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Radiolaria 14 Symposia<br />

TX, 77845. You will receive an application form to fill<br />

out and return to ODP.<br />

ODP Sets 1995 Drilling<br />

ODP is currently staffing Legs 159 onwards.<br />

Shipboard participation is by invitation from ODP's<br />

science operator at Texas A&M University. Information<br />

and applications can be obtained by contacting the Ocean<br />

Drilling Program. Texas A&M Univesity, 1000<br />

Discovery Drive, College Station, TX 77845-9547 or<br />

phone 409-845-2673, fax 409- 8454857, Internet:<br />

baldauf@nelson.tamu.edu.<br />

Leg 159 Return to Site 735<br />

The purpose of this leg is to return to ODP site 735<br />

on the southwest Indian Ridge, and deepen hole 735B to a<br />

nominal depth of 2 ~m mbsf. The principle objective of<br />

this proposed leg is to understand the nature of the<br />

processes involved in the generation of the lower crust,<br />

and the put some constraints on the lower crustal<br />

stratigraphy at the slowest end of the spreading spectrum.<br />

Leg 160 Eastern Eq. Atlantic Transform<br />

The key issues to be addressed by drilling include an<br />

evaluation of the tectonic and sedimentary processes<br />

involved in the creation of the main morpho-structural<br />

features ~enerated at the Cate d'Ivoire-Ghana Transform<br />

Margin. Results should provide data on the timing, rate<br />

and de~ree of vertical motion (subsidence and uplift) of the<br />

Cote d"Ivoire-Ghana Transform Margin.<br />

Leg 161/162 Mediterranean I & II<br />

The proposed two lef!s of drilling in the<br />

Mediterranean will address three main objectives: the<br />

- 13 -<br />

Alboran Basin (Western Mediterranean), drilling on the<br />

Mediterranean Accretionary Complex (Eastern<br />

Mediterranean), and an E-W transect across the<br />

Mediterranean Sea to sample and study organic-rich layers<br />

called Sapropels.<br />

Leg 163 N. Atlantic Arctic Gateways<br />

This is the second of two North Atlantic-Arctic<br />

Gateways (NAAG) legs. The first leg, ODP Leg 151 was<br />

drilled August - September of 1993. The scheduled second<br />

le~ of NAAG drilling will focus on the same goals as<br />

NAAG I but will also collect cores to try and resolve<br />

millermial scale climate variability and provide links to<br />

ice core data.<br />

Leg 164 Gas Hydrates<br />

Gas hydrates are a solid phase composed of water and<br />

low molecular weight gases (~redominantly methane)<br />

which form under conditions of low temperature, high<br />

pressure, and gas saturation; conditions that are common<br />

in the upper few hundred meters of rapidly accumulating<br />

marine sediments. The main o6jechves of the proposed<br />

leg are to investigate the in situ characteristics of gas<br />

hydrates.<br />

Leg 165 Test of the DCS<br />

Throughout the past six years the Ocean Drilling<br />

Program has expended considerable effort on the design<br />

and development of a Diamond Coring System (DCS).<br />

The Planning Committee has tentatively scheduled an<br />

engineering leg during which the prime objective will be<br />

a test of the diamond coring system and in particular the<br />

secondary heave compensation system.<br />

Report of "Radiolarian events" Symposium<br />

International Geological Congress, Kyoto, Japan August, 1992<br />

Symposium "Radiolarian events" of IGC (29th<br />

International Geological Congress) held on August 24-25<br />

convened by Drs. Patrick DE WEVER (Univ. Pierre et<br />

Marie-Curie, France), WANG Naiwen (Chinese Acad.<br />

Geol Sci., China) and Akira YAO (Osaka City Univ.,<br />

Japan) in the Kyoto International Conference Hall.<br />

Twenty-two abstracts were submitted covering<br />

biostratigraphy, paleobiogeography and paleoecology of<br />

Phanerozoic <strong>radiolaria</strong>ns. (Two presentations were<br />

canceled.) The following was the program of symposium<br />

Chairpersons: P. DE WEVER and A. YAO;<br />

A. ORAL SESSION (August 24, 1992)<br />

Aita, Y.: Triassic and Jurassic high latitude <strong>radiolaria</strong>n<br />

faunas from New Zealand<br />

Blome, C.D. and Reed K.M.: Permian <strong>radiolaria</strong>n<br />

faunas in the Grindstone terrane of central Oregon and<br />

their similarities to coeval Japanese faunas<br />

Akira Yao<br />

Joides Journal, February 1994<br />

Hori, R.: Radiolarian Toarcian event recorded in bedded<br />

cherts from Japan<br />

Ishida, K.: Radiolarian assemblage from the<br />

Kimmeridgian ammonite-bearing formation of the<br />

Torinosu Group in East Shikoku, Southwest Japan<br />

Ishiga, H.: Recent progress of the Paleozoic <strong>radiolaria</strong>n<br />

biostratigraphy<br />

JURASSIC-CRETACEOUS WORKING<br />

GROUP (Baumgartner, P.O.; Gorican S.; Jud,<br />

R.; O'Dogherty L. [co-leaders], Conti, M.; Danelian,<br />

T.; De Wever, P.; Dumitrica, P.; Kito, N.; Marcucci, M.;<br />

Matsuoka, A.; Steiger, T. and Urquhart, E. [principal<br />

contributors]: Middle Jurassic-Early Cretaceous <strong>radiolaria</strong>n<br />

biochronology of Tethys and Circum-Pacific low<br />

paleolatitudes<br />

Ling, H.Y.: Paleogene <strong>radiolaria</strong>n events<br />

Matsuoka, A.: Low-latitude Middle Jurassic to Lower<br />

Cretaceous <strong>radiolaria</strong>n stratigraphy in the western Pacific

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