• Title/Summary/Keyword: fossils

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Application of RTI to Improve Image Clarity of a Trace Fossil Cochlichnus Found from the Jinju and Haman Formations

  • Sangho Won;Dal-Yong Kong
    • Economic and Environmental Geology
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    • v.56 no.4
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    • pp.397-408
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    • 2023
  • A total of 64 specimens of trace fossils were collected from the Jinju Formation of the construction site of Jinju Aviation Industrial Complex, and from the Haman Formation of Namhae Gain-ri fossil site. The fossils are continuously and regularly meandering sine-curve in shape. The fossil varies in morphology: width between 0.2 and 5.6 mm, wavelength between 1.5 and 28 mm, and amplitude between 0.9 and 7.9 mm; the Jinju specimens are commonly wider than the Haman ones. The ratio of wavelength to amplitude is more or less regular regardless of width of the specimen, and the linear correlation of the ratios shows that the Jinju specimens fit better than the Haman specimens. Taking all morphometric parameters, specimens in all size ranges are temporarily identified as ichnospecies Cochlichnus anguineus. In order to obtain more distinct and clearer images of Cochlichnus, we selected two specimens and applied a new imaging technology RTI. For photography of the trace fossils, 50 to 80 images were taken per set with photometric lighting close to the surface and horizontally. RTI technology clearly showed that the images of tiny fossils were improved: the surface contrast become sharper and messy and unnecessary information disappeared. Currently, RTI technology is used in many fields including preservation of cultural properties and archaeology. As a consequence, we hope to apply this technique to the field of paleontology, especially to the study of trace fossils of very small size.

Trace Fossils from the Late Pleistocene Marginal Marine Deposits of Jeju Island, Korea: Implications for the Psilonichnus and Skolithos Ichnofacies

  • Kim, Jeong Yul;Kang, Ji Hyun
    • Journal of the Korean earth science society
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    • v.39 no.1
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    • pp.23-45
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    • 2018
  • Moderately diverse, but very abundant trace fossils are found from the Late Pleistocene deposits of Jeju Island, Korea. Vertical I-, Y- and U-shaped domichnia of annelids or decapods are, over 2500, extremely abundant, 3D network domichnia of callianassids are, over 200, very abundant, and small sinuous trails of nematode repichnia are, over 50, abundant in number. Horizontal trails attributable to polychaete or worm-like animals are, less than 50, common, but horizontal spreiten burrows, fish traces and crab trackways are, less than 10, rare in occurrence. Of these trace fossils, Taenidium barretti, Undichna britannica and Undichna unisulca represent the first record from the Pleistocene in Asia. Psilonichnus upsilon is the second record in Asia. Crab trackways probably produced by underwater punting gait of sideway walking crabs may represent the first record in the world. In addition, diverse and very abundant footprints of more than 500 hominids, more than 200 birds and more than 1000 mammals are closely associated with these invertebrate trace fossils. Trace fossil assemblage integrated with sedimentary facies is interpreted to have been formed in the marginal marine foreshore to backshore environment corresponding to the Psilonichnus and Skolithos ichnofacies.

Conservation and Application Scheme of Hominid and Other Vertebrate Footprints from Jeju Island, Korea

  • Lee, Chang-Zin;Kim, Jeong-Yul;Kim, Kyung-Soo
    • Journal of the Korean earth science society
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    • v.30 no.5
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    • pp.581-587
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    • 2009
  • This study intended to the optimal conservation method and to make an application scheme for the fossil locality of the Quaternary Hamori Formation at the northeastern coast of Mt. Songak. Many kinds of innumerable fossils are found from the Hamori Formation in the study area: Footprints of hominid, trace fossils of invertebrates, bird, artiodactyla, proboscidea, carnivores, unclassified footprints, and body fossils (arthropoda, gastropoda, mollusca, and plants). The formation has been outcropped and eroded out with innumerous fossils by the strong wave action of storm and typhoon. Korean government recognized the dangerous situation of the important fossils and decided to conserve the formation for the national heritage. Method D1 (conservation hall or museum on the fossil locality) may be the best way to protect the fossil locality from all the natural activities and to do the research, exhibition, education, and sightseeing together. The application of the geologic materials from the fossil locality should preferentially focus on the collection and research which should be accompanied by exhibition, education, and sightseeing. The application scheme may be stepped into three stages during 10 years: (1) systematic conservation and publicity during 2005-2007, (2) establishment of wellorganized museum during 2008-2010, and (3) international museum with the optimized roles 2011-2014.

Deterioration Diagnosis and Evaluation of Physical Properties in the Dinosaur Footprint Fossils in Cheongsong Sinseongri, Korea, for the Conservation Plans (보존방안 수립을 위한 청송 신성리 공룡발자국 화석지의 손상도 진단 및 물성평가)

  • Yang, Hye Ri;Lee, Chan Hee;Park, Jun Hyoung
    • Economic and Environmental Geology
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    • v.54 no.3
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    • pp.311-330
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    • 2021
  • The Sinseongri site contains at least eleven theropod trackways, three sauropod trackways, and one or more ornithopod walkways of dinosaur footprints. The host rock at the site is primarily siltstone and mudstone, but thermal alterations have metamorphosed it into hornfels. Except for micro cracks and exfoliations, joint systems in various directions appeared on the surface of the fossils site and showed a low share of all damage factors. The host rocks in the fossils site demonstrated relatively high physical properties as a result of ultrasonic velocity and were classified as stable. More than half of the fossils required reinforcement to control the progression of cracks if the type of conservation treatment was subdivided according to the damage type of dinosaur footprint fossils. The white paint used to visualize the footprints seems to deteriorate, allowing rock debris to spill out and causing damage to the fossil site, and alternative visualization schemes should be considered.

Understanding on the Fossilization of Middle School Students (화석 형성 과정에 대한 중학생들의 이해)

  • Hwang, Koo-Geun;Cho, Kyu-Seong;Huh, Min
    • Journal of the Korean earth science society
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    • v.30 no.3
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    • pp.305-316
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    • 2009
  • Experiments to explain fossilization have been introduced in elementary and middle school science textbooks. Most of them have explained the processes by the mold and cast formed by imprint of bivalve or leaf. The processes explained in the textbooks are more similar to that of trace fossil than body fossil, because the external molds from experiment are imprints after the model was taken off. However fossils of the figures in the textbooks are mostly body fossils. Therefore, the students may be willing to equate the experiment process with the fossilization of the body fossils. The misconceptions were confirmed in this study by the questionnaire which asked 9th grade students on this subject. Many students thought that the body fossils were fossilized imprints and the fossils of terrestrial organism were formed on land without transportation, that is, they did not understand well about biostratinomy and crustal movement. The misconception about the environment in which fossils formed was already reported in a survey on the elementary school students, but has not revised until ninth grade. Therefore, to remove the misconception related to the fossilization, the fossil models in the experiments may be replaced by trace fossils, or new experiments for body fossil should be designed.

Reconsideration of the Natural Monument Geummubong Petrified Tree Fern Fossil Site, Ghilgok, Korea (천연기념물 칠곡 금무봉 나무고사리 화석산지에 대한 고찰)

  • Seung-Ho Jung;Dal-Yong Kong
    • Economic and Environmental Geology
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    • v.57 no.1
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    • pp.93-105
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    • 2024
  • Chilgok Geummubong tree fern fossil site is the type locality where tree fern stem fossils (Cyathocaulis naktongensis) were first discovered by Tateiwa in 1925. Recognized for its academic value, it was designated as a natural monument in the 1930s during the Japanese colonial period, and preserved and managed for over 90 years. However, at the time of discovery, the stratigraphic level of tree fern fossils could not be located because the fossils were fragments detached from the rock body, and thus the Geummubong area where the conglomerate/sandstone layers of the Nakdong Formation are distributed, has been designated as a cultural heritage area. Only in the 2000s, when tree fern fossils were directly recovered from the outcrops near the designated area, the sedimentary rock facies containing the fossils were interpreted, and the anatomical characteristics of the Mesozoic tree fern fossils could be described and identified as a species level. Such studies are, in these days, redefining classification criteria done by Japanese paleontologist, Ogura. That is, Korean researchers pointed out that the classification criteria of the tree fern fossils (Cyathocaulis) reported early from Chilgok were ambiguous, and the possibility that the two species were the same species was suggested. In addition, it is necessary to reorganize designated areas as a way to resolve social conflicts and civil complaints caused by various regulations that have continued for a long time.

Albizia Fruit Fossils from the Miocene Duho Formation of Yeonil Group in the Pohang Basin, Korea (포항 분지의 마이오세 연일층군의 두호층에서 산출된 Albizia의 열매 화석)

  • Kim, Jong-Heon;Lee, Seong-Bok;An, Ji-Min;Lee, Hye-In;Hong, Han-Sol
    • Journal of the Korean earth science society
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    • v.30 no.1
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    • pp.10-18
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    • 2009
  • Two fruit fossils of Albizia miokalkora were collected from the Miocene Duho Formation of Yeonil Group in the northern Pohang Beach and Changpodong, Gyeongsangbug-do, Korea. The legume is flat and long and has 7 rounded seeds. Although the legume fossils are preserved as impression, they show their whole shape well. It is considered that the fossil Albizia might have flourished in a warm temperate climate in East Asia. This discovery is the second record of Albizia from the Neogene of Korea.

Development and Application of STEAM Class for Stratum and Fossil with Questions (질문이 있는 '지층과 화석' 관련 STEAM 수업 자료 개발 및 적용)

  • Jeong, Mi-Young;Hong, Seung-Ho
    • Journal of Korean Elementary Science Education
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    • v.37 no.4
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    • pp.455-465
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    • 2018
  • The purpose of this study is to investigate the effect of 'strata-fossils' STEAM program with questions on the academic achievement, creative problem-solving ability and scientific interests of elementary students. For this purpose, the STEAM program with questions was developed and applied to the third and fourth graders in elementary school. As a result, the academic achievement, creative problem-solving ability and scientific interests of the group applying the program showed a significant improvement in the post-test than the pre-test. The result of learner satisfaction survey of the STEAM program was also high. This means that the STEAM program class with questions for 'strata-fossils' could be meaningful works to encourage students' academic achievement as well as their creative problem-solving ability and scientific interests. Therefore, it seems necessary to apply for other themes in elementary science continuously.

Pleuronichthys sp. Fossils (Pleuronectidae) from the Duho Formation, Pohang Uhyeon-dong in Korea (포항시 우현동 두호층에서 산출된 Pleuronichthys sp. 화석)

  • Ko, Ju-Yeong;Nam, Kye-Soo
    • Journal of the Korean earth science society
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    • v.37 no.3
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    • pp.133-142
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    • 2016
  • Two specimens of the Cenozoic fish fossils were discovered from the Miocene Duho Formation of Uhyeon-dong, Pohang, Korea. These fossils are identified as Pleuronichthys sp. based on the following- firstly, front dorsal fin rays elongated to the upper part of neurocranium, Secondly, right sided orbit of neurocranium, Thirdly, presence of urohyal like fish-hook, Fourthly, curved sciatic part of the urohyal, Fifthly, presence of postcleithrum, Sixthly, over 27 centrum, Seventhly, elongated first pterygiophore of the anal fin rays, Eightly, c-shaped inner side of urohyal, Ninthly, small or few cardiac apophysis, and Tenthly, presence of many spots on body. These fossils of Pleuronichthys represent the first record in East-Asia. Two specimens are anatomically different in the extent of the asymmetry and the flatness of skull. This represents the unique ontogeny stage of the Pleuronectidae, because they accompany the above anatomical difference when they transform from pelagic lifestyle to benthic lifestyle.