Color b* value of sediment core LV76-21

The color b* values are widely used as a paleoproductivity proxy for the NW Pacific and its marginal seas (Nürnberg and Tiedemann, 2004; Riethdorf et al., 2013). The color b* index was measured onboard after sediment core splitting at 1 cm resolution using a Konica Minolta CM-700d spectrophotometer....

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Bibliographic Details
Main Authors: Gorbarenko, Sergey A, Kirichenko, Ivan S, Psheneva, Olga, Bosin, Aleksandr A
Format: Dataset
Language:English
Published: PANGAEA
Subjects:
Akademik M.A. Lavrentiev
AMS 14C ages
Benthic and planktonic foraminifera
Color
b*
DEPTH
sediment/rock
Detroit Seamount
GC
Gravity corer
IRD
LV76
LV76-21
magnetic susceptibility
productivity proxies
Spectrophotometer Konica Minolta CM-700d
Detroit
Pacific
Planktonic foraminifera
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.954775
Description
Summary:The color b* values are widely used as a paleoproductivity proxy for the NW Pacific and its marginal seas (Nürnberg and Tiedemann, 2004; Riethdorf et al., 2013). The color b* index was measured onboard after sediment core splitting at 1 cm resolution using a Konica Minolta CM-700d spectrophotometer.

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