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author Marcks, Basia
Santos, Thiago Pereira dos
Lessa, Douglas Villela de Oliveira
Cartagena-Sierra, Alejandra
Berke, Melissa A
Starr, Aidan
Hall, Ian R
Kelly, Roger P
Robinson, Rebecca S
author_facet Marcks, Basia
Santos, Thiago Pereira dos
Lessa, Douglas Villela de Oliveira
Cartagena-Sierra, Alejandra
Berke, Melissa A
Starr, Aidan
Hall, Ian R
Kelly, Roger P
Robinson, Rebecca S
collection Datos científicos de ciencias marinas y ambientales
contents Biogenic silica accumulation was obtained by analyzing approximately 200 mg of homogenized and freeze dried sediment for each sample. Cleaning, chemical treatment, and measurement followed protocols outlined in (Mortlock & Froelich, 1989, doi:10.1016/0198-0149(89)90092-7). Samples were measured with a UV Vis spectrophotometer at 812 nm wavelength. Full procedural replicates were performed on 163 of the 435 samples yielding an average standard deviation of 0.2 %. Samples were referenced to RICCA VerSpec SiO32- in 1 % NaOH for intercomparison. Opal mass accumulation rates were calculated by multiplying the fraction of opal by dry bulk density and sedimentation rates from Starr et al. (2021, doi:10.1038/s41586-020-03094-7).
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_945841
institution PANGAEA
language en
publishDate 2022
publisher PANGAEA
record_format pangaea
spellingShingle Opal mass accumulation rates from IODP Site 361-U1475
Marcks, Basia
Santos, Thiago Pereira dos
Lessa, Douglas Villela de Oliveira
Cartagena-Sierra, Alejandra
Berke, Melissa A
Starr, Aidan
Hall, Ian R
Kelly, Roger P
Robinson, Rebecca S
361-U1475B; 361-U1475C; 361-U1475E; 361-U1475F; Accumulation rate, biogenic silica; Age model; Age model (Starr et al., 2021); Agulhas Plateau; biogenic silica; Calculated, see abstract; DRILL; Drilling/drill rig; Event label; Exp361; Foraminifera-bound nitrogen isotopes; G. bulloides; G. inflata; Joides Resolution; mid-Pleistocene transition; opal; Opal, biogenic silica; Sample code/label; South African Climates (Agulhas LGM Density Profile); Subtropical Front
Biogenic silica accumulation was obtained by analyzing approximately 200 mg of homogenized and freeze dried sediment for each sample. Cleaning, chemical treatment, and measurement followed protocols outlined in (Mortlock & Froelich, 1989, doi:10.1016/0198-0149(89)90092-7). Samples were measured with a UV Vis spectrophotometer at 812 nm wavelength. Full procedural replicates were performed on 163 of the 435 samples yielding an average standard deviation of 0.2 %. Samples were referenced to RICCA VerSpec SiO32- in 1 % NaOH for intercomparison. Opal mass accumulation rates were calculated by multiplying the fraction of opal by dry bulk density and sedimentation rates from Starr et al. (2021, doi:10.1038/s41586-020-03094-7).
title Opal mass accumulation rates from IODP Site 361-U1475
topic 361-U1475B; 361-U1475C; 361-U1475E; 361-U1475F; Accumulation rate, biogenic silica; Age model; Age model (Starr et al., 2021); Agulhas Plateau; biogenic silica; Calculated, see abstract; DRILL; Drilling/drill rig; Event label; Exp361; Foraminifera-bound nitrogen isotopes; G. bulloides; G. inflata; Joides Resolution; mid-Pleistocene transition; opal; Opal, biogenic silica; Sample code/label; South African Climates (Agulhas LGM Density Profile); Subtropical Front
url https://doi.org/10.1594/PANGAEA.945841