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radiolaria - Marum

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Radiolaria 14 News<br />

we have our pets that we know well and determine easily,<br />

whereas we tend to doubt about other species which we do<br />

not know so well. A logical consequence of this human<br />

preference is the incoherence of our datasets. Correlation<br />

by BIOGRAPH is entirely based on species association or<br />

exclusion and on superpositional relationships between<br />

species and species associations. Incomplete data, in our<br />

case simply caused by the specialization of each worker,<br />

result in huge numbers of undetermined relationships, and<br />

hence poor superpositional control and poor lateral<br />

reproducibility of Unitary Associations.<br />

The new biozonation presented in our Atlas represents<br />

a synthesis of a number of local biozonations based on<br />

What is going on in the Cenozoic?<br />

Material from recent ODP legs in the Antarctic has<br />

resulted in a number of biostratigraphic and taxonomic<br />

studies in the high Southern latitudes. Other studies of<br />

importance are: description of Paleocene faunas from the<br />

Indian Ocean and New Zealand, biogeographical and<br />

paleoecological studies in the equatorial Pacific, flux<br />

pattern studies in the Southern Ocean, a detailed<br />

morphological study of the Pyloniacea and a report on the<br />

Tripyleans in the Subantarctic. Marine pollen and<br />

siliceous microfauna have been reported to record<br />

concurrent late glacial variations in the regional terrestrial<br />

and marine environments around the Okhotsk basin.<br />

Comparisons of Late Miocene to Recent <strong>radiolaria</strong>ns from<br />

the Oman margin with the fauna recovered from the Peru<br />

margin upwelling area suggests that the assemblage may<br />

be globally diagnostic of upwelling conditions;<br />

strengthening and weakening of upwelling pulses is<br />

indicated by marked faunal changes. A study of the origin<br />

and the evolution of the Pterocorythidae through the<br />

Cenozoic reveals that there are only two persistent stocks<br />

from which developed fourteen branches treated as genera<br />

and subgenera; interesting trends in abundance and<br />

geographic distribution have been documented in this<br />

family. Comparison of assemblages from plankton and<br />

sediments in the Norwegian fjords and from stations in<br />

the Norwegian Sea, using multivariate analysis, shows<br />

that the largest source of variability is between sediment<br />

and plankton, differences due to season, region and depth<br />

are secondary.<br />

The Cenozoic working group has not had a joint<br />

project, but several of its members have had close<br />

working relationships resulting in valuable scientific<br />

publications which can be seen in the above list of<br />

publications and from the following summary:<br />

News items:<br />

1) Simon K. Haslett (University OF East Anglia) visited<br />

Annika Sanfilippo at Scripps Institution of Oceanography<br />

on a Fulbright Scholarship (October 19, 1992 - Jan 4,<br />

1993). Mr Haslett works on modern distributional<br />

Cenozoic Working Group News<br />

Catherine Nigrini and Annika Sanfilippo<br />

- 9 -<br />

BIOGRAPH calculations. We realized, that sacrifices of<br />

local stratigraphic resolution are unavoidable to achieve a<br />

worldwide correlation. However, the large number of<br />

included taxa results in a good temporal resolution (about<br />

80 U.A. for the Middle to Upper Jurassic and 35 U.A. for<br />

the Lower Cretaceous). We create about 20 zones for the<br />

Aalenian - Barremian interval. Chronostratigraphic<br />

calibration was obtained by correlation to ammonites,<br />

calpionellids, nannofossils etc., and magnetic polarity<br />

zones.<br />

Peter O. Baumgartner<br />

patterns of <strong>radiolaria</strong>ns in the East tropical Pacific. During<br />

his visit Mr. Haslett sampled a number of coretops from<br />

the Scripps core collection to compliment his own<br />

samples from ODP Site 677A and 846 in the<br />

Olduvai/Gauss time interval.<br />

2) Donna Hull and Annika Sanfilippo participated in<br />

fieldwork conducted in Cuba from January 11-16, 1993 in<br />

conjunction with the International Geological<br />

Correlations Project #308 (Paleocene-Eocene boundary).<br />

The purpose was to review stratigraphic work in Cuba on<br />

three potential boundary stratotypes and to resample the<br />

sections in detail. Five geologists from the U.S<br />

participated and were hosted by nine Cuban colleagues<br />

from the IGCP committee. The Cuban sections are of<br />

special interest as they contain both siliceous and<br />

calcareous microfossils. Biostratigraphic work on the<br />

sections by Gena Fernandez (planktonic foraminifera) and<br />

Emilio Florez (Radiolaria) has provided the basic<br />

stratigraphic framework. Joint efforts are now underway<br />

between the US and the Cuban team to produce results by<br />

the fall of 1994.<br />

3) During the months of May, 1993 and February, 1994<br />

Dr. Jean-Pierre Caulet (Laboratoire de Geologie, Museum<br />

National d'Histoire Naturelle, Paris, France) visited<br />

Annika Sanfilippo at Scripps Institution of Oceanography<br />

to work on <strong>radiolaria</strong>n evolution in the Antarctic.<br />

4) Annika Sanfilippo and Amy Weinheimer finished the<br />

preparation of the <strong>radiolaria</strong>n samples from DSDP Legs 1-<br />

96 (3000 samples) for the eight DSDP/ODP<br />

Micropaleontological Reference Centers (MRC) around<br />

the world. The material is available at a MRC near you to<br />

compare prepared material with the reports and<br />

illustrations published in the DSDP Initial Reports. This<br />

will help stabilize taxonomy, enable researchers to view<br />

material for biostratigraphic and paleoenvironmental<br />

purposes and prior to a cruise, to better plan subsequent<br />

sample requests from the DSDP/ODP repository.<br />

5) During the months of October and November, 1993<br />

Catherine Nigrini (510 Papyrus Drive, La Habra Heights,<br />

CA 90631) held the position of professor at the Museum<br />

National d'Histoire Naturelle in Paris where she worked

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