Description: OUlogoResearch in the Hembree Lab

Department of Geological Sciences, Ohio University

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My research interests lie with the interaction of sedimentological and biological processes. I am interested in animal-substrate interactions in ancient and modern continental (or “non-marine”) environments. These interactions are preserved in the fossil record as trace fossils. Trace fossils provide an in situ record of ancient biodiversity, ecology, and environment. The study of trace fossils, therefore, provides vital information for accurate paleoenvironmental reconstructions. As sensitive indicators of environmental and climatic change, ichnofossils are also useful for detailed sequence stratigraphic analysis.


In my research, I interpret the paleoenvironmental, paleoclimatic, and paleoecological significance of paleosols and ichnofossils preserved in the geologic record. This involves not only the study of paleosols and continental trace fossils throughout geologic time, but also the experimental study of burrowing behaviors of extant terrestrial annelids, arthropods, amphibians, and reptiles. My current research projects involve the study of the influence of climate changes on ancient soils and soil ecosystems including those of the Pennsylvanian and Permian of southeast Ohio, Permian of eastern Kansas, and the Eocene to Miocene of Colorado and Wyoming.


I am interested in recruiting motivated Master’s students interested in these research areas.  For more information see News and Opportunities.






















Continental Ichnology



My research in continental ichnology has covered a range of geologic time and depositional settings. My research on Paleozoic vertebrates of Kansas has involved the study of the aestivation burrows of the lysorophid amphibian, Brachydectes elongates, from pond deposits within the Lower Permian Speiser Shale (Hembree et al., 2004, 2005). These burrows represent the earliest evidence of aestivation behavior by tetrapods in the fossil record. Aestivation allows aquatic and semi-aquatic animals to survive long periods of time without water and has become common among extant amphibians and reptiles. Along with the detailed study of the surrounding paleosols, associated ichnofossils and body fossils, these aestivation burrows provide evidence for the interpretation of seasonality in the Permian of the North American midcontinent. 



Description: Speiser insitu burrows

Top view of in situ lysorophid burrow casts in an ephemeral pond deposit of the Permian Speiser Shale, eastern Kansas.



Description: Spieser burrows

Lysorphid burrow casts (Torridorefugium eskridgensis) containing skeletal material excavated from the Permian Speiser Shale, eastern Kansas.


My dissertation research covered a more recent period of paleoenvironmental change, the late Eocene and early Oligocene. I completed a detailed study of the ichnofossils associated with paleosols in the White River Formation of northeastern Colorado (Hembree and Hasiotis, 2007). These deposits contain the fossils of a number of burrowing vertebrate groups, including the Amphisbaenia, an order limbless lizard common in modern tropical to arid environments. The paleosols of the White River Formation contain a diverse assemblage of continental ichnofossils including those produced by dung beetles (Pallichnus and Macanopsis), bees (Celliforma), ants (Parowanichnus), earthworms (Edaphichnium), wasps, beetles, plants, and vertebrates. I used the lateral and vertical changes in the distribution of ichnofossils to interpret paleoenvironmental change in the sedimentary basin. Along with ichnofossils I have also applied paleopedologic and sedimentologic principles to determine which environmental changes within the basin were due to autogenic and allogenic processes.

Description: rhizoliths

Large rhizoliths (fossil roots) preserved in an Oligocene paleosol from northeast Colorado.


Description: earthworm pellet

Small, elliptical fecal pellets within an Oligocene paleosol. These are interpreted as earthworm fecal pellets.



Description: dung beetle burrows

A system of interconnected burrows and chambers interpreted as a dung beetle nest. Preserved within an Oligocene paleosol.


Description: dung ball

Cross sectional view of a dung beetle brood burrow in an Oligocene paleosol.


I am currently studying Pennsylvanian and Permian continental ichnofossils from the paleosols of southeast Ohio and West Virginia. The Pennsylvanian-Permian world contained all of the animals that comprise modern soil ecosystems. The most abundant of these soil organisms were the arthropods. Pennsylvanian and Permian fossils of arthropod detritovores include millipedes, arthropleurids, mites, and insects, all of which would have engaged in feeding and dwelling behaviors in the soil based on comparisons with modern examples. Fossils of arthropod herbivores include flying insects. These organisms would have had temporary interaction with the soil through the production of such reproductive structures as nests or brood burrows. Fossils of arthropod predators include scorpions and arachnids. Modern arthropod predators construct burrows for use as dwellings, temporary resting places, and reproduction. Amphibians and early reptiles, such as microsaurs, temnospondyls, and cotylosaurs, likely constructed burrows for use as dwellings, temporary nests, and possibly aestivation.


Description: Casselman trace 1


Description: Casselman trace 2

Ichnofossils interpreted as millipede burrows from the Pennsylvanian Casselman Formation, southeast Ohio.



Description: rhizo 3


Description: rhizo 2

Rhizoliths from paleosols of the Pennsylvanian Casselman Formation.


My research in continental ichnology also involves experimental work with modern organisms, or neoichnology. Through detailed field observation and laboratory experiments with modern burrowing animals, continental tracemakers and their trace morphologies may be correlated to: 1) such substrate conditions as soil texture, moisture, and organic content; 2) depositional environments; and 3) such climatic factors as temperature and precipitation. I have established an animal burrowing laboratory that includes such burrowing animals as scorpions, whip scorpions, spiders, centipedes, millipedes, salamanders, toads, and skinks. A major goal of this research is to develop an online database that provides qualitative and quantitative data on the burrows produced by an array of terrestrial animals, with variations in morphology tied to environmental changes. For more information on this research click here. 


Description: African millipedes

Specimens of the giant African millipede (Archispirostreptus gigas) used in burrowing experiments.


Description: African spiral combo                                                        

Casts of spiral burrows produced by A. gigas burrowing in loose, organic-rich sediment.







The study of paleosols is important to geologists and biologists alike. Paleosols provide unique evidence for interpreting ancient terrestrial ecosystems, environment, and climate. They also provide some of the best evidence of the evolution of terrestrial ecosystems in addition to a deep time perspective of the effects of the interaction of terrestrial organisms and the substrate. I have used paleopedology extensively along with my studies of continental ichnology. My research has included the study of paleosols from the Pennsylvanian and Permian of Kansas, Oklahoma, and Ohio, the Triassic of Colorado, the Eocene of Wyoming, the Oligocene of Colorado, South Dakota, Nebraska, and Wyoming, and the Miocene of Colorado and Bolivia. In addition, by studying the characteristics of modern through field work and laboratory analysis, the pedogenic features preserved in these paleosols have been used to interpret specific paleoenvironmental and paleoclimatic conditions.  


My current research on Pennsylvanian paleosols of Ohio incorporates field descriptions and laboratory analyses, including the determination of bulk geochemistry, clay mineralogy, and stable isotope ratios. There is an extensive record of Pennsylvanian and Permian paleosols in southeastern Ohio and West Virginia. Exposures of the Allegheny, Conemaugh, Monongahela, and Dunkard groups in particular allow for both lateral and vertical analyses of the strata. One 30 m section of the Conemaugh Group, for example, contains 10 different paleosols interpreted as four different soil types based on parent material, pedogenic modification, and ichnofossils.


Description: Dan with Pawnee paleosol

Miocene paleosols in northeast Colorado.

Description: Casselman paleosol 2


Description: Casselman paleosol 1

Pennsylvanian paleosols in southeast Ohio.





Copyright © 2007

Daniel Hembree

Last revised: 5/2019