Academic literature on the topic 'Fossils'

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Journal articles on the topic "Fossils"

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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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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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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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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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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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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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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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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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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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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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Dissertations / Theses on the topic "Fossils"

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Van, Dijk D. E. "Contributions to knowledge of some Southern African fossil sites and their fossils /." Link to the online version, 2000. http://hdl.handle.net/10019/3561.

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Van, Dijk D. E. "Contributions to knowledge of some Southern African fossil sites and their fossils." Thesis, Stellenbosch : University of Stellenbosch, 2001. http://hdl.handle.net/10019.1/2988.

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Thesis (MSc (Botany and Zoology. Palaeontology))--University of Stellenbosch, 2001.<br>The fossil sites and fossils reported here range from the Archaean to the Recent. Information is presented on the circumstances of the discovery of some fossil sites in Southern Africa. A number of fossil sites, some of which can no longer be studied, are photographically recorded. Some recorded sites were relocated, while failure to locate others is noted. The assemblages at selected fossil sites are compiled, including some additions to their floras and faunas. Certain individual fossils are illustra
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Rydin, Catarina. "The Gnetales : fossils and phylogenies /." Stockholm : Department of Botany, Stockholm University, 2005. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-488.

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Brocks, Jochen J. "Molecular fossils in Archean rocks." Phd thesis, School of Geosciences, 2001. http://hdl.handle.net/2123/14300.

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Mounce, Ross. "Comparative cladistics : fossils, morphological data partitions and lost branches in the fossil tree of life." Thesis, University of Bath, 2013. https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.642021.

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In this thesis I attempt to gather together a wide range of cladistic analysis of fossil and extant taxa representing a diverse array of phylogenetic groups. I use this data to quantitatively compare the effect of fossil taxa relative to extant taxa in terms of support for relationships, number of most parsimonious trees (MPTs) and leaf stability. In line with previous studies I find that the effects of fossil taxa are seldom different to extant taxa – although I highlight some interesting exceptions. I also use this data to compare the phylogenetic signal within vertebrate morphological data
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Herman, Julie D. "Fossil preservation and the effects of groundwater leaching on fossils in the Yorktown Formation (Upper Pliocene), Virginia." Thesis, Virginia Polytechnic Institute and State University, 1987. http://hdl.handle.net/10919/90972.

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Patterns of fossil diagenesis caused by groundwater leaching provide insight into how shells are altered. This study analyzes fossils in unconsolidated terrigenous sediments from the Virginia Coastal Plain, unlike previous studies conducted mostly in carbonate terranes. The vertical and lateral distribution of diagenetic states was mapped in an outcrop (63 m by 2.1 m) of the Yorktown Formation. A paleostream channel located at one end was incised during the Pleistocene and filled with sediments of the Shirley Formation. The Tabb Formation unconformably overlies the outcrop. Acidic groundwater
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Buckman, James O. "Lower Carboniferous trace fossils from northwest Ireland." Thesis, Queen's University Belfast, 1992. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.262648.

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Legg, David. "The impact of fossils on arthropod phylogeny." Thesis, Imperial College London, 2013. http://hdl.handle.net/10044/1/24168.

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The arthropods are the most diverse, abundant and ubiquitous phylum on Earth. Five main extant groups (subphyla) can be recognized: Pycnogonida, Euchelicerata, Myriapoda, Hexapoda, and Crustacea. Each group displays a distinctive body plan and a suite of autapomorphies that makes determining their interrelationships difficult. Although a variety of hypotheses have been proposed regarding their interrelationships, just three have frequently been recovered in recent phylogenetic analyses. Rather than representing incongruent topologies these hypotheses represent variations of the position of the
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Cooper, Robert D. "A knowledge-based system for hominid fossils." [Gainesville, Fla.] : University of Florida, 2004. http://purl.fcla.edu/fcla/etd/UFE0004420.

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Friend, Duncan. "Palaeobiology of Palaeozoic medusiform stem group echinoderms." Thesis, University of Cambridge, 1995. https://www.repository.cam.ac.uk/handle/1810/265414.

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The morphological details of both external and internal anatomy of a group of Palaeozoic fossil medusiform animals are described with the aid of text-figures and plates with explanatory drawings. This fossil group had a worldwide distribution with a stratigraphic range from the Lower Cambrian to the Upper Devonian and includes the following taxa:- Eldonia ludwigi Walcott 1911, E. eumorphus sp. nov., Rotadiscus grandis Sun and Hou 1987, Discophylluni peltatum Hall 1847, D. mirabile Chapman 1926, D. cryptophya (Clarke) 1900. Newly recognised anatomical structures for E. ludwigi include c.30, int
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Books on the topic "Fossils"

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Spilsbury, Louise. Journal of a fossil hunter: Fossils. Raintree, 2004.

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Walker, Cyril Alexander. Fossils. Dorling Kindersley, 1992.

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Walker, Sally M. Fossils. Lerner Publications Co., 2007.

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Moody, Richard. Fossils. Collier Books, 1986.

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Canada, Geological Survey of. Fossils. s.n, 1987.

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Moody, Richard. Fossils. Hamlyn, 1986.

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Fortey, Richard A. Fossils. Natural History Museum, 2009.

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Stewart, Melissa. Fossils. Compass Point Books, 2003.

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Spilsbury, Richard. Fossils. Heinemann Library, 2011.

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Carl, Mehling, ed. Fossils. Thunder Bay Press, 2007.

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Book chapters on the topic "Fossils"

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Dahlgren, Rolf M. T., H. Trevor Clifford, and Peter F. Yeo. "Fossils." In The Families of the Monocotyledons. Springer Berlin Heidelberg, 1985. http://dx.doi.org/10.1007/978-3-642-61663-1_6.

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Prost, Gary L., and Benjamin P. Prost. "Fossils." In The Geology Companion. CRC Press, 2017. http://dx.doi.org/10.1201/9781315152929-7.

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Prance, Ghillean T. "Fossils." In Humiriaceae. Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-82359-7_4.

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Thulborn, Tony. "Dinosaur fossils." In Dinosaur Tracks. Springer Netherlands, 1990. http://dx.doi.org/10.1007/978-94-009-0409-5_1.

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Eigenbrode, Jennifer. "Molecular Fossils." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-642-11274-4_1015.

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Brenchley, Patrick J., and David A. T. Harper. "Trace fossils." In Palaeoecology. Springer US, 1998. http://dx.doi.org/10.1007/978-1-4684-1410-3_5.

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Eigenbrode, Jennifer. "Molecular Fossils." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2015. http://dx.doi.org/10.1007/978-3-662-44185-5_1015.

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Lindholm, Roy C. "Trace fossils." In A Practical Approach to Sedimentology. Springer Netherlands, 1987. http://dx.doi.org/10.1007/978-94-011-7683-5_4.

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Brenchley, Patrick J., and David A. T. Harper. "Trace fossils." In Palaeoecology. CRC Press, 2023. http://dx.doi.org/10.1201/9781003419921-5.

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Williams, Ross H. "Molecular Fossils." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2023. http://dx.doi.org/10.1007/978-3-662-65093-6_1015.

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Conference papers on the topic "Fossils"

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Buatois, Luis A., and Maria Gabriela Mangano. "CONGRUENCE OF DIVERSITY TRAJECTORIES BETWEEN BODY FOSSILS AND TRACE FOSSILS." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-286852.

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Tuzyak, Ya M. "FROM LIVING ORGANISMS TO FOSSILS. THE IMPORTANCE OF FOSSILS TO SOCIETY." In NATURAL SCIENCES AND THEIR IMPORTANCE FOR SOCIETY. Izdevnieciba “Baltija Publishing”, 2024. http://dx.doi.org/10.30525/978-9934-26-413-9-11.

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Oldham, Jordan C. "INVERTEBRATE FOSSILS OF OHIO CAVERNS." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-359616.

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Downs, Simon T., and Claire A. Lerpiniere. "The Future of Heuristic Fossils." In Design Research Society Conference 2018. Design Research Society, 2018. http://dx.doi.org/10.21606/drs.2018.612.

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Dunlap, Sam. "MATRIX FOSSILS IN MAINE AND MYANMAR." In 51st Annual Northeastern GSA Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016ne-272471.

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Lidgard, Scott, and Alan C. Love. "LIVING FOSSILS AS A RESEARCH PROGRAM." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-300986.

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Organ, Chris L. "GENOME MACROEVOLUTION: INSIGHTS FROM FOSSILS AND PHYLOGENIES." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-297650.

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Rindsberg, Andrew, and Tony Martin. "ICHNOGENY: GROWTH AND CHANGE IN TRACE FOSSILS." In Southeastern Section-70th Annual Meeting-2021. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021se-362345.

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Elsayed, Omar Refaie, Yosr Gamal ElKot, Dina Ashraf ElRefaai, Hagar Mohamed Abdelfattah, Maha ElSayed, and Alaa Hamdy. "Automated Identification and Classification of Teeth Fossils." In 2023 International Mobile, Intelligent, and Ubiquitous Computing Conference (MIUCC). IEEE, 2023. http://dx.doi.org/10.1109/miucc58832.2023.10278368.

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Letsch, Dominik, Simon Large, Simon Large, et al. "NW AFRICA’S OLDEST KNOWN SKELETAL FOSSILS: A NEW CAMBRIAN SMALL SHELLY FOSSIL FAUNA FROM SOUTH MOROCCO." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-298097.

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Reports on the topic "Fossils"

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Lanik, Amanda, Mikaela Ruga, Chad Hults, and Claire Schmid. Paleontological resources monitoring at Fossil Point, Lake Clark National Park and Preserve: 2019 field report. National Park Service, 2024. http://dx.doi.org/10.36967/2300633.

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Fossil Point is an exceptionally rich and scientifically important fossil locality found in Lake Clark National Park and Preserve. The rocks at Fossil Point are known for their abundant and well-preserved Middle Jurassic invertebrate fossils, including bivalves, ammonites, and belemnites. The abundance and quality, as well as the relatively easy coastal access, makes the fossils at Fossil Point vulnerable to unauthorized collection. Anecdotal evidence suggests that collection without a permit is occurring at Fossil Point and has been for decades. Monitoring of the prevalence and scale of unaut
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Harrington, Matthew, Amanda Lanik, Chad Hults, and Patrick Druckenmiller. Focused condition assessment of paleontological resources within Katmai National Park and Preserve. National Park Service, 2023. http://dx.doi.org/10.36967/2298782.

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The paleontological resources (fossils) of Katmai National Park and Preserve (also referred to as ?the park? or ?Katmai? throughout this report) record the evolution of the park?s ancient life throughout most of the Mesozoic Era and portions of the Cenozoic Era (see Table 1 for a geologic time scale). A focused condition assessment (FCA) of the paleontological resources of Katmai was conducted in 2021; this report summarizes the findings of the FCA, including information on the park?s geology and paleontology, management issues related to paleontological resources, and the results of a field s
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Rich, Megan, Charles Beightol, Christy Visaggi, Justin Tweet, and Vincent Santucci. Vicksburg National Military Park: Paleontological resource inventory (sensitive version). National Park Service, 2023. http://dx.doi.org/10.36967/2297321.

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Vicksburg National Military Park (VICK) was established for its historical significance as a one of the principle military sieges resulting in a turning point during the American Civil War. The steep terrain around the city of Vicksburg was integral in the military siege, providing high vantage points and a substrate that was easy to entrench for the armies, but unknown to many is the fossil content, particularly a diversity of fossil mollusks. These fossils at VICK are important paleontological resources which have yet to receive focused attention from park staff, visitors, and researchers. T
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Shaffer, Austin, Justin Tweet, and Vincent Santucci. Colorado National Monument: Paleontological resource inventory (sensitive version). National Park Service, 2024. http://dx.doi.org/10.36967/2303444.

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Colorado National Monument (COLM) in western Colorado was established on May 24, 1911 with the purpose of preserving, understanding, and enjoying the natural and cultural resources of the landscape, focusing on the history, erosional processes, and geology present. Although not explicitly mentioned in the monument?s purpose statement, the paleontological resources of COLM are nevertheless important. Significant fossils have been known from the area since the late 19th and early 20th centuries, and from COLM specifically within a few decades of the monument?s founding. The direct urban interfac
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Shaffer, Austin, Justin Tweet, and Vincent Santucci. Colorado National Monument: Paleontological resource inventory (public version). National Park Service, 2024. http://dx.doi.org/10.36967/2303613.

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Colorado National Monument (COLM) in western Colorado was established on May 24, 1911 with the purpose of preserving, understanding, and enjoying the natural and cultural resources of the landscape, focusing on the history, erosional processes, and geology present. Although not explicitly mentioned in the monument?s purpose statement, the paleontological resources of COLM are nevertheless important. Significant fossils have been known from the area since the late 19th and early 20th centuries, and from COLM specifically within a few decades of the monument?s founding. The direct urban interfac
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Harrington, Matthew, Amanda Lanik, and Chad Hults. Paleontological resource monitoring at Kaguyak Point, Katmai National Park and Preserve. National Park Service, 2023. http://dx.doi.org/10.36967/2298794.

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Fieldwork was conducted during the summers of 2017 and 2021 to assess the risk of unauthorized collection and erosion to ammonite fossils located at Kaguyak Point in Katmai National Park and Preserve. Past reports indicated that unauthorized fossil collecting may have occurred at Kaguyak Point. Our monitoring found no signs of unauthorized collecting during the summer of 2021 and our findings also indicate that it is unlikely that collecting occurred between 2017 and 2021. If unauthorized fossil collecting occurred in the past at Kaguyak Point, it appears to have now stopped. The best way to p
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Chriscoe, Mackenzie, Rowan Lockwood, Justin Tweet, and Vincent Santucci. Colonial National Historical Park: Paleontological resource inventory (public version). National Park Service, 2022. http://dx.doi.org/10.36967/nrr-2291851.

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Colonial National Historical Park (COLO) in eastern Virginia was established for its historical significance, but significant paleontological resources are also found within its boundaries. The bluffs around Yorktown are composed of sedimentary rocks and deposits of the Yorktown Formation, a marine unit deposited approximately 4.9 to 2.8 million years ago. When the Yorktown Formation was being deposited, the shallow seas were populated by many species of invertebrates, vertebrates, and micro-organisms which have left body fossils and trace fossils behind. Corals, bryozoans, bivalves, gastropod
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Hodnett, John, Ralph Eshelman, Nicholas Gardner, and Vincent Santucci. Geology, Pleistocene paleontology, and research history of the Cumberland Bone Cave: Potomac Heritage National Scenic Trail. National Park Service, 2023. http://dx.doi.org/10.36967/2296839.

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The Cumberland Bone Cave is a public visitation stop along the Potomac Heritage National Scenic Trail renowned for its unique fossil resources that help reconstruct Appalachian middle Pleistocene life in the mid-Atlantic region of North America. This site is gated for safety and to prevent unwanted exploration and damage. Approximately 163 taxa of fossil plant and animals have been collected from Cumberland Bone Cave since 1912. Most of the fossils that have been published pertain to mammals, including many extinct or locally extirpated genera and species. Though the early excavations made by
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Herring, Theodore, Justin Tweet, and Vincent Santucci. Wind Cave National Park: Paleontological resource inventory (public version). National Park Service, 2023. http://dx.doi.org/10.36967/2299620.

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Wind Cave National Park (WICA), the first cave in the world to become a national park, is famous for the park’s namesake feature. Wind Cave, named for the noticeable wind-flow patterns observed as air moves in and out of the natural cave entrance, is currently the third longest cave system in the United States and seventh longest in the world. Wind Cave formed when groundwater dissolved buried layers of the fossiliferous Madison Limestone, which were deposited during the Mississippian subperiod approximately 359 to 347 million years ago. In addition to the Madison Limestone, several other form
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Tweet, Justin, Vincent Santucci, Vincent Santucci, and Justin Tweet. Effigy Mounds National Monument: Paleontological resource inventory (public version). National Park Service, 2025. https://doi.org/10.36967/2307451.

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Effigy Mounds National Monument (EFMO) in northeastern Iowa was proclaimed on October 25, 1949, to protect a significant concentration of Native American burial mounds, many of which were built in the shapes of animals such as bears. Many of these effigy mounds are found atop commanding bluffs flanking the Yellow River at its junction with the Mississippi River. The geology of the monument has not been a central interest in its history, but the rocks contain evidence of millions of years of shallow marine life from the early Paleozoic. Paleozoic fossils were first documented at what is now EFM
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