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BRIGHAM YOUNG UNIVERSITY GEOLOGY STUDIES Volume 44,1999 BRIGHAM YOUNG UNIVERSITY BRIGHAM YOUNG UNIVERSITY GEOLOGY STUDIES Volume 44,1999 CONTENTS Symmetrodonts from the Late Cretaceous of Southern Utah, and Comments on the Distribution of Archaic Mammalian Lineages Persisting into the Cretaceous of North America ................................ Richard L. Cifelli and Cynthia L. Gordon I A Large Protospongia Hicksi Hinde, 1887, from the Middle Cambrian Spence Shale of Southeastern Idaho ................................ Stephen B. Church, J. Keith Rigby, Lloyd E Gunther, and Val G. Gunther 17 Iapetonudus (N. gen.) and Iapetognathus Landing, Unusual Earliest Ordovician Multielement Conodont Taxa and Their Utility for Biostratigraphy .................................. Robert S. Nicoll, James E Miller, Godfrey S. Nowlan, John E. Repetski, and Raymond L. Ethington 27 Sponges from the Ibexian (Ordovician) McKelligon Canyon and Victorio Hills Formations in the Southern Franklin Mountains, Texas ...............J. Keith Rigby, C. Blair Linford, and David Y LeMone 103 Lower Ordovician Sponges from the Manitou Formation in Central Colorado ...................................................... J. Keith Rigby and Paul M. Myrow 135 Sponges from the Middle Permian Quinn River Formation, Bilk Creek Mountains, Humboldt County, Nevada .............................. J. Keith Rigby and Rex A. Hanger 155 A Publication of the Department of Geology Brigham Young University Provo, Utah 84602 Editor Bart J. Kowallis Brigham Young University Geology Studies is published by the Department of Geology. This publication consists of graduate student and faculty research within the department as well as papers submitted by outside contributors. Each article submitted is externally reviewed by at least two qualified persons. ISSN 0068-1016 6-99 650 29580 Symmetrodonts from the Late Cretaceous of Southern Utah and Distribution of Archaic Mammals in the Cretaceous of North America RICHARD L. CIFELLI and CYNTHIA L. GORDON Oklahoma Museum of Natural History and Department of Zoology, University of Oklahoma, Norman, Oklahoma 73019 ABSTRACT New materials of Spalacotheriidae (Symmetrodonta, Mammalia) from the Late Cretaceous (Turonian through early Campanian) of the Kaiparowits region, Utah, add to knowledge of three species, Symmetro- dontoides oligodontos, S. foxi, and Spalacotheridium mckennai. Details of molar structure (e.g., reduction of m7, proportions of lower molar paraconid and metaconid) clarify relationships of these taxa, indicating that 1) S. mckennai is derived with respect to geologically older S. noblei; 2) Symmetrodontoides spp. form a monophyletic, terminal clade; and 3) all can be included in a monophyletic subfamily, Spalacolestinae. North American spalacotheriids represent an endemic group that enjoyed a modest radiation in the medial Cretaceous and maintained a broad geographic distribution through the early Campanian. Symmetrodonts are but one of a number of archaic mammalian groups known from faunas of the North American Cretaceous, which are otherwise dominated by multituberculates and marsupials. The history of these groups is poorly understood but evidently complex. Some, such as triconodontids (?and picopsids), also rep- resent North American endemics that radiated in the medial Cretaceous and may have been restricted to northerly faunas in the Campanian; others, such as spalacotheriids and a possible clade of marsupial-like tri- bosphenic mammals, may have been restricted to the south during at least part of the Campanian. Deltatheroidans, known in North America as early as the Turonian, may have arrived on the continent via immigration from Asia on two separate occasions. INTRODUCTION AND BACKGROUND (Cifelli and others, 1997; Eaton and Nelson, 1991). Finally, the uppermost, late Campanian part of the sequence is The Kaiparowits region of southern Utah includes a correlative with vertebrate-yielding units ranging from well-exposed, thick, relatively continuous series of largely southern Canada to southern Texas, and suggests some terrigenous sedimentary rocks spanning much of the degree of biogeographic zonation or provinciality in the Upper Cretaceous. Vertebrate faunas including ~nammals Late Cretaceous of North America (e.g., Cifelli, 1994; have been recovered from a number of horizons (Eaton Lehman, 1997; Rowe and others, 1992). and Cifelli, 1988; Eaton and others, in press). Though some Among the rarest of the mammals from the Cretaceous units remain poorly sampled and significant gaps exist of the Kaiparowits region are the symmetrodonts. These between some of the fossil-bearing horizons, these assem- are of particular interest to students of mammalian evolu- blages collectively merit attention for several reasons. tion because their "reversed triangle" pattern formed by First, they include representation of an otherwise poorly principal molar cusps is thought to be antecedent to the known interval in mammalian history, the early Late Cre- more complex molar crowns seen in eupantotheres and, taceous (see, e.g., Clemens and others, 1979). Second, the ultimately, tribosphenic mammals-marsupials, placentals, faunas span nearly 20 Ma and thereby provide unique evi- and fossil relatives (e.g., Butler, 1939; Patterson, 1956). dence bearing on in situ changes in the terrestrial ecosys- The Order Symmetrodonta was founded on taxa from the tem through the Late Cretaceous; the nearby fauna from Late Jurassic (Simpson, 1925). More ancient, extremely the uppermost Cedar Mountain Formation, central Utah, primitive forms (see Cassiliano and Clemens, 1979; Prothero, extends this record to the Albian-Cenomanian boundary 1981; Sigogneau-Russell, 1983; Sigogneau-Russell and 2 BYU GEOLOGY STUDIES 1999, VOL. 44 Hahn, 1995) were later added, as well as Cretaceous taxa, units of southern Utah, that evidently belong to sym- some of which are highly specialized (e.g., Bonaparte, 1990; metrodonts or other primitive mammals. Finally, we com- Fox, 1985; Sigogneau-Russell, 1989, 1991; Sigogneau- ment on the geographic and temporal distribution of sym- Russell and Ensom, 1997). Thus recognized, the Symme- metrodonts and other groups of archaic mammals that trodonta is a heterogeneous, long-ranging assemblage of persisted, in a limited fashion at least, through much of debatable taxonomic standing (e.g., Prothero, 1981; Rougier the Late Cretaceous in the Western Interior of North and others, 1996). Indeed, many included species are America. known only by isolated teeth, and as a result symmetro- donts are commonly ignored in general treatments of METHODS mammalian relationships, despite their widely acknowl- edged importance (e.g., Rowe, 1988). All specimens reported herein consist of isolated teeth The Cretaceous of southern Utah has yielded three or dentigerous jaw fragments, collected by underwater symmetrodonts (Cifelli, 1990a; Cifelli and Madsen, 1986), screenwashing and associated fossil concentration and all referable to the Spalacotheriidae. This family, known recovery techniques (Cifelli and others, 1996). Rock samples from the Cretaceous both of the New and Old World, from the Wahweap Formation, indurated with calcium appears to be monophyletic, with North American taxa carbonate, were disaggregated in dilute (10%) acetic acid. placed in the endemic subfamily Spalacolestinae (see Dental terminology (see discussion in Cifelli and Madsen, Cifelli and Madsen, in press). Each of the spalacotheriids in press) is shown in Fig. lA, B. Measurements, in mm, from southern Utah was based on one or two teeth only. were taken with a Reflex microscope (see MacLarnon, Herein we describe newly-collected fossils that add to 1989). These data are automatically recorded to 0.001 mm, knowledge of these species and their relationship with and the figures are given here verbatim, although this other members of the Spalacotheriidae. We also describe does not account for measurement error. Teeth of spala- enigmatic specimens, from the same Upper Cretaceous cotheriids are extremely small and fragile, and as a result protoconid distal stylar cusp paracristid protocristid mesial cingular cusp distal cingular cusp paraconid metawnid paracone Figure 1. Measurements and dental terminology. A, C, right lower molar in occlusal view. B, D left upper molar in occlusal ~iew. Abbreviations: L, greatest mesiodistal length; greatest labiolingual width (afer Cqelli and Madsen, in press). lower rnolars comnrorrly 1,ic.k parts of th(1 c~ingulunr;hence, S~rrokyIlollow \tc~rtrl)c~co~~sists of ~rltt~rk)(~(l(ledIIIII~- ~rreasllrc~ment\(Fig. 1C, 11) mere t,tlie~rrtrir-rus tlrc cingu- \tones, carl~orr,tcc>or~\trriltlstoncs, ar-ttl coals (Eatotr, 1981). lum. 'The identifieation of toot11 locr~s,ilnport,lnt in assess- ?I'h~sll11it 11,~syiclclccl a tlicer\c f'irina of m,tmr-rl,lls nr~tl i11g intr,apc~cificant! intc~rspccifictliff(~rc~~rcc~s, is 1)rol)leln- other tcrrostri,tl vt~tt~l>ratt.s(Cifelli, 1990a, E,lton, 1995, atic for sp~ilacotlreriicls.in \vhicli 5pcci1tir~rrscorrsist of i\o- E,ttoir '1nc1 C:iti.lli, 1988, E,iton ancl others, in prc5s) horn 1;ttttl tcetll ,u~dthe dentid ti~rrnulair1clr1dt.s :I high 111tnrl)er tl~cxuiiddlt. /o~rc~of P(xtc~rso~~(1 969). This hori~ouis lrc4ic\ t~l of molar\ that c1iffcffi.rfronl c;icll otlror in sul,tle \\a>\. Our to I)c of ldte ~tridcll~to early l'tte 'li~i-oni,~~~age jE,itorr, itlcrrtification of tooth positio~lis I),tsrci err co~nparisort 1995). I.i)ssilcrcportetl llt*rcincome fi-om tlrree sites in tlrcl with tax,^ kno\vrl by partial or cornpletc, tooth series. Snrok) tlollo\\ \Ic11rrl)c~r.blN,I 995 (=
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