Orbital-scale climate changes detected in Lower and Middle Ordovician cyclic limestones using oxygen isotopes of conodont apatite
Author:
Funder
National Science Foundation
Publisher
Elsevier BV
Subject
Paleontology,Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics,Oceanography
Reference68 articles.
1. Comparative Lower-Middle Ordovician conodont oxygen isotope palaeothermometry of the argentine Precordillera and Laurentian margins;Albanesi;Palaeogeogr. Palaeoclimatol. Palaeoecol.,2020
2. Role of seafloor production versus continental basalt weathering in Middle to Late Ordovician seawater 87Sr/86Sr and climate;Avila;Earth Planet. Sci. Lett.,2022
3. Oxygen isotopic composition of biogenic phosphate and the temperature of early Ordovician seawater;Bassett;Palaios,2007
4. Tectonic control on peritidal carbonate parasequence formation: an investigation using forward tectono-stratigraphic modelling;Benedictis;Sedimentology,2007
5. A paired apatite and calcite clumped isotope thermometry approach to estimating Cambro-Ordovician seawater temperatures and isotopic composition;Bergmann;Geochim. Cosmochim. Acta,2018
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1. Depositional and tectonic influences on preservation of Milankovitch record during long-term global cooling: Middle and Upper Ordovician convergent foreland, eastern USA;Palaeogeography, Palaeoclimatology, Palaeoecology;2023-10
2. Chitinozoan biostratigraphy of the regional Arenig Series in Wales and correlation with the global Lower–Middle Ordovician series and stages;Geological Magazine;2022-12-05
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