Oxygen isotope variability in conodonts: implications for reconstructing Palaeozoic palaeoclimates and palaeoceanography
Conodonts have the potential to elucidate the intricacies of Palaeozoic climates, especially if δ 18O values of single apatitic tooth-like 'elements' can be used to map evolving sea surface temperatures and differentiate oceanic water masses. Their ecological distribution as pelagic and ne...
Główni autorzy: | Wheeley, JR, Smith, M, Boomer, I |
---|---|
Format: | Journal article |
Język: | English |
Wydane: |
2012
|
Podobne zapisy
-
Paleoecologic and paleoceanographic interpretation of δ18O variability in Lower Ordovician conodont species
od: Wheeley, JR, i wsp.
Wydane: (2018) -
Paleoecologic and palaeoceanographic interpretation of δ18O variability in Lower Ordovician conodont species: REPLY
od: Wheeley, JR, i wsp.
Wydane: (2018) -
New group of the Early Palaeozoic conodont-like fossils
od: Hubert Szaniawski
Wydane: (2015-02-01) -
Coccolith-derived isotopic proxies in palaeoceanography: where geologists need biologists
od: Hermoso, M
Wydane: (2014) -
Chemostratigraphy of the Jurassic System: applications, limitations and implications for palaeoceanography
Wydane: (2002)