caltech.edu
authors.forename: Seth
authors.initials: S
authors.lastname: Finnegan
authors.forename: Kristin
authors.initials: K
authors.lastname: Bergmann
authors.forename: John M
authors.initials: JM
authors.lastname: Eiler
authors.forename: David S
authors.initials: DS
authors.lastname: Jones
authors.forename: David A
authors.initials: DA
authors.lastname: Fike
authors.forename: Ian
authors.initials: I
authors.lastname: Eisenman
authors.forename: Nigel C
authors.initials: NC
authors.lastname: Hughes
authors.forename: Aradhna K
authors.initials: AK
authors.lastname: Tripati
authors.forename: Woodward W
authors.initials: WW
authors.lastname: Fischer