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Paleontological Contributions THE UNIVERSITY OF KANSAS PALEONTOLOGICAL CONTRIBUTIONS June 9, 1967 Paper 18 TRACE FOSSILS FROM TWO UPPER PENNSYLVANIAN SANDSTONES IN KANSAS KLAUS BANDEL Geologisch-Pahontologisches Institut, Rheinische Friedrich-Wilhelm-Universitdt, Bonn ABSTRACT Trails and burrows from two sandstones of the Upper Pennsylvanian of Douglas County, Kansas, are described and interpreted. Some of these are known from the literature, others are new. The trace fossil fauna suggests deposition of the sandstones in littoral shallow water. Although shelly fossils in both units are similar, the differences in the two trace-fossil faunas which have only two species in common indicate presence of two different environments. INTRODUCTION During the spring of 1966, while attending the Pennsylvanian (Fig. 1) Both sandstones are of University of Kansas, I had opportunity to study marine origin. the Pennsylvanian rocks in Kansas. This paper is The sandstones of the Rock Lake Shale con- concerned with two rock units in the neighbor- tain Myalina and Aviculopecten, in addition to hood of Lawrence, Douglas County, Kansas, other less common marine fossils. The Rock Lake which include sandstone beds containing abun- Shale Member is overlain by the South Bend dant, well-preserved trace fossils. Two outcrops, Limestone Member, a fossiliferous limestone with one close to Eudora (Killough quarry, NW 1/4 abundant fusulinids and several species of brachi- sec. 20, T. 13 S., R. 21 E.) and the other at Blue opods. The base of the Rock Lake Shale is formed Mound (NE ¼, SW 1/4 sec. 22, T. 13 S., R. 20 by the Stoner Limestone containing fusulinids, E.), were studied in detail and trace fossils from bryozoans, brachiopods, crinoids, and echinoids. the sandstones were collected. Sandstones of the Vinland Shale at Blue The sandstones studied at the Killough quarry Mound contain Myalina, and shales interbedded near Eudora are part of the Rock Lake Shale with them contain septarian concretions with a Member of the Stanton Limestone of the Lansing brachiopod and molluscan fauna. The Vinland Group, Missourian Stage, Upper Pennsylvanian, Shale is overlain by the Haskell Limestone con- and those studied at Blue Mound belong to the taining a rich marine fauna, and underlain by the Vinland Shale Member of the Stranger Forma- Westphalia Limestone which contains ostracodes tion of the Douglas Group, Virgilian Stage, Upper and tiny gastropods. 9 The University of Kansas Paleontological Contributions—Paper 18 The fossil assemblages in the sandstones and ADOPTED NOMF.NCLATURE in the underlying and overlying limestones of GENERALIZEu a. G..... n 4") n both units indicate a marine environment of FORMATIONS AND Mt MR FIRS 0 — St row: a deposition of the two members. Stratigraphically c...) . the two units are not far apart and the fossil Ireland Ss. content is similar. — N — Fossil tracks, trails, and burrows resulting from biological activity furnish information about the sediment in which they are found. The origin 411.... of many tracks, trails, and burrows is difficult to Robbons Sh. interpret and resulting conclusions are uncertain. However, trace fossils have the advantage of r___ Ha kea Ls —_ being definitively autochthonous; they are, there- Vellond Sh. fore, important for interpretation of paleoenviron- Westphal a Ls. Z • 11.--- 0 < ments. .— ....... D a Z SEILACHER ( 1964) divided trace fossils into the I.. < Tonponorde Ss 5 > following five ethological groups: 1) Repichnia-- >- trails or burrows made by animals of the vagile z sai..... loton Ls. benthos during locomotion; 2) Pascichnia—wind- MM.'. Z LLI ing trails or burrows made by vagile mud-eaters, CS. cc reflecting a "grazing" activity in search for food, —. Lu a covering a surface more or less efficiently and Weston Sb. cL avoiding double coverage; 3) Fodinichnia—bur- D rows made by semisessile deposit-feeders in search 100 of food, at the same time providing permanent outh Bend Ls 11110.°11.1". • shelter; 4) Domichnia—permanent shelters dug Rock Lake Sb. 111/01.1 by vagile or semisessile animals that procure food MUM warollIN Stoner Ls. from outside the sediment as predators, scaven- r,rar".... t t..7 0 Eudora Sh. 2 Z 'c ...1n .... gers, or suspension-feeders; and 5) Cubichnia- coot. n Crsek Ls ..7) shallow resting tracks left by vagile animals hiding VII. Sh. temporarily in the sediment, usually sand, and WNW obtaining their food as scavengers or suspension- feeders. Flu. I. Part of Upper Pennsylvanian rock column of All groups, except the last, could be recognized Kansas (from O'Comvoit, 1963). in the two sandstones studied. Type specimens and others illustrated are de- Invertebrate Paleontology (KUMIP). The catalog posited in the University of Kansas Museum of numbers are given in the plate explanations. SYSTEMATIC DESCRIPTIONS Following practice adopted by FENTZSCHEL ASTERICHNUS LAWRENCENSIS 'Jamie!, n. sp. (1962), the trace-fossil genera are described in Plate 1; Plate 2, figure 4,6 Figure 2,3. alphabetical order. Diagnosis.—Starlike tracks with diameter of 4 to 12 cm., consisting of rays 5 to 8 mm. wide, in Genus ASTERICHNUS Bande!, n. gen. form of grooves or tubelike ridges; center of each track consisting of oval to round ridge; number of Type species.—Asterichnus lawrencensis BANDE.L, n. sp. unbranched rays 10 to 30. Diagnosis.—Starlike tracks in sediment just Description and discussion.—Single star tracks, above sediment -covered bedding plane; non- preserved as epireliefs, have a diameter of 4 to 12 branching star rays. cm. and are approximately circular in cross section. Bandel—T race Fossils from Upper Pennsylvanian in Kansas 3 Each track consists of 10 to 30 rays which are that the starlike tracks are found in a kind of grooves, 5 to 8 mm. wide, that may be partly filled linear pattern on the sandstone surface, suggesting by cylindrical structures (Pl. 1; Pl. 2, fig. 4). The movement of one or several animals in search of centers of the star tracks are irregularly oval knobs, new feeding grounds. A few of the starlike tracks some of which appear to consist of overlapping are connected by grooves, suggesting a trail made circles. The star tracks seem to show preference by movement of the animal on the sandstone sur- for ripple crests on bedding plane surfaces buried face. Again, the close similarity of these subsurface by sediment penetrated by the track-making or- tracks to surface tracks of Scrobicularia plana of ganism (Pl. 1; PI. 2, fig. 4,6). Rarely two struc- the North Sea tidal flats (ScriXFER, 1962) can be tures may overlap somewhat, but usually they are noted. This bivalve moves from one feeding area set far enough apart not to overlap. to the next close to the sediment surface, making The central knob of most starlike tracks ap- a groove between the star tracks. pears to be a broken-off tube that leads upward It cannot be decided what kind of animal made into the burrow of the animal that made these the tracks named Asterich nus. The large variety tracks. The overlying sediment into which the of animals that can produce star tracks on the burrow projected, is a silty clay, rich in iron sul- surface of sediment calls for caution. However, it fide and containing many fragments of wood. seems certain that it must have been a relatively Wood fragments are also common on the upper large organism, in which the organs used for surface of the sandstone beds, but are not present feeding had a diameter of about 5 to 8 mm. in them. The manner in which Asterich nus tracks were A section through the middle of one star made, that is along bedding planes in the sedi- structure showed that the tube does not continue ment, not on the sediment surface, distinguishes downward into the sandstone. Close to the central them from all other known Recent and fossil star part of the star tracks some tubelike sand-filled tracks. SCH;iFER (1962) described and illustrated ridges coated by silt on the outside are preserved. grazing tracks of the bivalves Macoma baltica and These ridges continue into grooves at their end Scrobicularia plana from North Sea intertidal where some of them are broken off. flats. These grazing tracks are strikingly similar Origin.—The animal that produced these to Asterich nus, but are formed on the sediment structures must have had its dwelling burrow in surface. HXNTZSCHEL (1939) described starlike the silty sediment above the sandstone bed on tracks of the small intertidal-flat-dwelling amphi- whose rippled surface the star tracks are super- pod, Corophium. A very peculiar producer of star imposed. The tracks can be interpreted as feeding tracks is a fish, Gobius microps, of the intertidal tracks made in very much the same way as star- flats of the Baltic Sea (HXNTzscHEL, 1935). NA- like structures are made by sediment-dwelling THORST (1900) described star tracks made by the organisms on the surface of the sediment. The annelids Glycera alba and Gonidia maculata, animal doubtless extended part of itself from the which live on muddy bottom in the North Sea burrow along the bedding plane, taking in sedi- at a depth of 15 feet. Nereis, a polychaete worm, ment of this area, extracting food particles from also produces starlike feeding tracks (HXNTzscHEL, it, and refilling part of the feeding burrow with 1940). The star track Paleocrista ostthuringiacus waste sediment. The cylindrical ridges are inter- HUNDT (1941), from the Ordovician Phycodes- preted to be refilled parts of the feeding burrows schichten of eastern Thuringia, has been inter- and the grooves are inferred to mark the primary preted as being of worm origin, and Spongia ottoi burrows made by the feeding animal. The animals GEINITZ, from Cenomanian sandstone of Saxony, closely followed the irregular bedding plane. They as of brachyuran origin.
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