Fossil Roots and Burrows

In general, to distinguish roots from burrows, we look for:

(a) plant material or structures (roots)

(b) diameter (relatively constant in burrows, frequently irregular
in roots, with secondary segments usually having a narrower
diameter than primary segments)

(c) branching style (usually lateral, i.e., more or less T-shaped in
burrows; either lateral or dichotomous, i.e., Y-shaped, in roots)
(Exception: Y-shaped branching is very common in crustacean
burrows.)

(d) structure of fill (active in some burrows; passive in originally
open burrows and in root cavities)

(e) enlarged junctions (e.g., in Thalassinoides)

Exceptions abound; nature is prolific and inventive. But a marked
difference in diameter between primary and secondary segments,
and a Y-shaped branching style without enlarged junctions, are
usually good indicators of a root origin even in the absence of
plant matter.

Dr. Andrew K. Rindsberg

Trace Fossil Menu
Useful Rules for Fossil Identification
Fossil Menu
Site Menu


St. Louis Pennsylvanian Fossils of the Altamont Formation