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...
Hlavní autoři: | Wheeley, JR, Smith, M, Boomer, I |
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Médium: | Journal article |
Jazyk: | English |
Vydáno: |
2012
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