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  1. Dpaul7

    STEGOPDON BONE 0.jpg

    From the album: MY FOSSIL Collection - Dpaul7

    Stegodon Bone China Pleistocene age (2,588,000 to 11,700 years ago) Stegodon (meaning "roofed tooth" from the Greek words stegein 'to cover' and odous 'tooth', because of the distinctive ridges on the animal's molars) is a genus of the extinct subfamily Stegodontinae of the order Proboscidea. It was assigned to the family Elephantidae (Abel, 1919), but has also been placed in Stegodontidae (R. L. Carroll, 1988). Stegodonts were present from 11.6 mya to late Pleistocene, with unconfirmed records of regional survival until 4,100 years ago. Fossils are found in Asian and African strata dating from the late Miocene. They lived in large parts of Asia, East and Central Africa during the Pleistocene. Kingdom: Animalia Phylum: Chordata Class: Mammalia Order: Proboscidea Family: †Stegodontidae Genus: †Stegodon
  2. Dpaul7

    STEGOPDON BONE 0.jpg

    From the album: MY FOSSIL Collection - Dpaul7

    Stegodon Bone China Pleistocene age (2,588,000 to 11,700 years ago) Stegodon (meaning "roofed tooth" from the Greek words stegein 'to cover' and odous 'tooth', because of the distinctive ridges on the animal's molars) is a genus of the extinct subfamily Stegodontinae of the order Proboscidea. It was assigned to the family Elephantidae (Abel, 1919), but has also been placed in Stegodontidae (R. L. Carroll, 1988). Stegodonts were present from 11.6 mya to late Pleistocene, with unconfirmed records of regional survival until 4,100 years ago. Fossils are found in Asian and African strata dating from the late Miocene. They lived in large parts of Asia, East and Central Africa during the Pleistocene. Kingdom: Animalia Phylum: Chordata Class: Mammalia Order: Proboscidea Family: †Stegodontidae Genus: †Stegodon
  3. Dpaul7

    STEGOPDON BONE 0.jpg

    From the album: MY FOSSIL Collection - Dpaul7

    Stegodon Bone China Pleistocene age (2,588,000 to 11,700 years ago) Stegodon (meaning "roofed tooth" from the Greek words stegein 'to cover' and odous 'tooth', because of the distinctive ridges on the animal's molars) is a genus of the extinct subfamily Stegodontinae of the order Proboscidea. It was assigned to the family Elephantidae (Abel, 1919), but has also been placed in Stegodontidae (R. L. Carroll, 1988). Stegodonts were present from 11.6 mya to late Pleistocene, with unconfirmed records of regional survival until 4,100 years ago. Fossils are found in Asian and African strata dating from the late Miocene. They lived in large parts of Asia, East and Central Africa during the Pleistocene. Kingdom: Animalia Phylum: Chordata Class: Mammalia Order: Proboscidea Family: †Stegodontidae Genus: †Stegodon
  4. Dpaul7

    STEGOPDON BONE 0.jpg

    From the album: MY FOSSIL Collection - Dpaul7

    Stegodon Bone China Pleistocene age (2,588,000 to 11,700 years ago) Stegodon (meaning "roofed tooth" from the Greek words stegein 'to cover' and odous 'tooth', because of the distinctive ridges on the animal's molars) is a genus of the extinct subfamily Stegodontinae of the order Proboscidea. It was assigned to the family Elephantidae (Abel, 1919), but has also been placed in Stegodontidae (R. L. Carroll, 1988). Stegodonts were present from 11.6 mya to late Pleistocene, with unconfirmed records of regional survival until 4,100 years ago. Fossils are found in Asian and African strata dating from the late Miocene. They lived in large parts of Asia, East and Central Africa during the Pleistocene. Kingdom: Animalia Phylum: Chordata Class: Mammalia Order: Proboscidea Family: †Stegodontidae Genus: †Stegodon
  5. MarcusFossils

    Parayiliangella quadrisulcata

    A new trilobite for my collection I don't think more complete specimens exist.
  6. oilshale

    Megapalaeolenus deprati Mansuy, 1912

    From the album: Invertebrates

    Megapalaeolenus deprati Mansuy, 1912 Early Cambrian Gaolufang Yunnan China
  7. oilshale

    Insect non det.

    From the album: Invertebrates

    Insect non det Upper Jurassic Daohugou Nei Mongol China
  8. MarcusFossils

    Extremely Rare Dictyella longispina

    A complete specimen of the trilobite wasn't known for more than 70 years after the Dictyella genus was established by Kobayashi in 1933.
  9. References: Sun, Weiguo and Hou Xianguang. (1987). Early Cambrian medusae from Chengjiang, Yunnan, China. Acta Palaeontologica Sinica 26:257–271. Jun-Yuan Chen, Di-Ying Huang and Shou-Hwa Chuang Journal of Paleontology Vol. 81, No. 1 (Jan., 2007), pp. 38-47 YUGAN, J. and HUAYU, W. (1992), Revision of the Lower Cambrian brachiopod Heliomedusa Sun & Hou, 1987. Lethaia, 25: 35–49. doi:10.1111/j.1502-3931.1992.tb01790.x
  10. oilshale

    Blattodea non det.

    From the album: Invertebrates

    Blattodea non det. Middle Jurassic Daohugou Nei Mongol China Length 1cm
  11. oilshale

    Ammonite Plaster

    From the album: Invertebrates

    Ammonites Late Triassic Carnian Xiaowa Formation Yunnan PRC
  12. MarcusFossils

    Zhangshania typica

    A very rare Chinese trilobite.
  13. Kane

    Coronocephalus gaoluoensis

    From the album: Trilobites

  14. Taxonomy from Schweitzer et al. 2014. Quote (Schweitzer et al. 2014, p. 457): "Although the lobsters were interpreted as having relatively durable cuticle, the shrimp discussed herein are characterized by having very thin cuticle that is readily deformed and oriented in a variety of positions. As a result, the description and interpretation of the morphology of the shrimp is, of necessity, a composite of several specimens; however, fine detail of many parts of the skeletal anatomy is exquisite." Diagnosis from Schweitzer et al. 2014, p. 467: "Carapace longer than high; rostrum very long, 40 percent length of carapace, with one basal suprarostral spine and one subrostral spine at midlength; uropodal exopod with diaeresis; ventral lateral margins of telson with setal pits, appearing to extend entire length of telson; third maxilliped about as long as first and second pereiopods, with spine bases or setal pits along propodal and dactyl ventral margin; pereiopods 1– 3 chelate, third pereiopod longest, fourth and fifth longer than first and second, pereiopods without spines; pleopods apparently with multiarticulate flagellae." Identified by oilshale using Schweitzer et al. 2014. Characteristic is the extremely long rostrum, constituting 40 percent of the carapace length. References: SCHWEITZER, C., FELDMANN, R.,HU, S.,HUANG, J., ZHOU, C., ZHANG, Q.,WEN, W., Xie, T.(2014): PENAEOID DECAPODA (DENDROBRANCHIATA) FROM THE LUOPING BIOTA (MIDDLE TRIASSIC) OF CHINA: SYSTEMATICS AND TAPHONOMIC FRAMEWORK. Journal of Paleontology, 88(3), 2014, p. 457–474,
  15. From the album: Vertebrates

    Wushaichthys exquisitus Xu, Zhao & Shen, 2015 Middle Triassic Ladinian - early Carnian Falang Formation Zhuganpo Member Wusha near Xingyi Guizhou Province PR China Length 5cm
  16. oilshale

    Palaeolenus douvillei Mansuy, 1912

    From the album: Invertebrates

    Palaeolenus douvillei Mansuy, 1912 Lower Cambrian Guanshan Fauna Wulongqing Formation Shitangshan Quarry Guangwei District Kunming Provinz Yunnan PR China Length 1cm Lit.: Liu, J. et al.(2012) New occurence of the Cambrian (Stage 4, Series 2) Guanshan Biota in Huize, Yunnan, South China. Bulletin of Geosciences Vol. 87, 1, 2012, pp125-132
  17. oilshale

    Sinoeocrinus lui

    From the album: Invertebrates

    Sinoeocrinus lui Zhao et al 1994 Lower Cambrian Kaili Formation Maiobanpo Guizhou China
  18. oilshale

    Palaeolenus lantenoisi Mansuy, 1912

    From the album: Invertebrates

    Palaeolenus lantenoisi Mansuy, 1912 Lower Cambrian Maotianshan Formation Chengjiang Province Yunnan PR China Length 1,2cm / .5" Lit.: Liu et al (2012) New occurence of the Cambrian Guanshan Biota in Huize, Yunnan, South China. Bull. of Geosciences 87,1, 125-132
  19. From the album: Invertebrates

    Distaeger prodigiosus Schweitzer et al., 2014 Middle Triassic Luoping Yunnan China
  20. From the album: Invertebrates

    Yuknessia sp. Early Cambrian Haikou Yunnan China Yuknessia was originally interpreted as a green alga and has since been reinterpreted it as a colonial pterobranch.
  21. Originally named Sinosaurichthys by Wu et al., 2011, the genus was reranked as Saurichthys by A. Tintori (2013) Diagnosis from Wu et al. 2011, p. 595: "Medium−sized Sinosaurichthys (standard body length ranging from 270–470 mm) with unusually elongated median fins with relatively few segments of fin rays; less number of neural arches between opercle and caudal fin (approximately 157–172), less number of anterior ones with neural spines (130–146); and less number of mid−dorsal scales in front of dorsal fin (69–86) than in type species; 14–15 distinct haemal spines in caudal region; pectoral fin triangular shaped with length about 1/3 of mandible length (shared with S. minuta described below); posttemporal−supracleithrum from either side separated from each other by anterior mid−dorsal scales (shared with S. minuta described below); cleithrum plate (depth/length ratio ca. 1.2–1.25) much lower than in type species (approximately 1.8), but close to that in S. minuta (ap− proximately 1). Fin formula: P 18–19, V 18–20, D/A 44–49/ >40–48, C 37–39/37–39." Identified by oilshale using Wu et al. 2011. References: Wu, F.X., Sun, Y.L., Xu, G.H., Hao, W.C., Jiang, D.Y., and Sun, Z.Y. (2011) New saurichthyid actinopterygian fishes from the Anisian (Middle Triassic) of southwestern China. Acta Palaeontologica Polonica 56 (3): 581–614. Tintori, A. (2013) A new species of Saurichthys (Actinopterygii) from the Middle Triassic (Early Ladinian) 0f the Northern Grigna Mountain (Lombardy, Italy). Rivista Italiana di Paleontologia e Stratigrafia 119 (3):287. DOI: 10.13130/2039-4942/6041.
  22. gigantoraptor

    Cicade

    Length is antenna included. The picture is from the trade itself, if anyone knows how to cut the chinese letters out, please let me know.
  23. gigantoraptor

    Cockroach

    Length is without the legs
  24. oilshale

    Diandongia pista Rong, 1974

    From the album: Invertebrates

    Diandongia pista Rong, 1974 Early Cambrian Series 2, Stage 3 Haikou Kunming County Yunnan China Lit.: Zhang, Z.-F., et al. (2003). Pediculate Brachiopod Diandongia pista from the Lower Cambrian of South China. Acta Geologica Sinica, Vol.77, Number 3. Zhifei Zhang, Jian Han, Yang Wang, Christian C. Emig, Degan Shu (2009) Epibionts on the lingulate brachiopod Diandongia from the Early Cambrian Chengjiang Lagerstätte, South China. Proc. R. Soc. B (2010) 277, 175–181. Zhifei Zhang, Jian Han, Z Xingliang Zhang, Jianni Liu, Degan Shu (2003) Pediculate Brachiopod Diandongia pista from the Lower Cambrian of South China. Acta Geologica Sinica. Vol. 77, No 3., pp 288-293.
  25. Dpaul7

    Lituites Fossil Specimen.jpg

    From the album: MY FOSSIL Collection - Dpaul7

    Lituites Fossil China TIME PERIOD: late Ordovician Period (445-458 Million Years ago) Data: Lituites is an extinct nautiloid genus from the Middle Ordovician and type for the Lituitidae (a tarphycerid family) that in some more recent taxonomies has been classified with the orthocerids and listed under the order Lituitida. it's now considered widespread, Fossils have been found in New York, Argentina, Norway, Sweden, Estonia, and China. Lituites produced a shell with a planospirally coiled juvenile portion at the apex, reflective of its tarphycerid ancestry, followed by a long, moderately expanding, generally straight, orthoconic adult section with a subdorsal siphuncle connecting the chambers. The adult body chamber may equal or exceed the length of the chambered part of the orthoconic section. The mature aperture has a pair of pronounced ventrolateral lappets and a similar but shorter pair of dorsolateral lappets. Lituites gives its name to the term "lituiticone" which refers to a shell that is coiled in the early growth stage and later becomes uncoiled. Kingdom: Animalia Phylum: Mollusca Class: Cephalopoda Order: †Orthocerida Family: †Lituitidae Genus: †Lituites
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