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

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. I...

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Bibliographic Details
Main Author: Ivanova, Elena V
Format: Dataset
Language:English
Published: PANGAEA 2006
Subjects:
Akademik Boris Petrov
Akademik Sergey Vavilov
Archive of Ocean Data
ARCOD
ARK-XI/1
ASV11
ASV11-858-3
ASV11-880-3
ASV11-987
ASV13_1200
ASV14
ASV14-1183-GC
ASV858
ASV880
Barents Sea
BIGSET
BP00
BP00-07/05
BP01
BP01-62/04
EAST_GC
GC
GeoB3011-1
GeoB3011-2
Gravity corer
Gravity corer (Kiel type)
Indian Ocean
Kara Sea
KOL
M31/3
M31/3_KL39
M31/3-113_GC
Meteor (1986)
MUC
MultiCorer
NAST_GC
Oman Upwelling
PC
Piston corer
Piston corer (Kiel type)
Polarstern
PS2718-6
PS36
PS36/002
Russkaya Gavan Bay
S-17666
S-17954
SL
South China Sea
Antarctic
Arctic
Indian
Kol’
Pacific
Russkaya
Antarc*
Foraminifera*
North Atlantic
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.745081
https://doi.org/10.1594/PANGAEA.745081
Description
Summary: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.

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