(Table 1) Interstitial water chemistry at DSDP Leg 80 Holes

Interstitial water studies of sediments recovered during DSDP Leg 80 (Goban Spur transect) indicate a well-developed dissolved-sulfate minimum at Site 548 resulting from increased sulfate reduction in the rapidly deposited Pleistocene sediment section. Changes in the concentration of dissolved stron...

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Bibliographic Details
Main Authors: Gieskes, Joris M, Johnston, Kirk
Format: Dataset
Language:English
Published: PANGAEA 1985
Subjects:
80-548
80-548A
80-549
80-549A
80-550
80-551
Alkalinity
total
Ammonium
Calcium
Chlorine
Deep Sea Drilling Project
DEPTH
sediment/rock
DRILL
Drilling/drill rig
DSDP
DSDP/ODP/IODP sample designation
Elevation of event
Event label
Glomar Challenger
Latitude of event
Leg80
Lithium
Longitude of event
Magnesium
North Atlantic/ESCARPMENT
North Atlantic/PLAIN
North Atlantic/SPUR
pH
Potassium
Salinity
Sample code/label
see reference(s)
Silicon
Strontium
Sulfate
North Atlantic
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.808109
https://doi.org/10.1594/PANGAEA.808109
Description
Summary:Interstitial water studies of sediments recovered during DSDP Leg 80 (Goban Spur transect) indicate a well-developed dissolved-sulfate minimum at Site 548 resulting from increased sulfate reduction in the rapidly deposited Pleistocene sediment section. Changes in the concentration of dissolved strontium at each site must be related to carbonate recrystallization processes.

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