Titlebook: Reconstructing Ocean History; A Window into the Fu Fatima Abrantes,Alan C. Mix Book 1999 Springer Science+Business Media New York 1999 Atla

DEBT

新星

The Overturning Circulation of the Glacial Atlanticeconstructed using the oxygen isotopic composition of benthic foraminifera. In the upper ocean, currents are strong and density contrasts are large and can easily be resolved from the isotope data. Here we use sediment cores from the Bahamas and off the Atlantic coast of Florida to reconstruct the d

反应

Atlantic Alkenone Sea-Surface Temperature Recordste change in low latitudes versus high latitudes for both hemispheres. For this purpose, special emphasis is given to variations in alkenone-derived SST estimates at time scales of 10 to 100kyr. Tropical SST records show relatively warm temperature values during the penultimate glacial marine oxygen

Nonconformist

Antimicrobial

Abrupt Climatic Changes—Causes and Consequencesnts in oceanic records. Numerous high quality posters focused on this subject and will aliment the literature for years ahead. In the meanwhile, we intend in this introduction to present the four papers of this Chapter within the context of our present knowledge on the causes and consequences of abr

syncope

Glacial and Interglacial Hydrological Changes in the North Atlantic Oceanhydrological reconstructions, to deep water chemistry proxies, clearly indicate that major reorganizations of the Atlantic happened together with, and to some extent are probably responsible for the abrupt climatic shifts recorded in Greenland ice, but also in many marine and continental sites aroun

Endemic

Age Screening of Deep-Sea Corals and the Record of Deep North Atlantic Circulation Change at 15.4KAand inexpensively screened for their ages using an Inductively Coupled Plasma-Mass Spectrometry (ICP-MS) technique. With this new method, 300 samples have been sorted into 5,000 year age bins and several dozen of these are useful for coupled precise uranium series and radiocarbon dating. Together wi

entitle

Phase Lag of Antarctic and Greenland Temperature in the Last Glacial and Link Between Co2 Variationsst is the relation between high-latitude polar sites since they are a major component in climate change. Ice cores are a unique climate archive with a high temporal resolution which directly record the atmospheric composition of trace gases..We have established coherent time scales for two Antarctic

阐明

Endometrium