Orbital-Scale Climate Changes Detected in Lower and Middle Ordovician Cyclic Limestones Using Oxygen Isotopes of Conodont Apatite

Author:

Elrick Maya

Publisher

Elsevier BV

Subject

General Earth and Planetary Sciences,General Environmental Science

Reference53 articles.

1. Comparative Lower-Middle Ordovician conodont oxygen isotope palaeothermometry of the Argentine Precordillera and Laurentian margins;Guillermo L Albanesi;Palaeogeography, Palaeoclimatology, Palaeoecology,2020

2. Oxygen isotopic composition of biogenic phosphate and the temperature of Early Ordovician seawater;D Bassett;Palaios,2007

3. Tectonic control on peritidal carbonate parasequence formation: An investigation using forward tectono-stratigraphic modelling;D D Benedictis;Sedimentology,2007

4. Cambro-Ordovician eustasy: Evidence from geophysical modelling of subsidence in Cordilleran and Appalachian passive margins;G C Bond;New perspectives in basin analysis,1988

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