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1

Kinyua, A. M., T. Plummer, N. Shimizu, W. Melson, and R. Potts. "Provenance of Kanjera Fossils by X-Ray Fluorescence and Ion Microprobe Analyses." Advances in X-ray Analysis 35, B (1991): 1165–73. http://dx.doi.org/10.1154/s0376030800013458.

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AbstractXRF and Ion mfcroprobe analyses of fossils of known and uncertain provenance from the Lower-Middle Pleistocene locality of Kanjera. Kenya, are reported. The goal of this study was to develop a nondestructive technique of provenancixig fossils, which could be applied to the Kanjera sample. The fossils of known provenance were collected in the excavations of the 1987 Smithsonian Expedition. Three fossils of uncertain provenance, two specimens of Theropithecus oswaldi and a hominid fossil, were analyzed as test cases.Both qualitative and quantitative XRF analyses of Kanjera fossils were c
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2

Harms, Danilo, and Jason A. Dunlop. "The fossil history of pseudoscorpions (Arachnida: Pseudoscorpiones)." Fossil Record 20, no. 2 (2017): 215–38. http://dx.doi.org/10.5194/fr-20-215-2017.

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Abstract. Pseudoscorpions, given their resemblance to scorpions, have attracted human attention since the time of Aristotle, although they are much smaller and lack the sting and elongated tail. These arachnids have a long evolutionary history but their origins and phylogenetic affinities are still being debated. Here, we summarise their fossil record based on a comprehensive review of the literature and data contained in other sources. Pseudoscorpions are one of the oldest colonisers of the land, with fossils known since the Middle Devonian (ca. 390 Ma). The only arachnid orders with an older
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3

Heikkilä, Maria, Joël Minet, Andreas Zwick, Anna Hundsdoerfer, Rodolphe Rougerie, and Ian J. Kitching. "Critical re-examination of known purported fossil Bombycoidea (Lepidoptera)." PeerJ 11 (November 10, 2023): e16049. http://dx.doi.org/10.7717/peerj.16049.

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We critically re-examine 17 records of fossils currently assigned to the lepidopteran superfamily Bombycoidea, which includes the silk moths, emperor moths and hawk moths. These records include subfossils, compression and impression fossils, permineralizations and ichnofossils. We assess whether observable morphological features warrant their confident assignment to the superfamily. None of the examined fossils displays characters that allow unequivocal identification as Sphingidae, but three fossils and a subfossil (Mioclanis shanwangiana Zhang, Sun and Zhang, 1994, two fossil larvae, and a p
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4

Maples, Christopher G., and Ronald R. West. "Introduction to Trace Fossils and Dedication to Robert W. Frey." Short Courses in Paleontology 5 (1992): 1–14. http://dx.doi.org/10.1017/s2475263000002269.

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Over the years, we've participated in several different workshops and short courses on trace fossils. So why this one? Our intention in bringing together these papers for the Trace Fossil Short Course is to give an overview of how trace fossils can be used in paleontology. Historically, trace fossil research has centered on paleoenvironmental and depositional reconstructions—areas where trace fossils have much to tell. Indeed, the use of trace fossils by sedimentologists has flourished and is experiencing another burst of activity through the use of ichnofabrics in sequence stratigraphic studi
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5

Lockley, Martin G. "Tracks and Traces: New Perspectives on Dinosaurian Behavior, Ecology, and Biogeography." Short Courses in Paleontology 2 (1989): 134–45. http://dx.doi.org/10.1017/s2475263000000921.

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Conventional paleontological wisdom holds that there are two major categories of fossil evidence: body fossils (skeletal remains), and trace fossils (including tracks and traces). Ichnology, the study of trace fossils, requires a parallel taxonomy of scientific names (parataxonomy or ichnotaxonomy), like the form taxa of fossil plant remains. This ichnotaxonomy describes a large variety of traces attributable to invertebrates (Hantzschel, 1975) and vertebrates (Haubold, 1984; Leonardi, 1984; Leonardi et al., 1986).
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6

Unger, Shem, and Mark Rollins. "Find a Fossil and “Choose your own Adventure”." International Journal of Educational Innovation and Research 3, no. 1 (2024): 86–96. http://dx.doi.org/10.31949/ijeir.v3i1.7253.

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Science education university curriculum should foster transformative methods of teaching and learning for science majors, including science communication. Pedagogical methods for increasing student awareness of paleontological fossils present challenges as fossils are often presented as preserved remains with little visualizations or reconstructions of fossils. As part of increasing scientific literacy and increasing confidence in professional development skills, student presentations can provide an avenue for promoting these necessary skills for biology majors. This study reports on a short m
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7

Harbowo, Danni Gathot, Aswan, Siti Khodijah Chaerun, Widi Astuti, and Yahdi Zaim. "Exploring Pliocene Vegetation Variability through Wood Fossil Analysis from Jasinga, Indonesia." Tropical Natural History 24 (May 26, 2024): 31–47. https://doi.org/10.58837/tnh.24.1.258579.

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Residents of Jasinga, West Java, consistently reported the presence of an abundance of wood fossils. We examined geological settings and wood fossils to investigate the paleovegetation types in the region. This research aims to map the distribution of wood fossils and interpret the paleoenvironment based on paleontological evidence. Lithostratigraphic measurements were performed, followed by a description of wood fossil anatomy in micro-thin section observations, isolation of palynological fossils from the host rock through chemical preparation techniques, and geochemical analysis using X-ray
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8

Walker, S. E. "Criteria for recognizing marine hermit crabs in the fossil record using gastropod shells." Journal of Paleontology 66, no. 4 (1992): 535–58. http://dx.doi.org/10.1017/s0022336000024410.

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Hermit crabs have left a rich fossil legacy of epi- and endobionts that bored or encrusted hermit crab-inhabited shells in specific ways. Much of this rich taphonomic record, dating from the middle Jurassic, has been overlooked. Biological criteria to recognize hermitted shells in the fossil record fall within two major categories: 1) massive encrustations, such as encrusting bryozoans; and 2) subtle, thin encrustations, borings, or etchings that surround or penetrate the aperture of the shell. Massive encrustations are localized in occurrence, whereas subtle trace fossils and body fossils are
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9

Winarto, Johan Budi, Wilda Aini Nurlathifah, Agustina Djafar, Andy Dharmedy Sipayung, Rahajeng Ayu Permana Sari, and Halmi Insani. "The Surficial Basin Sediment Investigation and Its Concerned Vertebrate Fossils in Sirtwo Island, Western Part of Saguling Dam, West Java, Indonesia." Indonesian Journal of Earth Sciences 2, no. 1 (2022): 1–15. http://dx.doi.org/10.52562/injoes.v2i1.288.

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In October 2021, the depreciation of the water level of dam Saguling revealed the surficial sediment where was dam up Citarum river. Sirtwo island and surroundings are part of the body sediment were arisen which is part of the sedimentary facies in the western of Bandung Lake ancient. Several vertebrate fossils were found on Sirtwo island and Pasir Benteng island. The investigation of vertebrate fossils was carried out to understand where are deposited in Bandung lake. The geological survey lead to the recognition of types of lake deposits and was divided into 5 block observations i.e., Block
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10

Sullivan, Colleen A., and Sarah W. Keenan. "Experimental dissolution of fossil bone under variable pH conditions." PLOS ONE 17, no. 10 (2022): e0274084. http://dx.doi.org/10.1371/journal.pone.0274084.

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Fossils exposed at the surface are an integral component of the paleontologic record and provide an archive of past life. However, it is widely known that fossils are not stable indefinitely upon exposure to surface conditions such as physical, chemical, and biological processes, and this last phase of taphonomy is poorly understood. Studies regarding the longevity of fossils subject to weathering, such as acidic precipitation, are absent in the literature. The goal of this study was to experimentally determine vertebrate fossil dissolution rates under variable pH conditions in a controlled la
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11

Puttick, Mark N. "Partially incorrect fossil data augment analyses of discrete trait evolution in living species." Biology Letters 12, no. 8 (2016): 20160392. http://dx.doi.org/10.1098/rsbl.2016.0392.

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Ancestral state reconstruction of discrete character traits is often vital when attempting to understand the origins and homology of traits in living species. The addition of fossils has been shown to alter our understanding of trait evolution in extant taxa, but researchers may avoid using fossils alongside extant species if only few are known, or if the designation of the trait of interest is uncertain. Here, I investigate the impacts of fossils and incorrectly coded fossils in the ancestral state reconstruction of discrete morphological characters under a likelihood model. Under simulated p
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12

Hannibal, J. T., and S. G. Lucas. "Trace fossils in two North American museums: the Cleveland Museum of Natural History and the New Mexico Museum of Natural History and Science." Geological Curator 8, no. 5 (2006): 261–68. http://dx.doi.org/10.55468/gc371.

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Ohio and New Mexico are rich in trace fossils (ichnofossils), and both states have longstanding traditions of ichnological research. The Cleveland Museum of Natural History, founded in 1920, has a substantial collection of ichnofossils that includes figured specimens from Ohio, West Virginia and New Jersey. Donations and intensive collecting of trace fossils followed the founding of the New Mexico Museum of Natural History and Science in 1986. This has resulted in North America's largest collection of Permian trace fossils, as well as important collections of trace fossils from several other g
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13

Buffetaut, Eric. "Minor Title Change: Fossils Becomes Fossil Studies." Fossil Studies 1, no. 1 (2023): 76. http://dx.doi.org/10.3390/fossils1010008.

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14

Sun, Mengyu, Yuanxin Zhong, Zhengwang Qin, Zheng Liu, Chunming Gao, and Yanli Gong. "Research on 3D Reconstruction of Paleontological Fossils Based on Photoacoustic Microscopy." Journal of Physics: Conference Series 2822, no. 1 (2024): 012095. http://dx.doi.org/10.1088/1742-6596/2822/1/012095.

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Abstract The focus on three-dimensional morphological analysis of endogenous trace fossils has emerged as a prominent aspect in the study of palaeobiological fossils. Photoacoustic imaging technology, renowned for its deep penetration, high resolution and non-destructiveness, holds considerable promise in exploring fossil morphology. In this work, a solid-coupling-based photoacoustic microscopic imaging system was developed, leveraging this technology to investigate small-scale physical fossils. The proposed system enabled layered imaging of various fossil specimens, achieving a lateral resolu
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15

HEIKKILÄ, MARIA, THOMAS J. SIMONSEN, and M. ALMA SOLIS. "Reassessment of known fossil Pyraloidea (Lepidoptera) with descriptions of the oldest fossil pyraloid and a crambid larva in Baltic amber." Zootaxa 4483, no. 1 (2018): 101. http://dx.doi.org/10.11646/zootaxa.4483.1.4.

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The identifications of known fossils currently placed in the lepidopteran superfamily Pyraloidea are critically re-examined. Of the eleven fossils examined, only three are confirmed to show morphological characters supporting placement in the superfamily. These fossils include a crambid larva in Baltic Amber, Baltianania yantarnia, Solis gen. n. et sp. n. and the oldest known fossil pyraloid, Eopyralis morsae Simonsen, gen. n. et sp. n. The third fossil, Glendotricha olgae Kusnezov, 1941, displays apomorphic characters for Pyraloidea, but is shown to be an inclusion in copal, not Baltic amber
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16

Sappenfield, Aaron, Mary L. Droser, and James G. Gehling. "Problematica, trace fossils, and tubes within the Ediacara Member (South Australia): redefining the ediacaran trace fossil record one tube at a time." Journal of Paleontology 85, no. 2 (2011): 256–65. http://dx.doi.org/10.1666/10-068.1.

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Ediacaran trace fossils are becoming an increasingly less common component of the total Precambrian fossil record as structures previously interpreted as trace fossils are reinterpreted as body fossils by utilizing qualitative criteria. Two morphotypes, Form E and Form F of Glaessner (1969), interpreted as trace fossils from the Ediacara Member of the Rawnsley Quartzite in South Australia are shown here to be body fossils of a single, previously unidentified tubular constructional morphology formally described herein as Somatohelix sinuosus n. gen. n. sp. S. sinuosus is 2-7 mm wide and 3-14 cm
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17

Khosroshahi, Habib G., and T. J. Ponman. "Fossil Galaxy Groups; Scaling Relations, Galaxy Properties and Formation of BCGs." Proceedings of the International Astronomical Union 2, S235 (2006): 214. http://dx.doi.org/10.1017/s174392130600620x.

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AbstractWe study fossil galaxy groups, their hot gas and the galaxy properties. Fossils are more X-ray luminous than non-fossil groups, however, they fall comfortably on the conventional L-T relation of galaxy groups and clusters indicating that their X-ray luminosity and temperature are both boosted, arguably, as a result of their early formation. The central dominant galaxy in fossils have optical luminosity comparable to the brightest cluster galaxies (BCGs), however, the isophotal shapes of the central galaxy in fossils are non-boxy in contrast to the isophotes of majority of the BCGs.
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18

Kidwell, Susan, and J. John Sepkoski. "The Nature of the Fossil Record." Paleontological Society Special Publications 9 (1999): 61–76. http://dx.doi.org/10.1017/s2475262200014015.

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The term “fossil record” is used in two ways: either the totality of fossils preserved in all rocks or the sum of human knowledge of those fossils. In either case, the term carries the connotation also of the geologic context of the fossils–their distribution in time and space and their relationship to the enclosing rock. One of the primary scientific interests in the fossil record is learning about the history of life and the processes of large-scale transformation, or evolution, in the forms, diversities, and biological interactions of life.
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19

Cleal, Christopher J., and Barry A. Thomas. "Naming of parts: the use of fossil-taxa in palaeobotany." Fossil Imprint 77, no. 1 (2021): 166–86. http://dx.doi.org/10.37520/fi.2021.013.

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Fossil plants are extinct plants whose remains (referred to as plant fossils) are found preserved in sedimentary deposits. Plant fossils are classified using fossil-taxa as defined in the International Code of Nomenclature. Fossil-taxa differ conceptually from taxa of living plants in that they often do not refer to whole organisms, but to the remains of one or more parts of the parent organism, in one or more preservational states. There can be complications when two parts of a plant are shown to be connected, or when two preservational states are correlated, and to avoid disrupting the wider
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20

Rathore, Akshaya. "Digital Inventory of Fossils: Dinosaur Fossils National Park Bagh Dhar." International Journal for Research in Applied Science and Engineering Technology 9, no. 12 (2021): 1311–17. http://dx.doi.org/10.22214/ijraset.2021.39528.

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Abstract: Dinosaur Fossils National Park Bagh has huge fossils reserves of late cretaceous period that includes Dinosaurs bones, whole dinosaurs’ nests, dinosaurs’ eggs, tree fossils, shark teeth, ammonites, bivalves, inoceramids, and other marine organisms. With the help of local researchers and forest staff over the period oftime we had collected fossils of many species. Firstly, we inventoried the fossils physically and documented each by maintaining Stock Registers. Digitizing the Stock Registers – to convert each register in excel file which includes all the details regarding that fossil.
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21

Bush, Andrew M., and Gwen M. Daley. "Comparative Paleoecology of Fossils and Fossil Assemblages." Paleontological Society Papers 14 (October 2008): 289–317. http://dx.doi.org/10.1017/s108933260000173x.

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Generating and testing hypotheses is an integral part of any science, and some of the most stimulating paleobiological hypotheses of the past few decades relate to the ecological properties of fossils or fossil assemblages. Here, we outline recent methods for framing paleoecological questions that should facilitate the further quantitative evaluation of paleoecological hypotheses. First, we describe theoretical ecospaces, which are frameworks for classifying the ecologic properties of individuals or species based on multiple characters. We discuss the utility of theoretical ecospace in underst
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22

Shah, S. K., Ashok Kumar, and C. S. Sudan. "Trace Fossils from the Cambrian Sequence of Zanskar (Ladakh Himalaya)." Journal Geological Society of India 51, no. 6 (1998): 777–84. http://dx.doi.org/10.17491/jgsi/1998/510607.

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Abstract Spiti - Zanskar Basin of Himalaya exposes rocks ranging in age from Proterozoic to Early Cenozoic. Cambrian trilobites, brachiopods and trace fossils are known from the Kurgiakh area of the basin. The present paper concerns with Early Cambrian trace fossils reported from the same stratigraphic section in which trilobite body fossils are known. The assemblage of trace fossils include: Chondrites sp., Cruziana sp., Rusophycus sp., Phycodes palmatum, sp., Didymaulichnus sp., Protichnites sp., Monomorphicnus monolinearis, Diplichnites sp. associated with scratch marks indicating trilobite
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23

BOSKOVIC, DANILO S., URIEL L. VIDAL, KEVIN E. NICK, et al. "STRUCTURAL AND PROTEIN PRESERVATION IN FOSSIL WHALE BONES FROM THE PISCO FORMATION (MIDDLE-UPPER MIOCENE), PERU." PALAIOS 36, no. 4 (2021): 155–64. http://dx.doi.org/10.2110/palo.2020.032.

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ABSTRACT Microstructural and biomolecular preservation is reported in fossils as old as the Triassic. Such preservation suggests unusual taphonomic conditions. We collected fragments of fossil whale bone from silty, tuffaceous, and diatomaceous rocks of the middle-upper Miocene portion of the Pisco Formation. The whale fossils within the region are generally well-preserved and mostly articulated, including some specimens with in situ baleen. Due to the depositional setting associated with the preservation of these fossils, they could be expected to be favorable candidates for the preservation
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Kidwell, Susan M., and J. John Sepkoski. "The Nature of the Fossil Record." Paleontological Society Special Publications 11 (2002): 47–62. http://dx.doi.org/10.1017/s2475262200009813.

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The term “fossil record” is used in two ways: to mean either the totality of fossils preserved in all rocks or the sum of human knowledge of those fossils. In both cases, the term carries the connotation also of the geologic context of the fossils—their distribution in time and space and their relationship to the enclosing rock. One of the primary scientific interests of the fossil record is what it can teach us about the history of life and the processes of large-scale transformation, or evolution, in the forms, diversities, and biological interactions of living things.
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25

Near, Thomas J., and Michael J. Sanderson. "Assessing the quality of molecular divergence time estimates by fossil calibrations and fossil–based model selection." Philosophical Transactions of the Royal Society of London. Series B: Biological Sciences 359, no. 1450 (2004): 1477–83. http://dx.doi.org/10.1098/rstb.2004.1523.

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Estimates of species divergence times using DNA sequence data are playing an increasingly important role in studies of evolution, ecology and biogeography. Most work has centred on obtaining appropriate kinds of data and developing optimal estimation procedures, whereas somewhat less attention has focused on the calibration of divergences using fossils. Case studies with multiple fossil calibration points provide important opportunities to examine the divergence time estimation problem in new ways. We discuss two cross–validation procedures that address different aspects of inference in diverg
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Houari, Imane Chmanti. "Development of a "Fossilis" tutorial on the concepts of fossils and fossilization." New Trends and Issues Proceedings on Humanities and Social Sciences 4, no. 1 (2017): 544–50. http://dx.doi.org/10.18844/prosoc.v4i1.2298.

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Cui, Tao. "Preservative Features of the Fossils in Bauxite Deposit of WZD Area, Northern Guizhou, China." Advanced Materials Research 989-994 (July 2014): 1384–87. http://dx.doi.org/10.4028/www.scientific.net/amr.989-994.1384.

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It is hardly to discovery fossil from the bauxite in Wuchuan-Zheng, an-Daozhen (WZD) area, northern Guizhou, China. But the new study suggests, containing a small amount of plant debris from massive bauxite in the lower part of the ledge. Preservative features of fossils in WZD bauxite indicates: metallogenetic materials experienced a transport process; sedimentary environment is reduced; fossils only preserved in the massive bauxite, that fossils in other types of ores were destroyed in the late oxidation modification. Metallogenic environment of bauxite has experienced two kinds of state-red
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Puttick, Mark N., and Gavin H. Thomas. "Fossils and living taxa agree on patterns of body mass evolution: a case study with Afrotheria." Proceedings of the Royal Society B: Biological Sciences 282, no. 1821 (2015): 20152023. http://dx.doi.org/10.1098/rspb.2015.2023.

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Most of life is extinct, so incorporating some fossil evidence into analyses of macroevolution is typically seen as necessary to understand the diversification of life and patterns of morphological evolution. Here we test the effects of inclusion of fossils in a study of the body size evolution of afrotherian mammals, a clade that includes the elephants, sea cows and elephant shrews. We find that the inclusion of fossil tips has little impact on analyses of body mass evolution; from a small ancestral size (approx. 100 g), there is a shift in rate and an increase in mass leading to the larger-b
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HORVÁTH, IDA. "New records of fossil bird bones from the Neogene in Hungary." Zootaxa 5627, no. 2 (2025): 327–42. https://doi.org/10.11646/zootaxa.5627.2.5.

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This paper presents previously unreported fossil bird bones from the Hungarian Neogene. They derive from seven sites as follows: Beremend 26 and 38, Egyházasdengeleg, Hidas and Máriahalom. The Early Miocene is represented by four new fossils from Máriahalom, with taxa and numbers of specimens as follows: Pandion pannonicus [1], Gruidae gen. et sp. indet. [1], Passeriformes sp. indet. [2]. Two fossils derive from one Middle Miocene sites as follows: Hidas (Aves sp. indet.. Two fossils come from Late Miocene sites: Alsótelekes (Aves indet.) and Egyházasdengeleg (Aves sp. indet.). A further 17 fo
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SOHN, JAE-CHEON, CONRAD LABANDEIRA, DONALD DAVIS, and CHARLES MITTER. "An annotated catalog of fossil and subfossil Lepidoptera (Insecta: Holometabola) of the world." Zootaxa 3286, no. 1 (2012): 1. http://dx.doi.org/10.11646/zootaxa.3286.1.1.

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In this catalog, we attempt to assemble all fossil records of Lepidoptera described formally or informally in the worldliterature. A total of 667 records dealing with at least 4,568 specimens have been compiled. They include descriptions of131 fossil genera and 229 fossil species, as well as 72 extant genera and 21 extant species to which some of these fossilssupposedly belong or show superficial similarity. Replacement names of two fossil genera are proposed to avoidhomonymy: Baltopsyche Sohn, gen. nov. for Palaeopsyche Sobczyk and Kobbert, 2009 and Netoxena Sohn, gen. nov. forXena Martins-Ne
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Minicucci, Jeffrey M. "Who Was the First Person Known to Have Discovered Fossils of the Precambrian (Ediacaran) Organism Aspidella terranovica?" Geoscience Canada 44, no. 1 (2017): 55. http://dx.doi.org/10.12789/geocanj.2017.44.115.

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This article briefly examines the possible confusion pertaining to the discoveries of Precambrian (Ediacaran) fossils made in the self-governing British colony of Newfoundland in 1868 by the amateur naturalist, the Reverend Moses Harvey, and the subsequent description and naming of the fossil organism Aspidella terranovica in 1872 by Elkanah Billings, the father of Canadian paleontology. Both events could be misinterpreted as one transaction that began with the former event and ended with the latter event. Accounts published by Alexander Murray, the director of the Geological Survey of Newfoun
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Van der Wal, Serita, Mario Schädel, Boris Ekrt, and Joachim T. Haug. "Description and ontogeny of a 40-million-year-old parasitic isopodan crustacean: Parvucymoides dvorakorum gen. et sp. nov." PeerJ 9 (December 9, 2021): e12317. http://dx.doi.org/10.7717/peerj.12317.

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A collection of exceptionally well-preserved fossil specimens of crustaceans, clearly representatives of Isopoda, is presented here. Excavated from the late Eocene (approximately 40 million years ago) freshwater sediments of the Trupelník hill field site near Kučlín, Czech Republic, these specimens are preserved with many details of the appendages. The morphological characteristics of the fossils were documented using macro-photography with polarised light, as well as stereo imaging. These characteristics, especially including the trunk appendage morphology, were compared to those of related e
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McMahon, Sean. "Earth's earliest and deepest purported fossils may be iron-mineralized chemical gardens." Proceedings of the Royal Society B: Biological Sciences 286, no. 1916 (2019): 20192410. http://dx.doi.org/10.1098/rspb.2019.2410.

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Recognizing fossil microorganisms is essential to the study of life's origin and evolution and to the ongoing search for life on Mars. Purported fossil microbes in ancient rocks include common assemblages of iron-mineral filaments and tubes. Recently, such assemblages have been interpreted to represent Earth's oldest body fossils, Earth's oldest fossil fungi, and Earth's best analogues for fossils that might form in the basaltic Martian subsurface. Many of these putative fossils exhibit hollow circular cross-sections, lifelike (non-crystallographic, constant-thickness, and bifurcate) branching
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Moura, Geraldo Jorge Barbosa, and Ulysses Paulino Albuquerque. "The First Report on the Medicinal Use of Fossils in Latin America." Evidence-Based Complementary and Alternative Medicine 2012 (2012): 1–5. http://dx.doi.org/10.1155/2012/691717.

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There have been very few ethnopharmacological studies performed on the traditional use of fossil species, although a few records have been conducted in Asia, Africa, and Europe. This study is the first ever to be performed on the use of Testudine (turtle) fossils for folk medicine in Latin America. An investigation was conducted in the Araripe Basin, which is one of the most important fossil-bearing reserves in the world due to the diversity, endemism, and quality of preservation of its fossils. We propose the formalization of a new discipline called ethnopaleontology, which will involve the s
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Martill, D. "The trade in Brazilian fossils: one palaeontologist's perspective." Geological Curator 7, no. 6 (2001): 211–18. http://dx.doi.org/10.55468/gc455.

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The Santana and Crato formations of the Araripe Basin are a prolific source of exceptionally well preserved mid Cretaceous fossils. Fossils are collected from the Crato Formation as a byproduct of quarrying activity, but those from the Santana Formation are mined commerically. The commerical trade in Brazilian fossils is illegal, but the trade flourishes. Despite occasional attempts to stamp out the trade, widespread corruption allows its continuity. A legitimate case can be made for the legalisation of the fossil trade that would be of benefit to the international scientific community and to
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Warner, Barry G., Helen J. Kubiw, and Paul F. Karrow. "Origin of a postglacial kettle-fill sequence near Georgetown, Ontario." Canadian Journal of Earth Sciences 28, no. 12 (1991): 1965–74. http://dx.doi.org/10.1139/e91-178.

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Stratigraphic relationships, radiocarbon dating, and pollen and plant macrofossil analyses establish the origin and developmental history of a kettle near Georgetown, Ontario. The early inorganic sediments contain redeposited fossils, particularly from local vegetation. Fossils in peat younger than 10 000 BP largely represent past wetland plant communities in the basin. Although the fossil record probably began about 1300 years after deglaciation of the site, an additional 1700 years passed before the dead ice block melted; only then did sedimentation and biological activity stabilize in the b
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37

BABCOCK, LOREN E. "Asymmetry in the fossil record." European Review 13, S2 (2005): 135–43. http://dx.doi.org/10.1017/s1062798705000712.

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Asymmetry is a fundamental aspect of the biology of all organisms, and has a deep evolutionary history. The fossil record contains evidence of both morphological and behavioural asymmetries. Morphological asymmetry is most commonly expressed as conspicuous, directional asymmetry (either lateral asymmetry or spiral asymmetry) in body fossils. Few examples of fluctuating asymmetry, a form of subtle asymmetry, have been documented from fossils. Body fossil evidence indicates that morphological asymmetry dates to the time of the appearance of the first life on Earth (Archaean Eon). Behavioural asy
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Debaaditya, Mukhopadhyay, and Chakrabarty Arghya. "Understanding the Significance of Protecting Wood Fossils to Preserve Palaeobotanical Past in Shahebgunj District, Jharkhand." Indian Journal of Natural Sciences 12, no. 68 (2021): 34807–11. https://doi.org/10.5281/zenodo.5708990.

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A wood fossil park in Mandro of Shahebgunj district in Jharkhand, India is at the risk of rapid weathering and decay. Sedimentological strata of stratigraphic columns frequently host wood fossils housing vital information about the past climate and ecology besides hinting at the possible evolutionary track. An understanding of wood fossils through palaeobotany reveals detailed track of development to the present fauna. Therefore, it is essential to conserve and study the exposed fossils.
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Gueriau, Pierre, Solenn Réguer, Nicolas Leclercq, et al. "Visualizing mineralization processes and fossil anatomy using synchronous synchrotron X-ray fluorescence and X-ray diffraction mapping." Journal of The Royal Society Interface 17, no. 169 (2020): 20200216. http://dx.doi.org/10.1098/rsif.2020.0216.

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Fossils, including those that occasionally preserve decay-prone soft tissues, are mostly made of minerals. Accessing their chemical composition provides unique insight into their past biology and/or the mechanisms by which they preserve, leading to a series of developments in chemical and elemental imaging. However, the mineral composition of fossils, particularly where soft tissues are preserved, is often only inferred indirectly from elemental data, while X-ray diffraction that specifically provides phase identification received little attention. Here, we show the use of synchrotron radiatio
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Colleary, Caitlin, Andrei Dolocan, James Gardner, et al. "Chemical, experimental, and morphological evidence for diagenetically altered melanin in exceptionally preserved fossils." Proceedings of the National Academy of Sciences 112, no. 41 (2015): 12592–97. https://doi.org/10.5281/zenodo.14820452.

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(Uploaded by Plazi for the Bat Literature Project) Significance Melanin is a widespread pigment that provides black to reddish brown hues to organisms. Recent evidence has shown that melanin is retained in exceptionally preserved fossils, including feathered dinosaurs, allowing the reconstruction of ancient color patterns. However, little is known about the chemical preservation of melanin or its distribution in the fossil record. Here, we show that melanin is preserved in a number of soft-bodied fossils, but its burial under high pressure and temperature for millions of years alters its origi
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King, Benedict, and Martin Rücklin. "Tip dating with fossil sites and stratigraphic sequences." PeerJ 8 (June 26, 2020): e9368. http://dx.doi.org/10.7717/peerj.9368.

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Tip dating, a method of phylogenetic analysis in which fossils are included as terminals and assigned an age, is becoming increasingly widely used in evolutionary studies. Current implementations of tip dating allow fossil ages to be assigned as a point estimate, or incorporate uncertainty through the use of uniform tip age priors. However, the use of tip age priors has the unwanted effect of decoupling the ages of fossils from the same fossil site. Here we introduce a new Markov Chain Monte Carlo (MCMC) proposal, which allows fossils from the same site to have linked ages, while still incorpo
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Hasiotis, S. T., and M. C. Bourke. "Continental trace fossils and museum exhibits: displaying organism behaviour frozen in time." Geological Curator 8, no. 5 (2006): 211–26. http://dx.doi.org/10.55468/gc366.

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This paper introduces continental trace fossils, and suggests ways in which modern and ancient traces can be used in museum exhibits. Burrows, tracks, trails, nests, borings, excrement and root patterns represent organism-substratum interactions of terrestrial and aquatic plants, invertebrates and vertebrates, and are preserved in the geologic record as continental trace fossils. Trace fossils are important because they are analogous to behaviour frozen in time and preserve information about organisms not recorded by body fossils. They can be used also as fossil evidence of organisms in the ge
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alrawi, Sufyan Shlash, and Abdulhammed A. Alhadaithy. "Sedimentology Study Of Exposed Formations In Al-Assad Valley, Al-Baghdadi Area, Western Iraq." IOP Conference Series: Earth and Environmental Science 1300, no. 1 (2024): 012038. http://dx.doi.org/10.1088/1755-1315/1300/1/012038.

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Abstract The presence of the Sheikh Alas Formation, the Shurau Formation, and the Euphrates Formation in the area of the current study. The inference of the Sheikh Alas Formation was from Nummlite fossils and planktonic Foraminifera fossils. The Euphrates Formation was deposited in a shallow marine environment, the Sheikh Alas Formation was deposited in an environment in for reef, and the Shurau Formation was deposited in an environment Back reef. The environment of the Euphrates Formation is a shallow lagoon environment for the presence of milliolied fossils, which represent the Miocene age a
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Hughes, Nigel C., Frederick J. Collier, Joanne Kluessendorf, Jere H. Lipps, Wendy L. Taylor, and Russell D. White. "Fossil Invertebrate and Microfossil Collections: Kinds, Uses, Users." Paleontological Society Special Publications 10 (2000): 25–36. http://dx.doi.org/10.1017/s2475262200008935.

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INVERTEBRATE and micro-fossil collections vary in size, scope, degree of documentation, quality of curation, purpose, usage, and security. This chapter introduces the main categories of fossil collections and curatorial attention, and documents the sources and uses of invertebrate paleontological materials. The term ‘permanent collection’ is used to describe collections housed in professional collections-care institutions that provide long-term commitment to collection security and curation. Invertebrate fossils include the hardparts (spicules, shells, etc., other body fossils [e.g., impressio
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Lalchhandama, Kholhring. "The Himalayan fossil hoax." WikiJournal of Science 7, no. 1 (2024): X. http://dx.doi.org/10.15347/wjs/2024.008.

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The Himalayan fossil hoax, or simply the Himalayan hoax, or the case of the peripatetic fossils, was perpetrated by an Indian geologist Vishwa Jit Gupta of Panjab University. Since his doctoral research in the early 1960s and the following two decades, Gupta worked on the geological and fossil studies of the Himalayan region, producing hundreds of research publications that were taken as fundamental to understanding the geology of the Himalayas. The Australian geologist John Talent of Macquarie University, who also worked on the geology of the Himalayas, found that Gupta's reports did not matc
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Edgecombe, Gregory D. "Arthropod Origins: Integrating Paleontological and Molecular Evidence." Annual Review of Ecology, Evolution, and Systematics 51, no. 1 (2020): 1–25. http://dx.doi.org/10.1146/annurev-ecolsys-011720-124437.

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Phylogenomics underpins a stable and mostly well-resolved hypothesis for the interrelationships of extant arthropods. Exceptionally preserved fossils are integrated into this framework by coding their morphological characters, as exemplified by total-evidence dating approaches that treat fossils as dated tips in analyses numerically dominated by molecular data. Cambrian fossils inform on the sequence of character acquisition in the arthropod stem group and in the stems of its main extant clades. The arthropod head problem incorporates unique appendage combinations and remains of the nervous sy
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47

Colleary, Caitlin, Andrei Dolocan, James Gardner, et al. "Chemical, experimental, and morphological evidence for diagenetically altered melanin in exceptionally preserved fossils." Proceedings of the National Academy of Sciences 112, no. 41 (2015): 12592–97. http://dx.doi.org/10.1073/pnas.1509831112.

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In living organisms, color patterns, behavior, and ecology are closely linked. Thus, detection of fossil pigments may permit inferences about important aspects of ancient animal ecology and evolution. Melanin-bearing melanosomes were suggested to preserve as organic residues in exceptionally preserved fossils, retaining distinct morphology that is associated with aspects of original color patterns. Nevertheless, these oblong and spherical structures have also been identified as fossilized bacteria. To date, chemical studies have not directly considered the effects of diagenesis on melanin pres
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Rule, James Patrick, Gustavo Burin, and Travis Park. "A quantitative test of the “Ecomorphotype Hypothesis” for fossil true seals (Family Phocidae)." PeerJ 12 (June 19, 2024): e17592. http://dx.doi.org/10.7717/peerj.17592.

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The fossil record of true seals (Family Phocidae) is mostly made up of isolated bones, some of which are type specimens. Previous studies have sought to increase referral of non-overlapping and unrelated fossils to these taxa using the ‘Ecomorphotype Hypothesis’, which stipulates that certain differences in morphology between taxa represent adaptations to differing ecology. On this basis, bulk fossil material could be lumped to a specific ecomorphotype, and then referred to species in that ecomorphotype, even if they are different bones. This qualitative and subjective method has been used oft
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Yamamura, Daigo. "Investigating the Timing of Carbonate Precipitations and Their Potential Impact on Fossil Preservation in the Hell Creek Formation." Minerals 14, no. 11 (2024): 1133. http://dx.doi.org/10.3390/min14111133.

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Because fossilized skeletal remains and enclosing sedimentary rocks experience similar diagenetic conditions (i.e., temperature, pressure, and pore fluid interaction,) enclosing sedimentary rocks may provide insight into bone diagenesis. A fossil assemblage, including in situ dinosaur fossils, was discovered in Makoshika State Park near Glendive, MT. Fossil-bearing sandstone is a crevasse splay deposit, and fossils show no sorting or preferred orientation. Bone-bearing sandstone exhibits evidence for intense diagenesis, suggesting a maximum temperature of ~90 °C. Concretion associated with fos
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Tilgner, Erich. "The fossil record of Phasmida (Insecta: Neoptera)." Insect Systematics & Evolution 31, no. 4 (2000): 473–80. http://dx.doi.org/10.1163/187631200x00507.

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AbstractA review of the Phasmida fossil record is provided. No fossils of Timema Scudder are known. Euphasmida fossils include: Agathemera reclusa Scudder, Electrobaculum gracilis Sharov, Eophasma oregonense Sellick, Eophasma minor Sellick, Eophasmina manchesteri Sellick, Pseudoperla gracilipes Pictet, Pseudoperla lineata Pictet and various unclassified species from Grube Messel, Baltic amber, and Dominican Republic amber. The oldest documented Euphasmida fossils are 44-49 million years old; molecular clock dating underestimates the origin of the sister group Timema by at least 24 million year
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