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Concentration of diatom frustules in Lake Michigan sediment cores 1
Author(s) -
Parker Jon I.,
Edgington David N.
Publication year - 1976
Publication title -
limnology and oceanography
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.7
H-Index - 197
eISSN - 1939-5590
pISSN - 0024-3590
DOI - 10.4319/lo.1976.21.6.0887
Subject(s) - diatom , biogenic silica , photic zone , sediment , water column , sediment core , sink (geography) , dissolution , deposition (geology) , geology , environmental chemistry , frustule , oceanography , environmental science , hydrology (agriculture) , phytoplankton , ecology , chemistry , geomorphology , nutrient , biology , cartography , geotechnical engineering , geography
The concentration of diatom frustules was determined in 14 sediment cores that were dated by 210 Pb and 137 Cs techniques. The concentration in the 0–0.5‐cm sediment layer varied from 6.31 × 10 5 to 3.71 × 10 7 frustules g dry wt −1 . The annual deposition of frustules to the sediment ranged from 7.00 × 10 3 to 5.20 × 10 5 frustules cm −2 yr −1 , <5% of the estimated annual diatom production based on average annual diatom standing crop, turnover rate, and depth of the euphotic zone. The vertical distribution of frustules in every core showed a logarithmic decrease of at least two orders of magnitude in a depth equivalent to 80–100 years B.P. Scanning electron photomicrographs of frustules from the sediment show evidence of dissolution. Dissolved silica concentrations in deep and interstitial water support the conclusion that diatom frustules are dissolving in both the water column and sediment. The permanent sediment is probably not a major sink for particulate biogenic silica in Lake Michigan.