By Rainer Zahn (auth.), Fatima Abrantes, Alan C. Mix (eds.)
This quantity is one final result of the sixth foreign convention on Paleoceano graphy (ICP VI). The convention used to be held August 23-28, 1998 in Lisbon, Portugal. The assembly the normal layout of a small variety of invited oral shows complemented via a mess ofcontributed posters. Over 550 contributors attended, representing thirty international locations and approximately 450 posters have been awarded. The invited audio system addressed the most issues of the 5oral classes. The consultation themes have been: Polar-Tropical and Interhemisphere Linkages; Does the sea reason, or reply to, Abrupt Climatic Changes?; Biotic Responses to significant Paleoceanographic adjustments; prior hot Climates; and concepts In tracking Ocean heritage. this is often the 1st time in ICP historical past that the convention complaints are released. the purpose of the organisers with the ebook of this publication is two-fold: to supply an invaluable evaluation of the sphere and to record the ideas/controversies raised throughout the con ference which could stimulate destiny paintings. The e-book displays the preliminary intentions of the convention, however it isn't really a conven tional convention complaints, provided that the papers were reviewed by way of formal exter nal referees. all of the convention subject matters is brought by means of a evaluate article designed to summarize the cutting-edge in each one subject matter by means of articles ready by way of the invited audio system. As with such a lot convention complaints, each one subject is roofed heterogenously. a few issues have all of the anticipated contributions, others are much less good covered.
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Extra resources for Reconstructing Ocean History: A Window into the Future
For cores GeoB 1711-4 and ODP 658C, both of which exhibit a higher temporal resolution, additional stratigraphic tie points were derived from accelerator mass spectrometry (AMS) radiocarbon dating of foraminiferal tests. Detailed references for the data sources and core chronologies are given in the respective figure captions and in Table I. de). 2. Glacial-Interglacial SST Pattern Three different types of alkenone SST patterns can be recognized from the above selection of Atlantic records. The first type is the SST pattern shown in Fig.
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A. Durkoop, W. Hale, G Wefer, and H. Niebler, Planktonic foraminifera as recorders of past surface-water stratification, Geology, 25,335-338, 1997. N. K. Mayeda, Oxygen isotope fractionation in divalent metal carbonates, Journal of Chemical Physics, 5, 5547-5558, 1969. , and SJ. Lehman, Mid-Depth Circulation of the Subpolar North-Atlantic During the Last Glacial Maximum, Science, 259 (5098), 1148-1152, 1993. , The Gulf Stream, Rep. Supt. Us. Coast and Geod. , 459-620, 1891. P. Niiler, The velocity structure of the Florida Current from the Straits of Florida to Cape Fear, Deep-Sea Research, Suppl.