Ither Fossils? Studying Morphological Character Evolution in the Age of Molecular Sequences Elizabeth J
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Paleontology of the Neoproterozoic Uinta Mountain Group Robin M. Nagy* and Susannah M. Porter* ABSTRACT Sedimentary rocks of the Uinta Mountain Group (northeastern Utah) preserve fossils deposited in a marine setting during middle Neoproterozoic time. Although well preserved, species diversity is much lower than many other midddle Neoproterozoic siliciclastic deposits. Microfossil assemblages are mostly limited to Leiosphaeridia sp., Bavlinella faveolata, and fi laments. Diverse ornamented acritarchs, vase- shaped microfossils, and the macroscopic compression fossil Chuaria circularis, also occur, but are much more rare. Although the Uinta Mountain Group does not preserve as wide a range of facies as other middle Neoproterozoic units – the unit is carbonate-free – it is unlikely that preservation alone can account for its relatively limited fossil diversity. Rather, the Uinta Mountain Group likely records deposition in an environment that was inimical to most eukaryotes. INTRODUCTION own (see table 2). We find that although the UMG is fossiliferous throughout its stratigraphic and The Uinta Mountain Group (UMG) is one geographic range, (appendix A) fossil assemblages of several western North American successions are, for the most part, taxonomically depauperate, that provide a glimpse of middle Neoproterozoic limited to just one or a few morphologically simple life (Link and others, 1993). Other successions species. This probably reflects, at least in part, the from this region have yielded important insight limited range of taphonomic windows preserved into this critical interval, including the earliest in the UMG, but also suggests that much of the evidence for eukaryotic biomineralization UMG was deposited in an environment inimical to (Horodyski and Mankiewicz, 1990; Porter and high species diversity. -
Tayside, Central and Fife Tayside, Central and Fife
Detail of the Lower Devonian jawless, armoured fish Cephalaspis from Balruddery Den. © Perth Museum & Art Gallery, Perth & Kinross Council Review of Fossil Collections in Scotland Tayside, Central and Fife Tayside, Central and Fife Stirling Smith Art Gallery and Museum Perth Museum and Art Gallery (Culture Perth and Kinross) The McManus: Dundee’s Art Gallery and Museum (Leisure and Culture Dundee) Broughty Castle (Leisure and Culture Dundee) D’Arcy Thompson Zoology Museum and University Herbarium (University of Dundee Museum Collections) Montrose Museum (Angus Alive) Museums of the University of St Andrews Fife Collections Centre (Fife Cultural Trust) St Andrews Museum (Fife Cultural Trust) Kirkcaldy Galleries (Fife Cultural Trust) Falkirk Collections Centre (Falkirk Community Trust) 1 Stirling Smith Art Gallery and Museum Collection type: Independent Accreditation: 2016 Dumbarton Road, Stirling, FK8 2KR Contact: [email protected] Location of collections The Smith Art Gallery and Museum, formerly known as the Smith Institute, was established at the bequest of artist Thomas Stuart Smith (1815-1869) on land supplied by the Burgh of Stirling. The Institute opened in 1874. Fossils are housed onsite in one of several storerooms. Size of collections 700 fossils. Onsite records The CMS has recently been updated to Adlib (Axiel Collection); all fossils have a basic entry with additional details on MDA cards. Collection highlights 1. Fossils linked to Robert Kidston (1852-1924). 2. Silurian graptolite fossils linked to Professor Henry Alleyne Nicholson (1844-1899). 3. Dura Den fossils linked to Reverend John Anderson (1796-1864). Published information Traquair, R.H. (1900). XXXII.—Report on Fossil Fishes collected by the Geological Survey of Scotland in the Silurian Rocks of the South of Scotland. -
An Analysis of Fossil Identification Guides to Improve Data Reporting in Citizen Science Programs
Palaeontologia Electronica palaeo-electronica.org An analysis of fossil identification guides to improve data reporting in citizen science programs Dava K. Butler, Donald A. Esker, Kristopher L. Juntunen, and Daniel R. Lawver ABSTRACT An increasing number of organizations use untrained volunteers to gather scien- tific data. This citizen science movement builds enthusiasm for science by engaging the public, as well as providing a way to gather large amounts of data at little or no expense. The challenge of citizen science is obtaining accurate information from par- ticipants. Many citizen science programs encourage participants to use visual identification guides to ensure they provide correct data. Identifying an image style that increases correct identifications helps not only the citizen science movement but also scientific instruction in general. This study tests three image-based identification guides for iden- tifying late Hemphillian (5–4.5 m.y.a.) fossils from Polk County, Florida. Each guide has identical layout and text, differing only in image style: color photos, grayscale photos, or illustrations. Untrained participants each use one guide to identify fossils. Geology and paleontology professionals also identify fossils for comparison. Comparing results reveals that color photographic images produce results most similar to data from pro- fessionals. In addition, participants provide data on their years of education, previous experi- ence finding fossils, and enthusiasm about finding fossils. Analysis of this information reveals that participants with higher education and/or previous experience finding fos- sils produce data most similar to that from professionals. Paradoxically, participants with higher enthusiasm produce data less similar to that from professionals, while mod- erate interest levels correlated with greater similarity. -
Mesa Verde National Park Paleontological Resource Inventory (Non-Sensitive Version)
National Park Service U.S. Department of the Interior Natural Resource Stewardship and Science Mesa Verde National Park Paleontological Resource Inventory (Non-Sensitive Version) Natural Resource Report NPS/MEVE/NRR—2017/1550 ON THE COVER An undescribed chimaera (ratfish) egg capsule of the ichnogenus Chimaerotheca found in the Cliff House Sandstone of Mesa Verde National Park during the work that led to the production of this report. Photograph by: G. William M. Harrison/NPS Photo (Geoscientists-in-the-Parks Intern) Mesa Verde National Park Paleontological Resources Inventory (Non-Sensitive Version) Natural Resource Report NPS/MEVE/NRR—2017/1550 G. William M. Harrison,1 Justin S. Tweet,2 Vincent L. Santucci,3 and George L. San Miguel4 1National Park Service Geoscientists-in-the-Park Program 2788 Ault Park Avenue Cincinnati, Ohio 45208 2National Park Service 9149 79th St. S. Cottage Grove, Minnesota 55016 3National Park Service Geologic Resources Division 1849 “C” Street, NW Washington, D.C. 20240 4National Park Service Mesa Verde National Park PO Box 8 Mesa Verde CO 81330 November 2017 U.S. Department of the Interior National Park Service Natural Resource Stewardship and Science Fort Collins, Colorado The National Park Service, Natural Resource Stewardship and Science office in Fort Collins, Colorado, publishes a range of reports that address natural resource topics. These reports are of interest and applicability to a broad audience in the National Park Service and others in natural resource management, including scientists, conservation and environmental constituencies, and the public. The Natural Resource Report Series is used to disseminate comprehensive information and analysis about natural resources and related topics concerning lands managed by the National Park Service. -
Volume 26C-Nogrid
Priscum Volume 26 | Issue 1 May 2021 The Newsletter of the Paleontological Society Inside this issue Diversity, Equity, and Inclusion Matter in Diversity, Equity, & Inclusion matter in Paleontology Paleontology PS Development Developments Building an inclusive and equitable Where are we now? PaleoConnect Paleontological Society (see Section 12 of the Member Code of Conduct for definitions) is Since the Paleontological Society (PS) was Journal Corner essential to realizing our core purpose — founded in 1908, its membership has been advancing the field of paleontology (see Article dominated by white men from the United PS-AGI Summer 2020 Interns II of the Articles of Incorporation). However, like States. Racial and ethnic diversity in the PS many other scientific societies, ours has remain extremely low. More than 88% of Tribute to William Clemens, Jr. historically only fostered a sense of belonging respondents to PS membership surveys Educational Materials for a subset of individuals. conducted in 2013 and 2019 self-identified as White (Stigall, 2013; unpublished data, 2019). PS Ethics Committee Report Consider your outreach experiences. Imagine These surveys revealed that, unlike the visiting a series of first grade classrooms — proportion of women, which has increased in Research and Grant Awardees overwhelmingly, the children are fascinated by younger age cohorts (Stigall, 2013), racial and PS Annual meeting at GSA Connects dinosaur bones, scale trees, and trilobites — ethnic diversity varied little among age groups, 2021 regardless of their identities. Now, reflect on suggesting that substantial barriers to the your experiences in paleontological settings as inclusion of most racial and ethnic groups have Upcoming Opportunities an adult; do they include as much diversity as persisted across generations of PS members. -
Carboniferous-Permian Transition in Socorro County, New Mexico
Lucas, S.G., DiMichele, W.A. and Krainer, K., eds., 2017, Carboniferous-Permian transition in Socorro County, New Mexico. New Mexico Museum of Natural History and Science Bulletin 77. 1 CARBONIFEROUS-PERMIAN TRANSITION IN SOCORRO COUNTY, NEW MEXICO, USA: AN OVERVIEW SPENCER G. LUCAS1, KARL KRAINER2, BRUCE D. ALLEN3 and WILLIAM A. DIMICHELE4 1New Mexico Museum of Natural History, 1801 Mountain Road NW, Albuquerque, New Mexico M 87104; email: [email protected]; 2Institute of Geology, University of Innsbruck, Innrain 52, A-6020 Innsbruck, Austria ; 3New Mexico Bureau of Geology & Mineral Resources, 801 Leroy Place, Socorro, New Mexico 87801; 4Department of Paleobiology, NMNH Smithsonian Institution, Washington, DC 20560 Abstract— This volume documents the results of 20+ years of field, laboratory and museum research on the Pennsylvanian-Permian rocks and fossils of Socorro County, New Mexico. The articles in this volume report studies of the Pennsylvanian-Permian strata east of Socorro (Joyita Hills-Cerros de Amado-Carthage area), in the Los Pinos Mountains (Sepultura Canyon area), in the Little San Pascual Mountains and at Bell Hill in the Southern San Mateo Mountains. Lithostratigraphy, sedimentary petrography, microfacies analysis and sedimentological interpretation as well as diverse paleontological studies (fossil plants, calcareous microfossils, conodonts, fossil insects, tetrapod footprints, coprolites and fossil fishes) are presented. The entire Pennsylvanian-Permian stratigraphic section in Socorro County is about 2 km thick. The Pennsylvanian strata are a complex succession of sedimentary rocks of marine and nonmarine origin deposited during the Middle-Late Pennsylvanian. These are synorogenic deposits of the ancestral Rocky Mountain (ARM) orogeny and associated marine carbonates of shallow seaways along the western periphery of equatorial Pangea. -
Stromatolites: Biogenicity, Biosignatures, and Bioconfusion
Invited Paper Stromatolites: Biogenicity, Biosignatures, and Bioconfusion Stanley M. Awramikl*a d Kathleen Greyb a Departmentof Geological Sciences, Preston Cloud Research Laboratory, University of California, Santa Barbara, CA 93 1 06, USA b Geological Survey of Western Australia, Department of Industry and Resources, 100 Plain Street, East Perth, WA 6004, Australia ABSTRACT Stromatolites represent a multifarious system ofnested, physically, chemically, and biologically influenced components that range in scale from microscopic to macroscopic. These components can include microorganisms, organic compounds of microorganisms, sediment grains, precipitated sediment, sedimentary textures (fabrics), microstructure, laminae, domes, columns, branched columns, and cones. Millimeter to meter scale edifices (stromatolites) are the result. Stromatolites once played a significant role in establishing life's presence on the early Earth, but now a shift away from reliance on stromatolites is occurring. There is a perception that Archean stromatolite-like structures have low reliability to signal life. This is likely due to (1) no unified theory on stromatolite morphogenesis, (2) no valid or appropriate modern analog to use in the interpretation ofArchean stromatolites, and (3) disagreement on how to defme the word stromatolite. No single feature or line ofevidence has yet been found that can unequivocally indicate a biogenic nature for a stromatolite. However, a range of features and their combinations that are well documented for the vast majority offossil stromatolites and are found in some living stromatolites, are difficult, ifnot impossible, to account for by inorganic processes. Morphology remains a valid criterion to indicate biogenicity. Keywords: stromatolites, biogenicity, abiogenic, Archean 1. INTRODUCTION As the sedimentary layers of Earth's history are peeled away and Archean rocks (older than >2.5 Ga) are exposed, the record of sedimentary rocks becomes sparse and the evidence for life becomes meager and difficult to read. -
Newsletter Number 58
The Palaeontology Newsletter Contents 58 Association Business 2 News 8 Association Meetings 10 Meeting Reports 14 Mysterious Fossils 25 From our correspondents Inferring Developmental Mode 26 Foiling vertebrate inversion 32 PalaeoBioSuperstar 40 Palaeo-math 101: Regression 4 44 Obituary: Ehrhard Voigt 54 Progressive Palaeontology 2005 57 Future meetings of other bodies 58 Book Reviews 72 Palaeontology vol 48 parts 1 & 2 92–93 Discounts for PalAss members 94 Reminder: The deadline for copy for Issue no 59 is 20th May 2005 On the Web: <http://www.palass.org/> Newsletter 58 2 Newsletter 58 3 Association Business the compilation of fossil collections, and their care and conservation, to published studies in recognised journals. Nominations should comprise a short statement (up to one page of A4) outlining the candidate’s principal achievements. Members putting forward candidates should Nominations for Council also be prepared, if requested, to write an illustrated profile in support of their nominee. The deadline for nominations is 1st September 2005. The award comprises a cash prize plus a At the AGM in December 2005, the following vacancies will occur on Council: framed scroll, and is usually presented at the Annual meeting. Vice-President Sylvester-Bradley Award Newsletter Editor three handling editors Awards are made to assist palaeontological research (travel, visits to museums, fieldwork etc.), one Ordinary member with each award having a maximum value of £1,000. Preference is given to applications for a single purpose (rather than top-ups of other grant applications) and no definite age limit is Nominations are now invited for these posts. Please note that each candidate must be proposed applied, although some preference may be given to younger applicants or those at the start by at least two members of the Association and that any individual may not propose more than of their careers. -
Chapter 2. History of Paleontological Work at Grand Canyon National Park
Chapter 2. History of Paleontological Work at Grand Canyon National Park Up and Down the Long Federal and NGO Trails of Paleontology in Grand Canyon National Park, 1858–2019 By Earle E. Spamer1 1Academy of Natural Sciences Research Associate Philadelphia, Pennsylvania Introduction The Grand Canyon! Anywhere in the world the name rouses recognition. Monumentally impossible to describe (or so have said thousands of writers who then effused their own descriptions), it has been a lure to geologists since 1858. From the start, the rocks were read for the clues of their relative ages. It has been the draw of government agencies and non-government organizations (NGO) alike. The national park is a century old now; the canyon six to 70-some million years (depending upon with whom you argue, and about which parts of the canyon you consider); and fossils in the canyon have awaited the hammer and scanning electron microscope for even more than a billion years. So, to avoid the traps of superlatives and the gulping periods of time, this is a fast trot through “the best of” Grand Canyon paleontology, refreshed with bits of human history, with a few pauses on peculiar details—a 100th birthday present to the national park. Here, beginning with the first Grand Canyon field trip in 1858, is an accounting of how the first explorers, and scientists and educators over the years, have fashioned our understanding and encouraged our participation in the story of ancient life presented in Grand Canyon’s strata and secluded deposits. With this long look backward, we also may gain an appreciation for how paleontologists, federal administrators, and NGO champions built up the scientific and educational programs that modern resource managers receive as a legacy. -
Changing the Picture of Earth's Earliest Fossils (3.5–1.9
Changing the picture of Earth’s earliest fossils (3.5–1.9 SPECIAL FEATURE Ga) with new approaches and new discoveries Martin D. Brasiera,1, Jonathan Antcliffeb,c, Martin Saundersd, and David Waceyd,e,2,3 aDepartment of Earth Sciences, University of Oxford, Oxford OX1 3AN, United Kingdom; bDepartment of Zoology, University of Oxford, Oxford OX1 3PS, United Kingdom; cSchool of Earth Sciences, University of Bristol, Bristol BS8 1RJ, United Kingdom; dCentre for Microscopy Characterisation and Analysis, The University of Western Australia, Crawley, WA 6009, Australia; and eAustralian Research Council Centre of Excellence for Core to Crust Fluid Systems, The University of Western Australia, Crawley, WA 6009, Australia Edited by David Jablonski, The University of Chicago, Chicago, IL, and approved August 20, 2014 (received for review March 27, 2014) New analytical approaches and discoveries are demanding fresh of these debates. Four major areas of advancement are now thinking about the early fossil record. The 1.88-Ga Gunflint chert changing our understanding: (i) prokaryotic phylogeny and cell provides an important benchmark for the analysis of early fossil diversity, (ii) diverse bacterial environments (including extrem- preservation. High-resolution analysis of Gunflintia shows that ophile habitats) traced from the present and back into deep time, microtaphonomy can help to resolve long-standing paleobiologi- (iii) new analytical techniques, and (iv) testing of criteria for cal questions. Novel 3D nanoscale reconstructions of the most an- recognizing ancient fossil bacteria. Below, we use three case cient complex fossil Eosphaera reveal features hitherto unmatched studies (the 1.88-Ga Gunflint chert, the 3.46-Ga Apex chert, and in any crown-group microbe. -
Criteria for Distinguishing Microbial Mats and Earths
CRITERIA FOR DISTINGUISHING MICROBIAL MATS AND EARTHS GREGORY J. RETALLACK Department of Geological Sciences, University of Oregon, 1275 East 13th Avenue, Eugene, Oregon 97302, USA e-mail: [email protected] ABSTRACT: Microbial earths are communities of microscopic organisms living in well-drained soil. Unlike aquatic microbial mats and stromatolites, microbial earths are sheltered from ultraviolet radiation, desiccation, and other surficial hazards within soil cracks and grain interstices. Currently, such ecosystems are best known in small areas of unusually cold, hot, or saline soils unfavorable to multicellular plants and animals. During the Precambrian, microbial earths may have been more widespread, but few examples have been reported. This review outlines a variety of features of modern microbial earths that can be used to distinguish them from aquatic microbial mats and stromatolites in the fossil record. Microbial earths have vertically oriented organisms intimately admixed with minerals of the soil, whereas microbial mats are laminated and detachable from their mineral substrate as flakes, skeins, and rollups. Microbial earths have irregular relief, healed desiccation cracks, and pressure ridges, whereas microbial mats have flexuous, striated domes, and tufts. Microbial earths form deep soil profiles with downward variations in oxidation, clay abundance, and replacive nodular subsurface horizons, whereas microbial mats form as caps to unweathered, chemically reduced sedimentary layers. Microbial earths develop increasingly differentiated soil profiles through time, whereas microbial mats build upward in laminar to domed increments. Microbial earths are found in nonmarine sedimentary facies, whereas microbial mats form in lacustrine, floodplain, and marine sedimentary facies. Microbial mats and stromatolites are known back to the oldest suitably preserved sedimentary rocks in the 3458 Ma Apex Chert and 3430 Ma Strelley Pool Formation (respectively) of the Pilbara region of Western Australia. -
Ichnotaxonomic Assessment of Mazon Creek Area Trace Fossils, Illinois, USA
Ichnotaxonomic Assessment of Mazon Creek Area Trace Fossils, Illinois, USA by David J. LoBue B.S. Geology B.A. Religious Studies B.A. Political Science Arizona State University 2006 Submitted to the Department of Geology and the Faculty of the Graduate School of The University of Kansas in partial fulfillment of the requirements for the degree of Master of Science 2010 _________________________ Stephen T. Hasiotis, Chair _________________________ Paul Selden _________________________ Anthony Walton Date Defended: ____________ The Thesis Committee for David J. LoBue certifies that this is the approved version of the following thesis: Ichnotaxonomic Assessment of Mazon Creek Area Trace Fossils, Illinois, USA __________________________ Stephen T. Hasiotis, Chairperson Date Approved: _____________ ii ABSTRACT David J. LoBue, M.S. Department of Geology, July 2010 University of Kansas The Francis Creek Shale Member (FCSM) of the Mid-Pennsylvanian Carbondale Formation along Mazon Creek in northern Illinois is known for soft-bodied organisms preserved within siderite concretions. Trace fossils, though less well known, also occur in concretions. Several hundred trace-fossil-bearing concretions were examined from collections at The Field Museum, Chicago, and The University of Kansas Natural History Museum, Lawrence. Identification was based on accepted diagnostic criteria and comparison with like specimens. Described were 24 ichnogenera and 28 ichnospecies, including a new ichnospecies of Pennatulites and a new ichnogenera of coprolite— Funiculichnus spiralis, unnamed trace fossils including a bivalve-locomotion trail, spiral and amorphous coprolites, and two possible galls, and several deformation structures and body fossils misidentified as trace fossils. Trace-fossil assemblages indicate a Skolithos– Cruziana ichnofacies transition from shallow, high-energy to deeper, lower-energy nearshore marine environments, which is consistent with previous interpretations that the FCSM was deposited in a nearshore, deltaic environment.