Hasiotis, Stephen T.1, Mary J. Kraus2
(1) University of Kansas, Lawrence, KS
(2) University of Colorado, Boulder, CO
ABSTRACT: Examples of how Ancient Soil Biota Mediated Features in Paleosols: Lower Eocene Willwood Formation, Wyoming
Paleopedogenic features of Lower Eocene Willwood paleosols in the Bighorn Basin,
Wyoming, include carbonate nodules and complicated paleosol color patterns. These features
are intimately related to ancient, above- and below-ground soil biota activities. Previous
studies attributed roots and root channels to these features. Willwood paleosols, however,
also show that animal burrows were important mediators of carbonate nodules and paleosol
color patterns.
Carbonate nodules precipitated in and around burrows and roots. Elliptical to spherical
carbonate nodules, 2 to 30 mm in diameter, are composed of solid to boxwork carbonate
surrounded by gray zones depleted of iron oxides. Distinct burrows and roots cemented by
carbonate are also present. These features grade into segments of burrows and roots offset
from the main trace by paleosol slickenside shear planes. In turn, these grade into
carbonate nodules with features attributed to burrows and roots but are dispersed through
the paleosol. Original shape and surficial morphology of burrow and root pieces are gone,
probably due to continued pedogenesis.
Red, yellow-brown, and purple mottles are common and attributed to roots as well as
activities of such soil organisms as bacteria, annelids, insects, and other arthropods.
Mottles range in size from 0.1 to tens of mm and in shape from crescents and spheres to
ellipses that overlap and crosscut one another. Immature paleosols have discrete burrows
with distinct mottle patterns. More mature paleosols have complex mottles that, on close
examination and by comparison to mottles in immature paleosols, are amalgamations of
different shapes and sizes of burrow remnants.
AAPG Search and Discovery Article #90026©2004 AAPG Annual Meeting, Dallas, Texas, April 18-21, 2004.