Planktonic foraminifera and Quaternary paleoceanology of the Atlantic Ocean


Autoria(s): Barash, Max S
Cobertura

MEDIAN LATITUDE: 24.824389 * MEDIAN LONGITUDE: -15.242722 * SOUTH-BOUND LATITUDE: -23.001667 * WEST-BOUND LONGITUDE: -47.950000 * NORTH-BOUND LATITUDE: 63.933000 * EAST-BOUND LONGITUDE: 12.165000

Data(s)

25/11/1988

Resumo

An original method of paleotemperature analysis on planktonic foraminifera is substantiated and actively used for stratigraphy of bottom sediments and paleoceanologic reconstructions. On the base of this method, as well as on lithological, geochemical, and oxygen isotope data, radiocarbon dating, constructions of other investigators, etc., the main features of dynamic Quaternary paleoceanology of the Atlantic Ocean is reconstructed. It is discussed in the context of global paleogeography. Paleotemperature field, climatic zonation, paleoecology of foraminifera, position of the main water masses, water fronts, currents, distribution of sea ice boundaries, upwelling activity, benthic circulation, processes of sedimentation are econstructed and analyzed.

Formato

application/zip, 6 datasets

Identificador

https://doi.pangaea.de/10.1594/PANGAEA.771897

doi:10.1594/PANGAEA.771897

Idioma(s)

en

Publicador

PANGAEA

Direitos

CC-BY: Creative Commons Attribution 3.0 Unported

Access constraints: unrestricted

Fonte

P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow

Supplement to: Barash, Max S (1988): Chetvertichnaya Paleookeanologiya Atlanticheskogo Okeana (Quaternary Paleoceanology of the Atlantic Ocean). Nauka Publ. (Moscow): in Russian, 272 pp

Palavras-Chave #+ Globigerinoides tenellus; Age, 14C benzol synthesis; Age, dated; Age, dated standard deviation; Age dated; Age std dev; AK3-205GC; Akademik Kurchatov; AKU3; Archive of Ocean Data; ARCOD; Atlantic Ocean; Benguela Upwelling; C. nitida; Calculated; Candeina nitida; Counting, foraminifera, planktic; d18O cal; delta 18O, calcite; Depth; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Depth bot; Depth top; Foraminifera, planktic; Foram plankt; G. aequilateralis; G. anfracta; G. bradyi; G. bulloides; G. calida; G. conglobatus; G. crassaformis; G. digitata; G. dutertrei; G. falconensis; G. glutinata; G. hexagona; G. hirsuta; G. humilis; G. inflata; G. iota; G. menardii; G. menardii flexuosa; G. pachyderma d; G. pachyderma s; G. quinqueloba; G. ruber; G. rubescens; G. sacculifer; G. scitula; G. truncatulinoides; G. truncatulinoides d; G. truncatulinoides s; G. tumida; GC; Globigerina bulloides; Globigerina calida; Globigerina digitata; Globigerina falconensis; Globigerina quinqueloba; Globigerina rubescens; Globigerinella aequilateralis; Globigerinita bradyi; Globigerinita glutinata; Globigerinita humilis; Globigerinita iota; Globigerinoides conglobatus; Globigerinoides ruber; Globigerinoides sacculifer; Globoquadrina dutertrei; Globoquadrina hexagona; Globoquadrina pachyderma dextral; Globoquadrina pachyderma sinistral; Globorotalia anfracta; Globorotalia crassaformis; Globorotalia hirsuta; Globorotalia inflata; Globorotalia menardii; Globorotalia menardii flexuosa; Globorotalia scitula; Globorotalia truncatulinoides; Globorotalia truncatulinoides dextral; Globorotalia truncatulinoides sinistral; Globorotalia tumida; Gravity corer; Mass spectrometry; Mikhail Lomonosov; ML3; ML3_198-4GC; ML5; ML5_348; ML6_475; MULT; Multiple investigations; North Atlantic; O. universa; Orbulina universa; P. obliquiloculata; Pulleniatina obliquiloculata; S. dehiscens; Samp com; Sample comment; Sphaeroidinella dehiscens; T cal; Temperature, calculated
Tipo

Dataset