Stratigraphic first occurrence of Emiliania huxleyi in sediments of the Chatham Rise (Table 2), supplement to: Fenner, Juliane M; Di Stefano, Agata (2004): Late Quaternary oceanic fronts along Chatham Rise indicated by phytoplankton assemblages, and refined calcareous nannofossil stratigraphy for the mid-latitude SW Pacific. Marine Geology, 205(1-4), 59-86

Juliane M Fenner & Agata Di Stefano
A quantitative analysis was carried out of planktonic diatoms (biogenic opal) and calcareous nannofossils (biogenic calcite) in late Quaternary sediments (MIS 1–6) from four cores along a N–S transect east of New Zealand from 39°50'S to 50°04'S across the E–W-trending submarine ridge, the Chatham Rise. This was done to trace movements of oceanic fronts and to improve calcareous nannofossil stratigraphy for the last 130 000 yr in the SW Pacific. Sites ODP 1123 and Q...
This data repository is not currently reporting usage information. For information on how your repository can submit usage information, please see our documentation.