PANGAEA_712496 Geochemistry of sediment core GeoB2809-4 Zabel, Matthias Geochemistry of sediment core GeoB2809-4 2009-02-11 PANGAEA Dataset https://doi.pangaea.de/10.1594/PANGAEA.712496 Investigator Matthias Zabel mzabel@uni-bremen.de Earth Science DEPTH, sediment/rock Calcium Carbon, inorganic, total Aluminium Iron Magnesium Manganese Carbon, organic, total Strontium Barium geoscientificInformation GeoB2809-4 Gravity corer (Kiel type) M29/2 HF/HNO3/H2O2 pressure digestion Element analyser CHN, LECO Meteor (1986) 1994-07-20 1994-07-20 Complete -36.331666666667 -36.331666666667 -51.521666666667 -51.521666666667 0.1 m (DEPTH, sediment/rock) 10.3 m (DEPTH, sediment/rock) GeoB Geosciences, University of Bremen unrestricted CC-BY-3.0: Creative Commons Attribution 3.0 Unported English PANGAEA Data Publisher for Earth & Environmental Science https://www.pangaea.de/ Data Center Contact Michael Diepenbroek info@pangaea.de

Leobener Str.

Bremen Bremen 28359 Germany online 360 data points text/tab-separated-values Zabel, Matthias; Bickert, Torsten; Dittert, Lars; Haese, Ralf R (1999): Significance of the sedimentary Al : Ti ratio as an indicator for variations in the circulation patterns of the equatorial North Atlantic. Paleoceanography, 14(6), 789-799, https://doi.org/10.1029/1999PA900027

For all details see the full metadata description at "https://doi.pangaea.de/10.1594/PANGAEA.712496"!

http://www.leco.com/ Element analyser CHN, LECO https://doi.org/10.1029/1999PA900027 Significance of the sedimentary Al : Ti ratio as an indicator for variations in the circulation patterns of the equatorial North Atlantic https://doi.org/10.2312/cr_m29 M29/2 https://en.wikipedia.org/wiki/RV_Meteor_(1986) Meteor (1986) https://www.geo.uni-bremen.de/page.php?langid=EN GeoB DIF 9.4 2009-02-11 2024-07-19