Icaronycteris index Jepsen 1966
Creators: name: Jepsen, Glenn L.
Publisher: name: Zenodo
Year: 1966
Subjects: Biodiversity
Taxonomy
Animalia
Chordata
Mammalia
Chiroptera
Archaeonycteridae
Icaronycteris
Icaronycteris index

description: <i>Icaronycteris</i> <i>index</i> (4), new genus and species; Figs. 1 and 2; Tables 1- 4 Type: Princeton University Museum of Natural History No. 18150; skeleton lacking right fibula and several toe bones. Known distribution: Early Eocene; Green River Formation of ancient Fossil Lake; about 21 m above Wasatchian Knight Formation; northwest quarter section 13, Township 21 North, Range 117 West, 8 km west of Kemmerer, southwest Lincoln County, Wyoming. 41° 48'15"N, 110039'W. Previously illustrated: <i>Time</i> 37(1), 44 (6 Jan. 1941). Anatomy: Many of the vertebrate anatomists who have examined PU 18150, perhaps the smallest complete Tertiary mammalian skeleton, have remarked upon similarities in size and general structure to members of <b>the</b> <i>Myotis</i> group, probably because this genus of microbat is so well known and because it has a wider distribution than any other vertebrate genus except <i>Homo</i>. If the skull is counted as a single element, <i>L</i>. <i>index</i> had at least 254 bones and 38 teeth in its solid skeleton; all except a few of the 44 sesamoids in the wings and feet have been studied on one side or the other (or both) of PU 18150. From head to tail and from limb girdles to limb ends <i>L</i>. <i>index</i> has the following distinctive combination of qualities, with the few that are especially characteristic of Megachiroptera indicated by <i>M</i>: long narrow head; pre-maxillaries not united at midline (<i>M</i>); dental formula, (2.1.3.3.)/(3.1.3.3.) = 38; diastema between upper incisors; one root on P2 and p2, two on p3 and p4, three on P3 and P4; W-shaped labial wall of upper molars; metaconid and long, deep talonid basin ("postfossid") on p4; long nasal bones (<i>M</i>); shallow eye orbits; no postorbital processes on frontals or jugals; zygomatic arch, slender, long, and complete; very small sagittal and occipital ridges; palate projected rearward beyond posterior molars; stylohyals, long, slender, and articulating with bullae; dentary body, long, low, and slender; mental foramina below i 3 and p2; ascending process of dentary, broad anteroposteriorly, with high, rounded superior border (<i>M</i>); condyle of dentary, well above line of tops of molar cusps; angle of dentary, hook-shaped and pointed; vertebral formula, 7- 12-7-3-13 or 14; no vertebral fusion except in sacrum; no coalesced ribs; segments of sternum (5), not fused; mesosternum, not keeled; pubic bones, loosely united at symphysis; pubic spine, short and robust; long and free tail; 5th to 7th caudal vertebrae, larger than others; tail tapers abruptly near tip; large supraglenoid tuberosity on scapula; coracoid process of scapula, long and slendernot bifid; clavicle, heavy and not expanded at ends; trochiter of humerus, large and articulates with scapula; high flange-like deltoid crest on straight, slender humerus; relatively short radius; no trace of sesamoid at end of ulna; large scapholunar; very flexible metacarpophalangeal joint; claw on thumb, not hooded; claw on index finger (<i>M</i>); digital formula, 2-3-3 -3 -3 (wing) and 2-3-3 -3 -3 (foot); all claws of wings and feet, compressed laterally; decreasing order of finger length, 3-4- 5-2-1; femur comparatively robust; femur has a distinct, very short neck between head and shaft; femur head and neck, at angle to shaft; fibula, slender and well developed; fibula, slightly longer than tibia; tibia, shorter than femur; metatarsal I, shorter and heavier than others; big toe, shorter than other toes; no calcar; decreasing order of toe length, 4-3-2-5-1. Characteristics of <i>I</i>. <i>index</i> that might be called "primitive" or "generalized," or lacking specialization among bats, are the (i) large number of teeth, (ii) shapes of teeth, (iii) uncoalesced ribs, vertebrae, and sternal segments, (iv) lack of prominent keel on the mesosternum, (v) long tail, (vi) shape of scapula, (vii) relatively short ra.- dius, (viii) index claw, (ix) complete phalangeal formula, (x) head and neck of the femur being at an angle to the shaft, (xi) big toe being shorter than the others, (xii) absence of calcar, and (xiii) low aspect ratio of the wings (see 5). Attempts to reconstruct the taphonomic (death-to-discovery) history of PU 18150 draw- upon several areas of geobiotic information and upon experiments based on the assumption that bat behavior, in life and death, and the physical and biotic conditions in nature were about the same in early Tertiary time as they are now. The following individual characteristics of PU 18150 are pertinent to its preservation: Age. All permanent teeth of the bat are fully erupted and worn to a degree normal in some 2- to 3-year-old microchiropts (6). The lingual slope of each molar parastyle shows comparatively heavy wear and many surficial fractures, perhaps the result of specific but unknown feeding habits. Epiphyses of the long bones are solidly welded to the shafts, and most of the cranial sutures seem to be obliterated. <i>Sex</i>. A small bone is in the appropriate position at the rear of the pelvis (Fig. 2, No. 88) to be an os penis; it has the tapered-club shape characteristic of the bacula of some small bats (7). <i>Skeletal pose</i>. Experiments indicate that the bone positions (Fig. 1) are normal for a dead bat in water-with the wings folded and the femora at angles to the vertebral column. In a bat having a well-developed uropatagium, however, the tail must be curved forward under the body when the femora are at the angle (about 450 to the body axis) of this specimen; this fact and the apparent absence of calcars are evidence that the bat was free-tailed. The anatomy of dead bats causes them to sink through water back first, with the wings trailing upward, and to rest, on the bottom, belly-side up. PU 18150 was probably buried in the calcitic ooze in this position, although no field records of its attitude were made at the time of its discovery. All minor displacements of the bones (except those of the left wrist) are readily explained by the collapse of the carcass as the muscles and ligaments and other tissues disintegrated, and as the weight of muds accumulating on the lake bottom pressed downward upon its ventral side. <i>Ingested material</i>. Within the area of the rib cage, a single scale (Fig. 1, A) of a small fish has evoked speculation that it may have been in the intestinal tract of the bat. This inference (supported by the provenience of the skeleton) is more reasonable than the possibility that the scale drifted into this position after the bat's death. Several kinds of bats eat fish (8), and some such forms, like <i>Pizonyx</i> and <i>Noctilio leporinus</i>, use their exceptionally large feet to gaff fish at the surface of the water. The feet of <i>I</i>. <i>index</i> are no larger than the feet of many living microbats; nor are special aptitudes for fishing or swimming otherwise indicated. Constituents of the very small mass of fecal material (Fig. 1, <i>D</i>) near the posterior border of the pelvis have not been fully identified; it may include bits of insect chitin and fragments of bacteria, algae, pollen, spores, and arthropods. <i>Cause and</i> <i>place of death</i>. No sign of disease, functional (respiratory, neural, or circulatory) failure, or injury is clearly manifest in the skeleton, although the slight displacement of bones in the lumbar, left carpal, and sternal areas may have resulted from attack by bird or fish; either of these predators, however, would probably have consumed the bat. Perhaps, but improbably, it was killed by lightning or hail. Neither can one determine where the bat died: on land (with subsequent transportation into the lake), above the water, or in it. Bats frequently drink water to compensate the great evaporation from their wings; some scoop up water with their mouths from streams and lakes during crepuscular and nocturnal flight. Sediments enclosing PU 18150 were deposited in quiet water, with little or no current at the bottom, but the body may have been carried to its site from shore (perhaps a few kilometers to the east) by surficial currents. The longer it drifted on the surface or in the water of the epilimnion, the more remarkable became the fact that it was not destroyed by fish or other predators before it sank into the near-sterile hypolimnion. <i>Flower</i>. Near the midpoint of the bat's tail is a small, delicate, unidentified flower (Fig. 1, <i>E</i>) having six petaloid structures and a stem; it presumably reached the lake floor about 1 year later than the bat, because it is enclosed in the tan carbonate layer of the varve that was originally the next one above that enveloping the skeleton. All flying mammals are formally classified in the ordinal taxon Chiroptera, which has no nonvolant members. It is usually divided into two suborders: (i) Megachiroptera, large Old World tropical fruit bats (all in the family Pteropidae), having a clawed ungual phalanx on the index finger and teeth of simple crown pattern, and (ii) Microchiroptera, almost worldwide in distribution and in many families, that lack an index claw and have diversified tooth forms that correlate with feeding habits. Upper molars of most of the insect-eating bats have a W-shaped external wall. (These statements grossly oversimplify the complexity of bat structure, but retain a classic, nearly true, and useful simplicity.) * Total less than the midline length of Ml-3 together, because the teeth are wasp-waisted. t Total of external labial border lengths is greater than midline length of M1I-3 because labial styles overlap. t Parastyle to innermost (lingual) base of cingulum, a diagonal dimension. § Total is greater than p2-m3 because of overlap. * Dorsal dimensions less than when measured around the curve of the original body. <i>Icaronycteris</i> <i>index</i> differs from all other known bats by combining the megabat characteristic of clawed index finger with the typical insectivorous microchiropteran structure of W-shaped labial crests on the upper molars. Allocation of this new form to either the Microchiroptera or Megachiroptera therefore makes it an exception to the long-serviceable generality that in bats an index claw is associated with simple teeth and that lack of that claw usually accompanies W-form molars. One could retain this old quality-pair criterion by continuing to ignore the few minor and inconvenient exceptions to it and to create a third suborder, Mesochiroptera, for the reception of the family Icaronycteridae and subordinate taxa in a taxonomic hierarchy for the species 1. <i>index</i>. Clearly, however, this species is more similar, and hence presumably more closely allied phylogenetically, to living microchiropterans (in teeth, "advanced" type of shoulder articulation of humerus and scapula, long tail, and many other anatomical features) than it is to megachiropts; therefore I tentatively classify it within the suborder Microchiroptera. It has not been possible to compare PU 18150 with the bones of all other Tertiary bats, but all described fossil bats are apparently more recent (mid-Eocene to Recent), and none has this combination of skeletal structures (9). Recently I have examined a partial skeleton (axial elements, limb girdles, and proximal segments of the limbs) of a bat (10) from a level of rock (11) apparently higher and less ancient (mid-Eocene, Bridgerian) than the level (early Eocene, Wasatchian) yielding PU 18150. A dense, hard matrix covers most of the soft bone of this specimen but study of the exposed parts, and of x-ray photos of the whole, shows that it is smaller than PU 18150 and different in many proportions (12). A few other American specimens of early Tertiary age (Paleocene and Eocene), once believed to represent taxa of bat ancestors, have been lost physically or by reallocation to nonbat orders (<i>Vesperugo anemophilus</i>, <i>Zanycteris paleocena</i>, <i>Nyctitherium</i>, <i>Picrodus</i>). Search in American pre-Eocene rocks has not found fossil bones that certainly pertain to bats. Thousands of man-hours of work on the eroded Paleocene rocks in the Bigborn Basin of Wyoming have discovered many thousands of fossil vertebrate specimens (many of them as small as analogous parts of most bats) but not a single fragment that is clearly related to bats. Paleocene sediments in other western states have been explored with similar results. Traces of early bats may have been sought in the wrong places; filled ancient crevices and fissures may be more favorable sites. Tilly Edinger (13) recently discussed a fossil, Princeton University No. 16494, from the late-Paleocene Silver Coulee beds in the Polecat Bench Formation of northwest Wyoming. This specimen, the cracked and incomplete rear part of a head and about 25 mm long, lacks the front half of the skull and all teeth, the conventional basis for most paleomammal classifications. Edinger believes that the development of the large midbrain acoustic colliculi (posterior corpora quadrigemina), clearly preserved in the flattened clay endocast, indicate that the animal was a chiropteran. Regretfully (as discoverer of the specimen) I cannot confirm Edinger's conclusion; the bones of the skull show that it was not the cranium of a flying animal: They are heavv, unlike the gracile and delicate analogous regions in heads of bats. Detailed osteologic analysis of the skull is here out of place, but all its observable structures closely resemble those of some larger contemporary miacid carnivores from the same quarry. One such specimen (Princeton University No. 16495), *with a midbrain endocast sufficiently well preserved to reveal the colliculi also, shows that the posterior ones are bigger than the anterior pair. The teeth of this specimen place it in or near the miacid genus <i>Protictis</i>, and many details of its posterior cranial structures ally it closely with PU 16494: in both crania the position of the fossa subarcuata is similar, and the mastoid process is similar in position and shape-as is the stylohyoid fossa, the fenestra ovale, the foramen lacerum medium, the glenoid pedicle, and many another feature. <b>Several</b> lower jaws almost certainly represent the species to which cranium PU 16495 pertains, and one dentary (PU 16523), with the diagnostic first lower molar in place, is of proper size and structure to be part of the same individual as PU 16494. Unfortunately, no other known cranial parts are assignable to the specific taxon of this jaw. * Taken from deepest part of concavity of proximal articular surface lo tip, for calculating length of foot. . Thus at least two Paleocene carnivores possessed comparatively large acoustical colliculi that may possibly indicate advanced ability to echolocate or some other auditory specialization. Land-living animals known to be capable of echolocation (or audioresponse) include some subterranean shrews, some terrestrial and arboreal members of the family Tenrecidae (14), and some cave-frequenting <i>birds-Steatornis caripensis</i> (oilbird) and <i>Callocalia brevirostris</i> (cave swiftlet).j A few other living mammals (certain marsupials, carnivores, and insectivores) apparently have relatively large posterior colliculi but, like most fruit bats, are not known to practice echolocation. Although remains of most classes of vertebrates are extremely rare in the <b>Green</b> River Formation, it is the source of many thousands of fish skeletons. Sediments of this formation were deposited in the waters of several separate lakes that formed in basins of accumulation in the Wyoming-Colorado-Utah region in early Tertiary time (15). Indirect evidences indicate that these lakes were not wholly contemporaneous-that their geologic cycles neither began nor ended at the same time (see 18, 19). Rocks of this formation west of Kemmerer, including those at the source of PU 18150, began as sediments on the floor of relatively small Fossil Lake, in a long, narrow depression north of Lake Uinta (Utah) and west of Gosiute Lake, both of which lakes were much larger than Fossil Lake at maximum development in their discrete hydrographic basins. At present the irregular and discontinuous outcrop pattern of the Fossil Lake sediments extends about 27 km in the <b>east-west</b> direction and about 48 km north-south. The bat skeleton was found in these sediments, a kilometer or two <b>west</b> of their <b>eastern</b> border, about 19 km west of the closest mapped sediments of Gosiute Lake. Part of the terrane between the fluctuating borders of these two Eocene lakes was probably as rugged as nearby eroded rock outcrops are today, with small fissures and caves that many bats favor. Various members and tongues of the Green River Formation in its several basins are interdigitated marginally with fluviatile mudstones that contain Wasatchian (early Eocene) and Bridgerian (mid-Eocene) mammals. Paleontologic evidence, based on fossil mammals collected (16) within a few kilometers of the source of the bat, indicates (17) that the local red-banded fluviatile rocks immediately below the Green River Formation of Fossil Lake are of Lysite age, representing the time span between the earlier (Gray Bull) and later (Lost Cabin) intervals of tripartite Wasatchian time-all of early-Eocene date (Sparnacian and Ypresian equivalents). About 107 m below the Green River Formation in this area, the gray fluviatile beds underlying the red-banded (Knight) sediments yield late-Paleocene mammals of Tiffanian provincial age. Evernden <i>et al</i>. (20) list potassiumargon ages of 49.2 X 106 years for a late Wasatchian "Wind River Formation" locality and 49.0 X 106 years for a late Wasatchian-early Bridgerian site in central Wyoming. These tests, coupled with the evidence from fossils, indicate that the lowest sediments of Fossil Lake are a little older than 49 million years. The entire mass of Fossil Lake sediments has been charted as of early Eocene age (21). Now at an altitude of about 2200 m above sea level, the bat stratum has been elevated tectonically from its original position, which was "... probably less than 1000 feet above sea level" (18), in early and mid-Eocene time. Analyses of the paleobiotas of the Green River Formation indicate that they developed in a humid subtropical climate like that of Alabama today. From analogies with the Ziirichsee and other central-European lakes, Bradley concludes that *the water of Fossil Lake was at least 30 and possibly more than 100 m deep. The marlstone matrix around, and fortunately slightly softer than, the bat's brittle bones is composed of varves or annually deposited pairs of layers of sediment; each year is represented by-two laminae of fine-grained clastic material, one being a thin darkbrown layer; the other, thicker, more granular, and light-buff in color. Bradley (letter, 22 March 1965) states that "Such varves form only in lakes that have a permanent, stagnant hypolimnion and that have enough Ca in the surface waters so that it precipitates each summer as calcite particles by reason of the photosynthesis of the phytoplankton and by warming of the surface waters." The thinner brown layers, richer in organic material, reached the floor of the lake between the periods of carbonate deposition. At present a 1 -cm-thick section of bat-quarry rock contains about 100 alternating light and dark layers, or about 50 varves (Fig. 2, <i>F</i>), but the original thickness of each uncompacted varve, when it was deposited at the bottom of the lake, was of course much grea
description: Published as part of <i>Jepsen, Glenn L., 1966, Early Eocene Bat from Wyoming, pp. 1333-1339 in Science (New York, N. Y.) (New York, N. Y.) 154 (3754)</i> on pages 1334-1338, DOI: 10.1126/science.154.3754.1333, http://zenodo.org/record/7841967
description: {"references": ["1. By C. Cushman, Rangley, Colo., and presented to Princeton Univ. in 1941.", "5. T. T. Struhsaker, J. Mammal. 42, 152 (1961).", "22. J. H. D. Hooper, Animals of Britain No. 2 (1962) (courtesy Sunday Times, London).", "6. L. C. Stegeman, ibid. 37, 58 (1956).", "7. P. H. Krutzsch and T. A. Vaughan, ibid. 36, 96 (1955).", "8. P. Bloedel, ibid., p. 390; J. Shortt, Proc. Zool. Soc. London 1863, 438 (1863); W. G. Reeder and K. S. Norris, J. Mammal. 35, 81 (1954).", "9. Remains of Oligocene, Miocene, and Pliocene bats are extremely rare because of their habitat, erosion, and chance; Eocene types are even rarer. Regarding Eocene bats, see: G. M. Allen, Bats (Harvard Univ. Press, Cambridge, Mass., 1939), 368 pp.; C. Dechaseaux, in Traite de Paldontologie, J. Piveteau, Ed. (Masson, Paris, 1958), tome 6, vol. 2, pp. 919 - 944; P. P. Grass 6, Traits de Zoologie (Masson, Paris, 1955), pp. 1729 - 1853; C. 0. Handley, J. Mammal. 36, 128 (1955); F. Heller, Nova Acta Leopoldina No. 2 (1935); P. Revilliod, Abhandl. Grossherz. Hess. Geol. Landesamtes 7, 157 (1917); Compt. Rend. Soc. Hist. Nat. GenAve 36, 93 (1919); M, m. Soc. Paleontol. Suisse 45, 131 (1922); P. Robinson, in M. C. McKenna, P. Robinson, D. W. Taylor, Amer. Museum Novitates No. 2102 (1962), p. 1 - 33.", "10. Univ. of Wyoming No. 2244, found in the Green River shales of Gosiute Lake; available by courtesy of P. McGrew.", "11. C. J. Hesse, Sci. Monthly 48, 147 (1939).", "12. Six more undescribed mid-Eocene (Bridgerian age) chiropteran fragments merit future attention although they reveal little or nothing of the ancestry or primordial structures of bats: Carnegie Museum No. 13711 - 14, each a tooth or part of one; Amer. Museum Nat. Hist. No. 55696, a dentary with the second molar; and Yale Peabody Museum No. 16222, part of a dentary, with two incomplete teeth (collected in 1875 but only recently recognized as chiropteran).", "13. T. Edinger, Anat. Record 138, 345 (1960); World Neurol. 2, 938 (1961); Amer. Zoologist 4, 5 (1964).", "14. E. Gould, Proc. Am. Phil. Soc. 109, 352 - 360 (1965).", "15. Anon., Proposed Fossil Butte National Monument (U. S. Nat. Park Serv., Midwest Region, Omaha, Neb., 1964), pp. 1 - 30 (geology by S. S. Oriel and J. I. Tracey).", "16. By the U. S. National Museum and Princeton Univ", "17. C. L. Gazin, Smithsonian Inst. Misc. Collections 144, 1 (1962).", "20. J. F. Evernden, D. E. Savage, G. H. Curtis, G. T. James, Amer. J. Sci. 262, 145 (1965).", "21. B. Schaeffer and M. Mangus, Nat. Hist. 74, 10 (1965).", "18. W. H. Bradley, U. S. Geol. Surv. Profess. Papers 158 - E, 87 (1929)."]}