CBS Annual Conference Abstracts 2017
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Contents Part III. the LAST FIFTY THOUSAND YEARS
STATE OF MICHIGAN Insects ................................................................... 60 DEPARTMENT OF CONSERVATION Worms And Others ................................................ 61 P. J. Hoffmaster, Director The Pleasant Peninsulas .............................................62 Man and his Towns ......................................................69 THEY NEED NOT VANISH A DISCUSSION OF THE NATURAL RESOURCES In Conclusion .................................................................71 OF MICHIGAN Part III. THE LAST FIFTY THOUSAND YEARS "THE GOOD EARTH" Edited by HELEN M. MARTIN ir, sunlight, water, and soil are essential for the Acontinuance of life—plant, animal, and human life, from contributions by on the earth. Of these four basic requirements, the soil Shirley W. Allen, Geo. C. S. Benson, University of is most directly subject to the care and management of Michigan man. However, the soil has frequently been the object of man's most careless use and abuse. It is, therefore, Stannard B. Bergquist, L. R. Schoenmann, H. C. most fitting that the eminent soil scientist, A. F. Beeskaw, J. H. Kraemer, W. F. Morofsky, J. A. Porter, E. Gustafson, should begin his book on soils and soil C. Sackrider, Michigan State College management with: G. S. Mclntire, H. M. Martin, O. F. Poindexter, C. F. "During his existence upon the earth, man has depended upon Welch, Department of Conservation the soil, either directly or indirectly, for the production of the materials used by him for food and clothing and, in part, for the M. G. Adams, Stream Control Commission production of those used for fuel and shelter as well. Grains, Frank DuMond, Public Museum, Grand Rapids fruits, and vegetables that serve him as food grow directly on the soil. Cotton and flax yield materials that are made into Lynn Heatley, High School, Midland. -
RI Equisetopsida and Lycopodiopsida.Indd
IIntroductionntroduction byby FFrancisrancis UnderwoodUnderwood Rhode Island Equisetopsida, Lycopodiopsida and Isoetopsida Special Th anks to the following for giving permission for the use their images. Robbin Moran New York Botanical Garden George Yatskievych and Ann Larson Missouri Botanical Garden Jan De Laet, plantsystematics.org Th is pdf is a companion publication to Rhode Island Equisetopsida, Lycopodiopsida & Isoetopsida at among-ri-wildfl owers.org Th e Elfi n Press 2016 Introduction Formerly known as fern allies, Horsetails, Club-mosses, Fir-mosses, Spike-mosses and Quillworts are plants that have an alternate generation life-cycle similar to ferns, having both sporophyte and gametophyte stages. Equisetopsida Horsetails date from the Devonian period (416 to 359 million years ago) in earth’s history where they were trees up to 110 feet in height and helped to form the coal deposits of the Carboniferous period. Only one genus has survived to modern times (Equisetum). Horsetails Horsetails (Equisetum) have jointed stems with whorls of thin narrow leaves. In the sporophyte stage, they have a sterile and fertile form. Th ey produce only one type of spore. While the gametophytes produced from the spores appear to be plentiful, the successful reproduction of the sporophyte form is low with most Horsetails reproducing vegetatively. Lycopodiopsida Lycopodiopsida includes the clubmosses (Dendrolycopodium, Diphasiastrum, Lycopodiella, Lycopodium , Spinulum) and Fir-mosses (Huperzia) Clubmosses Clubmosses are evergreen plants that produce only microspores that develop into a gametophyte capable of producing both sperm and egg cells. Club-mosses can produce the spores either in leaf axils or at the top of their stems. Th e spore capsules form in a cone-like structures (strobili) at the top of the plants. -
Bayesian Total-Evidence Dating Reveals the Recent Crown Radiation of Penguins Alexandra Gavryushkina University of Auckland
Ecology, Evolution and Organismal Biology Ecology, Evolution and Organismal Biology Publications 2017 Bayesian Total-Evidence Dating Reveals the Recent Crown Radiation of Penguins Alexandra Gavryushkina University of Auckland Tracy A. Heath Iowa State University, [email protected] Daniel T. Ksepka Bruce Museum David Welch University of Auckland Alexei J. Drummond University of Auckland Follow this and additional works at: http://lib.dr.iastate.edu/eeob_ag_pubs Part of the Ecology and Evolutionary Biology Commons The ompc lete bibliographic information for this item can be found at http://lib.dr.iastate.edu/ eeob_ag_pubs/207. For information on how to cite this item, please visit http://lib.dr.iastate.edu/ howtocite.html. This Article is brought to you for free and open access by the Ecology, Evolution and Organismal Biology at Iowa State University Digital Repository. It has been accepted for inclusion in Ecology, Evolution and Organismal Biology Publications by an authorized administrator of Iowa State University Digital Repository. For more information, please contact [email protected]. Syst. Biol. 66(1):57–73, 2017 © The Author(s) 2016. Published by Oxford University Press, on behalf of the Society of Systematic Biologists. This is an Open Access article distributed under the terms of the Creative Commons Attribution Non-Commercial License (http://creativecommons.org/licenses/by-nc/4.0/), which permits non-commercial re-use, distribution, and reproduction in any medium, provided the original work is properly cited. For commercial re-use, please contact [email protected] DOI:10.1093/sysbio/syw060 Advance Access publication August 24, 2016 Bayesian Total-Evidence Dating Reveals the Recent Crown Radiation of Penguins , ,∗ , ALEXANDRA GAVRYUSHKINA1 2 ,TRACY A. -
A Rhinopristiform Sawfish (Genus Pristis) from the Middle Eocene (Lutetian) of Southern Peru and Its Regional Implications
Carnets Geol. 20 (5) E-ISSN 1634-0744 DOI 10.4267/2042/70759 A rhinopristiform sawfish (genus Pristis) from the middle Eocene (Lutetian) of southern Peru and its regional implications Alberto COLLARETA 1, 2 Luz TEJADA-MEDINA 3, 4 César CHACALTANA-BUDIEL 3, 5 Walter LANDINI 1, 6 Alí ALTAMIRANO-SIERRA 7, 8 Mario URBINA-SCHMITT 7, 9 Giovanni BIANUCCI 1, 10 Abstract: Modern sawfishes (Rhinopristiformes: Pristidae) are circumglobally distributed in warm wa- ters and are common in proximal marine and even freshwater habitats. The fossil record of modern pristid genera (i.e., Pristis and Anoxypristis) dates back to the early Eocene and is mostly represented by isolated rostral spines and oral teeth, with phosphatised rostra representing exceptional occurren- ces. Here, we report on a partial pristid rostrum, exhibiting several articulated rostral spines, from middle Eocene strata of the Paracas Formation (Yumaque Member) exposed in the southern Peruvian East Pisco Basin. This finely preserved specimen shows anatomical structures that are unlikely to leave a fossil record, e.g., the paracentral grooves that extend along the ventral surface of the rostrum. Ba- sed on the morphology of the rostral spines, this fossil sawfish is here identified as belonging to Pristis. To our knowledge, this discovery represents the geologically oldest known occurrence of Pristidae from the Pacific Coast of South America. Although the fossil record of pristids from the East Pisco Basin spans from the middle Eocene to the late Miocene, sawfishes are no longer present in the modern cool, upwelling-influenced coastal waters of southern Peru. Given the ecological preferences of the extant members of Pristis, the occurrence of this genus in the Paracas deposits suggests that middle Eocene nearshore waters in southern Peru were warmer than today. -
Chians in Nova Scotia,. by J. \V. DAWSON, LL.D., F.R.S
440 Dawson-New Oarboniferous Batmchians of Nova Scotia. ART. XLVIII.-On a Recent Di~covery of Oarbo?Jifero1.l.s Batra chians in Nova Scotia,. by J. \V. DAWSON, LL.D., F.R.S. 1. General Remarks. THE erect Sigillarire enclosed in the f!andstone overlying coal-group 15 of Section XV, Division 4 of the SOIl.th Joggins section, are perhaps the most remarkable repositories ever dis covered of the remains of Paleozoic land animals. As I have shown in discussing their character in my memoirs on the South Joggins Coal FOl'mation,* and my "Acadian Geology," some of these trees became em bedded in sandy deposits, and being rendered hollow by decay of their inner bark and the crumbling of their woody axes, remained for a long time as open holes or pits, gradually filling with vegetable debris and the wash of rains and land floods. They thus became places of habitation for land snails and millepedes, and pit-falls into which the smaller batrachians, prowling for prey among the undergrowth of the coal forest, fell and were unable to extri cate themselves. In this way the successive layers of deposit became stored with skeletons of batrachians which they have retained in an admirable st.ate of preservation. Onlrone sandstone at the Joggins is known to contain these reptiliferous trees, though erect Sigillarire are known at. more than sixty different levels, and many of these erect stumps have been broken up in the hope of making such discoveries. In the past summer, however, shells of Pupa vetustu were found bv Mr. -
Femur of a Morganucodontid Mammal from the Middle Jurassic of Central Russia
Femur of a morganucodontid mammal from the Middle Jurassic of Central Russia PETR P. GAMBARYAN and ALEXANDER 0.AVERIANOV Gambaryan, P.P. & Averianov, A.O. 2001. Femur of a morganucodontid mammal from the Middle Jurassic of Central Russia. -Acta Palaeontologica Polonica 46,1,99-112. We describe a nearly complete mammalian femur from the Middle Jurassic (upper Bathonian) from Peski quarry, situated some 100 km south east of Moscow, central Rus- sia. It is similar to the femora of Morganucodontidae in having a globular femoral head, separated from the greater trochanter and reflected dorsally, fovea capitis present, both trochanters triangular and located on the same plane, distal end flat, mediolaterally expanded, and somewhat bent ventrally, and in the shape and proportions of distal condyles. It is referred to as Morganucodontidae gen. et sp. indet. It is the first representa- tive of this group of mammals in Eastern Europe from the third Mesozoic mammal local- ity discovered in Russia. Exquisite preservation of the bone surface allowed us to recon- struct partial hind limb musculature. We reconstruct m. iliopsoas as inserting on the ridge, which starts at the lesser trochanter and extends along the medial femoral margin for more than half of the femur length. On this basis we conclude that the mode of loco- motion of the Peski morganucodontid was similar to that of modern echidnas. During the propulsive phase the femur did not retract and the step elongation was provided by pronation of the femur. Key words : Mammalia, Morganucodontidae, femur, anatomy, locomotion, Jurassic, Russia. Petr P. Gambaryan [[email protected]] and Alexander 0. -
Bayesian Phylogenetic Estimation of Fossil Ages
Bayesian phylogenetic estimation of fossil ages Alexei J. Drummond1;2;3 and Tanja Stadler3;4 1Centre for Computational Evolution, University of Auckland, Auckland, New Zealand; 2Department of Computer Science, University of Auckland, Auckland, 1010, New Zealand; 3Department of Biosystems Science & Engineering, Eidgen¨ossischeTechnische Hochschule Z¨urich, 4058 Basel, Switzerland; 4Swiss Institute of Bioinformatics (SIB), Switzerland. Corresponding author: Alexei J. Drummond, Centre for Computational Evolution, University of Auckland, Auckland, New Zealand; E-mail: [email protected] Abstract Recent advances have allowed for both morphological fossil evi- dence and molecular sequences to be integrated into a single combined inference of divergence dates under the rule of Bayesian probability. In particular the fossilized birth-death tree prior and the Lewis-Mk model of discrete morphological evolution allow for the estimation of both di- vergence times and phylogenetic relationships between fossil and extant taxa. We exploit this statistical framework to investigate the internal consistency of these models by producing phylogenetic estimates of the age of each fossil in turn, within two rich and well-characterized data sets of fossil and extant species (penguins and canids). We find that the estimation accuracy of fossil ages is generally high with credible intervals seldom excluding the true age and median relative error in the two data sets of 5.7% and 13.2% respectively. The median relative standard error (RSD) was 9.2% and 7.2% respectively, suggesting good precision, although with some outliers. In fact in the two data sets we analyze the phylogenetic estimates of fossil age is on average < 2 My from the midpoint age of the geological strata from which it was ex- cavated. -
Acosta Hospitaleche.Vp
vol. 34, no. 4, pp. 397–412, 2013 doi: 10.2478/popore−2013−0018 New crania from Seymour Island (Antarctica) shed light on anatomy of Eocene penguins Carolina ACOSTA HOSPITALECHE CONICET. División Paleontología de Vertebrados, Museo de La Plata, Paseo del Bosque s/n, B1900FWA La Plata, Argentina <[email protected]> Abstract: Antarctic skulls attributable to fossil penguins are rare. Three new penguin crania from Antarctica are here described providing an insight into their feeding function. One of the specimens studied is largely a natural endocast, slightly damaged, and lacking preserved osteological details. Two other specimens are the best preserved fossil penguin crania from Antarctica, enabling the study of characters not observed so far. All of them come from the uppermost Submeseta Allomember of the La Meseta Formation (Eocene–?Oligocene), Seymour (Marambio) Island, Antarctic Peninsula. The results of the comparative studies suggest that Paleogene penguins were long−skulled birds, with strong nuchal crests and deep temporal fossae. The configuration of the nuchal crests, the temporal fossae, and the parasphenoidal processes, appears to indicate the presence of powerful muscles. The nasal gland sulcus devoid of a supraorbital edge is typical of piscivorous species. Key words: Antarctica, Sphenisciformes, crania, La Meseta Formation, late Eocene. Introduction Penguins (Aves, Sphenisciformes) are the best represented Paleogene Antarc− tic seabirds. This is probably so because of the intrinsic features of their skeletons, dense and heavy bones increase the chance of fossilization, and the presumably gregarious habit, typical of extant species. The oldest penguin record is known from the Paleocene of New Zealand (Slack et al. -
At the Root of the Early Penguin Neck: a Study of the Only Two Cervicodorsal Spines Recovered from the Eocene of Antarctica Piotr Jadwiszczak
RESEARCH/REVIEW ARTICLE At the root of the early penguin neck: a study of the only two cervicodorsal spines recovered from the Eocene of Antarctica Piotr Jadwiszczak Institute of Biology, University of Bialystok, Swierkowa 20B, PL-15-950, Bialystok, Poland Keywords Abstract Antarctic Peninsula; La Meseta Formation; Palaeogene; early Sphenisciformes; The spinal column of early Antarctic penguins is poorly known, mainly due to cervicodorsal vertebrae. the scarcity of articulated vertebrae in the fossil record. One of the most interesting segments of this part of the skeleton is the transitional series located Correspondence at the root of the neck. Here, two such cervicodorsal series, comprising rein- Piotr Jadwiszczak, Institute of Biology, terpreted known material and a new specimen from the Eocene of Seymour University of Bialystok, Swierkowa 20B, Island (Antarctic Peninsula), were investigated and contrasted with those PL-15-950 Bialystok, Poland. of modern penguins and some fossil bones. The new specimen is smaller E-mail: [email protected] than the counterpart elements in recent king penguins, whereas the second series belonged to a large-bodied penguin from the genus Palaeeudyptes. It had been assigned by earlier researchers to P. gunnari (a species of ‘‘giant’’ penguins) and a Bayesian analysis*a Bayes factor approach based on size of an associated tarsometatarsus*strongly supported such an assignment. Morphological and functional studies revealed that mobility within the aforementioned segment probably did not differ substantially between extant and studied fossil penguins. There were, however, intriguing morphological differences between the smaller fossil specimen and the comparative material related to the condition of the lateral excavation in the first cervicodorsal vertebra and the extremely small size of the intervertebral foramen located just prior to the first ‘‘true’’ thoracic vertebra. -
Gilles Cuny, a Late Triassic Cynodont from Holwell Quarries
ORYCTOS, Vol. 5 : 69 - 73, Décembre 2004 A LATE TRIASSIC CYNODONT FROM HOLWELL QUARRIES (SOMERSET, ENGLAND) Gilles CUNY Geological Museum, University of Copenhagen, Øster Voldgade 5-7, 1350 Copenhagen K, Denmark Abstract : The presence of the dromatheriid cynodont Pseudotriconodon wildi is reported from the Rhaetian of Great Britain in the fissure deposits at Holwell Quarries. The British Rhaetic cynodont fauna, although consisting only of one dromatheriid tooth, one tooth of Tricuspes, and one tritylodontid fragmentary jaw, is similar to that found in the Germanic Realm. It appears to be the remnant of a fauna that covered all of Western Europe before the fragmentation of its habitat due to the Rhaetian transgression. Keywords : Cynodontia, Triassic, Rhaetian, Great Britain, Europe. Un cynodonte dans le Trias supérieur des carrières d’Holwell (Somerset, Angleterre) Résumé : La présence du cynodonte Pseudotriconodon wildi est signalée dans des remplissages de fissures rhétiens des carrières d’Holwell, en Angleterre. La faune de cynodontes du Rhétien d’Angleterre, bien que connue unique- ment d’après une dent de Dromatheriidés, une dent de Tricuspes, et un fragment de mâchoire de Tritylodontidés, est similaire à celle trouvée à la même époque en Europe continentale dans le bassin germanique. Il s’agit probablement des restes d’une faune plus ancienne qui couvrait l’ensemble de l’Europe avant que celle-ci ne soit fragmentée en plusieurs îles par la transgression rhétienne. Mots clés : Cynodontia, Trias, Rhétien, Europe, Grande-Bretagne. INTRODUCTION Moore (1859, 1861, 1862, 1864, 1867) was the first to study these fissures, set in quarries that are now The fissure fillings at Holwell quarries have closed. -
Supplementary Information
Supplementary Information Substitution Rate Variation in a Robust Procellariiform Seabird Phylogeny is not Solely Explained by Body Mass, Flight Efficiency, Population Size or Life History Traits Andrea Estandía, R. Terry Chesser, Helen F. James, Max A. Levy, Joan Ferrer Obiol, Vincent Bretagnolle, Jacob González-Solís, Andreanna J. Welch This pdf file includes: Supplementary Information Text Figures S1-S7 SUPPLEMENTARY INFORMATION TEXT Fossil calibrations The fossil record of Procellariiformes is sparse when compared with other bird orders, especially its sister order Sphenisciformes (Ksepka & Clarke 2010, Olson 1985c). There are, however, some fossil Procellariiformes that are both robustly dated and identified and therefore suitable for fossil calibrations. Our justification of these fossils, below, follows best practices described by Parham et al. (2012) where possible. For all calibration points only a minimum age was set with no upper constraint specified, except for the root of the tree. 1. Node between Sphenisciformes/Procellariiformes Minimum age: 60.5 Ma Maximum age: 61.5 Ma Taxon and specimen: Waimanu manneringi (Slack et al. 2006); CM zfa35 (Canterbury Museum, Christchurch, New Zealand), holotype comprising thoracic vertebrae, caudal vertebrae, pelvis, femur, tibiotarsus, and tarsometatarsus. Locality: Basal Waipara Greensand, Waipara River, New Zealand. Phylogenetic justification: Waimanu has been resolved as the basal penguin taxon using morphological data (Slack et al. 2006), as well as combined morphological and molecular datasets (Ksepka et al. 2006, Clarke et al. 2007). Morphological and molecular phylogenies agree on the monophyly of Sphenisciformes and Procellariiformes (Livezey & Zusi 2007, Prum et al. 2015). Waimanu manneringi was previously used by Prum et al. (2015) to calibrate Sphenisiciformes, and see Ksepka & Clarke (2015) for a review of the utility of this fossil as a robust calibration point. -
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Contents lists available at ScienceDirect Palaeogeography, Palaeoclimatology, Palaeoecology journal homepage: www.elsevier.com/locate/palaeo Pangea B and the Late Paleozoic Ice Age ⁎ D.V. Kenta,b, ,G.Muttonic a Earth and Planetary Sciences, Rutgers University, Piscataway, NJ 08854, USA b Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY 10964, USA c Dipartimento di Scienze della Terra 'Ardito Desio', Università degli Studi di Milano, via Mangiagalli 34, I-20133 Milan, Italy ARTICLE INFO ABSTRACT Editor: Thomas Algeo The Late Paleozoic Ice Age (LPIA) was the penultimate major glaciation of the Phanerozoic. Published compi- Keywords: lations indicate it occurred in two main phases, one centered in the Late Carboniferous (~315 Ma) and the other Late Paleozoic Ice Age in the Early Permian (~295 Ma), before waning over the rest of the Early Permian and into the Middle Permian Pangea A (~290 Ma to 275 Ma), and culminating with the final demise of Alpine-style ice sheets in eastern Australia in the Pangea B Late Permian (~260 to 255 Ma). Recent global climate modeling has drawn attention to silicate weathering CO2 Greater Variscan orogen consumption of an initially high Greater Variscan edifice residing within a static Pangea A configuration as the Equatorial humid belt leading cause of reduction of atmospheric CO2 concentrations below glaciation thresholds. Here we show that Silicate weathering CO2 consumption the best available and least-biased paleomagnetic reference poles place the collision between Laurasia and Organic carbon burial Gondwana that produced the Greater Variscan orogen in a more dynamic position within a Pangea B config- uration that had about 30% more continental area in the prime equatorial humid belt for weathering and which drifted northward into the tropical arid belt as it transformed to Pangea A by the Late Permian.