Relative contents of foraminifera species in bottom sediments of northern and southern seas

DOI

Correlation of paleoceanographic events in several key regions of the World Ocean: North Atlantic, Antarctic, West Arctic Seas, North Pacific and tropical Indo-Pacific has been carried out for the last 135 ka based on micropaleontological, stable isotope, geochronological (AMS-14C) and other data. It has been shown that the global thermohaline circulation controls remote climatic teleconnections on millennial-scale and partly on centennial-scale, while short-term climate changes are mainly transferred by the atmosphere. The basic information is given about the recent thermohaline circulation and stages of its development during Neogene.

Supplement to: Ivanova, Elena V (2006): The Global Thermohaline Paleocirculation. Scientific World, Moscow (original Russian version); Springer Science+Business Media B.V., 2009 (English translation), 320 pp

Identifier
DOI https://doi.org/10.1594/PANGAEA.745081
Related Identifier https://doi.org/10.1007/978-90-481-2415-2
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.745081
Provenance
Creator Ivanova, Elena V
Publisher PANGAEA
Publication Year 2006
Rights Creative Commons Attribution 3.0 Unported; https://creativecommons.org/licenses/by/3.0/
OpenAccess true
Representation
Resource Type Supplementary Publication Series of Datasets; Collection
Format application/zip
Size 13 datasets
Discipline Earth System Research
Spatial Coverage (39.914W, -20.608S, 111.525E, 79.925N); Barents Sea; Russkaya Gavan Bay, Barents Sea; Kara Sea; Indian Ocean; Oman Upwelling; South China Sea
Temporal Coverage Begin 1995-03-17T18:50:00Z
Temporal Coverage End 2001-09-04T00:00:00Z