(Table 1) Distribution of planktic foraminifera in sediments from Core AMK4-410GC

DOI

Sediments in 36 cores recovered from the rift zone of the Reykjanes Ridge were dated on the basis of planktic foraminifera. Their ratios in samples were used to determine temperature of the water surface layer during the last glaciation. Benthic foraminifera were studied in 12 samples of surface sediments and in five cores, and conclusions made on changes in the bottom water layer from changes in composition of these benthic foraminifera.

Supplement to: Lukashina, Nadezhda P (1985): Stratigraphy of Upper Quaternary sediments from the rift valley of the Reykjanes Ridge (according to foraminiferal analysis). Oceanology, 25(4), 623-629

Identifier
DOI https://doi.org/10.1594/PANGAEA.756127
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.756127
Provenance
Creator Lukashina, Nadezhda P
Publisher PANGAEA
Publication Year 1985
Rights Creative Commons Attribution 3.0 Unported; https://creativecommons.org/licenses/by/3.0/
OpenAccess true
Representation
Resource Type Supplementary Dataset; Dataset
Format text/tab-separated-values
Size 91 data points
Discipline Earth System Research
Spatial Coverage (-31.617 LON, 58.358 LAT); North Atlantic