Age determination of sediment cores from the Northeast Atlantic


Autoria(s): Trauth, MH; Sarnthein, Michael; Arnold, Maurice
Cobertura

MEDIAN LATITUDE: 65.531667 * MEDIAN LONGITUDE: -0.000556 * SOUTH-BOUND LATITUDE: 52.448333 * WEST-BOUND LONGITUDE: -16.656667 * NORTH-BOUND LATITUDE: 72.111667 * EAST-BOUND LONGITUDE: 9.266667 * DATE/TIME START: 1988-07-21T00:00:00 * DATE/TIME END: 1990-08-11T00:00:00

Data(s)

15/01/1997

Resumo

Radiocarbon dating series, bulk sediment, and organic carbon flux from various Atlantic deep-sea regions reveal that the thickness of the bioturbated zone increases by 2 cm if food supply increases by 1 gC/m**2/yr (r = 0.8). Bulk sediment accumulation rates do not influence the depth of bioturbational mixing under normal pelagic sedimentary conditions. We believe that this relationship between nutrient supply and benthic mixing can be used for a quantitative and time-variable unmixing procedure to improve high-resolution stratigraphic correlations and paleoclimatic interpretations of deep-sea records.

Formato

application/zip, 3 datasets

Identificador

https://doi.pangaea.de/10.1594/PANGAEA.730489

doi:10.1594/PANGAEA.730489

Idioma(s)

en

Publicador

PANGAEA

Direitos

CC-BY: Creative Commons Attribution 3.0 Unported

Access constraints: unrestricted

Fonte

Supplement to: Trauth, MH; Sarnthein, Michael; Arnold, Maurice (1997): Bioturbational mixing depth and carbon flux at the seafloor. Paleoceanography, 12(3), 517-526, doi:10.1029/97PA00722

Palavras-Chave #Age, 14C AMS; Age, 14C calibrated, CALIB (Stuiver & Reimer, 1993); Age, 14C milieu/reservoir corrected (-400 yr); Age, dated; Age, dated standard deviation; Age dated; Age std dev; Arctic Ocean; Biscaya; Calender years; Depth; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Depth bot; Depth top; Giant box corer; GIK17045-2; GIK17730-2; GIK23259-3; GKG; M11/1; M13/2; M7/2; Meteor (1986); Norwegian Sea; Quaternary Environment of the Eurasian North; QUEEN
Tipo

Dataset