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Observations on Opal Phytoliths in a Soil Biosequence in Southeastern Minnesota
Author(s) -
Verma Shive D.,
Rust R. H.
Publication year - 1969
Publication title -
soil science society of america journal
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.836
H-Index - 168
eISSN - 1435-0661
pISSN - 0361-5995
DOI - 10.2136/sssaj1969.03615995003300050035x
Subject(s) - vegetation (pathology) , phytolith , soil water , shrub , geology , horizon , botany , biology , soil science , pollen , medicine , physics , pathology , astronomy
The content of opal phytoliths was measured in selected horizons of six soils from Goodhue County, Minn. The highest amount of opal phytoliths occurred in a Typic Hapludoll (Kenyon series) suggesting a soil developed under dominant grass vegetation because most of the opal is derived from big bluestem ( Andropogon gerardi L.) and little bluestem ( A. scoparius L.). Opal phytoliths isolated from some horizons were similar in morphology to reference slides made of opal from burr oak ( Quercus macrocarpa Michx.), ironwood ( Ostrya virginiana (Mill.) K. Koch), and a shrub, hazel ( Corylus americana Walt.). Opal phytoliths in two associated Aquollic Hapludalfs (Kasson and Taopi series) were derived primarily from big and little bluestem and with minor amounts from trees. This suggested at least a period of forest vegetation. A striking feature of Kasson, Kenyon, and Taopi soils is the higher content of opal phytoliths in till material II which begins in the B 2 horizon at depths of about 50 inches. Possibly at one time the top of material II might have been prairie covered landscape and the overlying silty material was deposited later.