An explanation for the 18O excess in Noelaerhabdaceae coccolith calcite
Coccoliths have dominated the sedimentary archive in the pelagic environment since the Jurassic. The biominerals produced by the coccolithophores are ideally placed to infer sea surface temperatures from their oxygen isotopic composition, as calcification in this photosynthetic algal group only occu...
Những tác giả chính: | Hermoso, M, Minoletti, F, Aloisi, G, Bonifacie, M, McClelland, H, Labourdette, N, Renforth, P, Chaduteau, C, Rickaby, R |
---|---|
Định dạng: | Journal article |
Được phát hành: |
Elsevier
2016
|
Những quyển sách tương tự
-
An explanation for the 18O excess in Noelaerhabdaceae coccolith calcite.
Bằng: Rickaby, R, et al.
Được phát hành: (2016) -
The origin of carbon isotope vital effects in coccolith calcite
Bằng: McClelland, H, et al.
Được phát hành: (2017) -
The origin of carbon isotope vital effects in coccolith calcite
Bằng: H. L. O. McClelland, et al.
Được phát hành: (2017-03-01) -
Towards the use of the coccolith vital effects in palaeoceanography: A field investigation during the middle Miocene in the SW Pacific Ocean
Bằng: Hermoso, M, et al.
Được phát hành: (2020) -
Environmental control of the isotopic composition of subfossil coccolith calcite: Are laboratory culture data transferable to the natural environment?
Bằng: Hermoso, M, et al.
Được phát hành: (2015)