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  1. Rava89

    Hello from Italy!!

    Hello everyone!! I'm from Italy, new to the fossils world but I've always been fascinated by extinct creatures since I was a little kid. I've been reading posts in this forum for a little while, and I finally decided to join you guys, so that I can learn something about identification, fake/restored fossils, and much more... Can't wait to know more about this world!!
  2. Agos1221

    Real fossil seahorse?

    Hello all, I am considering buying this specimen but I know that fossil seahorses are often conflated with fossil pipe fish, which are more common and less valuable. Can anyone weigh in on the authenticity of this identification and whether or not the specimen appears to have been altered? Thanks!
  3. Taxonomy according to Taverne and Capasso 2012. Amended diagnosis by Taverne and Capasso 2012, p. 30 (translated from French by oilshale): “Pycnodontine which can reach several tens of centimeters. Moderately high body. Dorsal apex located in front of the origin of the dorsal fin. Ventral apex located at the level of the origin of the anal fin. Triangular cephalic profile and pointed snout. Cranial dermal bones decorated with microgranulations and wrinkles. Endocranium exposed behind the dermocranium. Frontal with a narrow posteroventral branch descending to the dermosphenotic and dermopterotic and having only limited contact with these two bones. Parietal narrow, elevated, surmounting dermosphenotic and lined with a posterior brush-like process.…” Line drawing from Taverne and Capasso 2012, p. 32: Identified by oilshale using Taverne and Capasso 2012 References: Taverne L. (1997) Les poissons crétacés de Nardò. 5°. Pycnodus nardoensis sp. nov. et considérations sur l’ostéologie du genre Pycnodus (Actinopterygii, Halecostomi, Pycnodontiformes). Bollettino del Museo di Storia Naturale di Verona, 21: 437-454. Taverne L. and Capasso L. (2012) Les poissons crétacés de Nardò. 35°. Compléments à l’étude des halécostomes Belonostomus (Aspidorhynchiformes) et Pseudopycnodus (Pycnodontiformes). Bollettino del Museo Civico di Storia Naturale di Verona, 36: 25-44.
  4. I encountered this facing stone in the lobby of the Chicago Board of Trade building (1930). It’s some kind of cobble conglomerate(?) but I’ve never seen its like. The security guard said it was from Italy, but I haven’t done further research. Photos below show fossils and various lithologies. Help, please!
  5. Taxonomy according to fossilworks.org. Diagnosis for the genus from Bannikov 2008, p. 79: "Body depth is 13-14 times in SL; head length 2.9 times in SL; teeth moderate, conical; 56 vertebrae; 2 epurals; epaxial hypurals unfused; distance between dorsal fins exceeds distance between second dorsal and caudal fin; 12 to 13 interdorsal bones between dorsal fins; a spine and 7 or 8 soft rays in second dorsal fin; a spine and 9 or 10 soft rays in anal fin; second dorsal fin originates not less than 2 vertebrae behind anal-fin origin; pectoral fins short, with 13 or 14 rays; 6-rayed pelvic fins moderate, situated about 4 vertebrae anterior to first dorsal-fin origin; pectoral to pelvic fin distance less than pelvic to anal fin distance." Line drawing from Bannikov 2008, p. 83: Identified by oilshale using Bannikov 2008. Confirmed by A. F. Bannikov, Paleontological Institute of the Russian Academy of Sciences, Moscow. References: Agassiz, L. (1835) Recherches Sur Les Poissons Fossiles. Tome IV (livr. 4). Imprimerie de Petitpierre, Neuchatel 33-52. Bannikov A.F., (2008e). Revision of the atheriniform fish genera Rhamphognathus Agassiz and Mesogaster Agassiz (Teleostei) from the Eocene of Bolca, northern Italy. Miscellanea Paleontologica n. 9. Studi e Ricerche sui Giacimenti Terziari di Bolca, 12: 77-97. Carnevale, G., Bannikov, A. F., Marramá, G., Tyler, J. C. and Zorzin, R. (2014): The Pesciara-Monte Postale Fossil-Lagerstätte: 2. Fishes and other vertebrates. Rendiconti della Società Paleontologica Italiana 4:37-63. Bannikov. A. F. (2014): The systematic composition of the Eocene actinopterygian fish fauna from Monte Bolca, northern Italy, as known to date. Studi e ricerche sui giacimenti terziari di Bolca, XV - Miscellanea paleontologica 12:23-34.
  6. Taxonomy according to Marramà & Carnevale 2015. Diagnosis for the genus Bolcaichthys according to Marramà & Carnevale 2015: “Small- to medium-sized clupeid (largest specimen measuring 101.1 mm SL) with elongated and tapered body, sardine-like; † Bolcaichthys, gen. nov., is unique among clupeids in having the following combination of characters: head length approximately one third to one quarter SL; skull roof with 10–14 frontoparietal striae; mouth terminal; two supramaxillae, anterior small and rod-like, and posterior paddle-shaped; teeth absents in jaws and palate; complete series of abdominal keeled scutes (10–11 prepelvic and 10 or 11 postpelvic) with ascending arms; dorsal scutes absent; fewer branchiostegal rays (5 or 6), supraneurals (8), vertebrae (40–42), and pleural ribs (20–22) compared with other genera of clupeids; pleural ribs–preural vertebrae ratio ranging from 0.48 to 0.55; three epurals; deeply forked caudal fin with 19 principal caudal-fin rays; dorsal fin small, inserting at about mid-length of the body with 15 or 16 rays; about 15 or 16 anal-fin rays; about 14–18 pectoral-fin rays; pelvic-fin origin slightly in front of or behind the posterior end of the dorsal fin; eight pelvic-fin rays.” Line drawing of Bolcaichthys catopygopterus (Woodward, 1901) from Marramà and Carnevale, 2015: Identified by oilshale using Marramà & Carnevale, 2015. References: Agassiz, L. (1833–1844). Recherches sur les Poissons Fossiles. Petitpierre, Neuchâtel, 1420 pp. Woodward, A. S. (1901): Catalogue of Fossil Fishes in the British Museum (Natural History), 4: Containing the Actinopterygian Teleostomi of the Suborders Isospondyli (in part), Ostariophysi, Apodes, Percesoces, Hemibranchii, Acanthopterygii and Anacanthini. Taylor and Francis, London, 636 pp. Marramà, G. & Carnevale, G. (2015): The Eocene sardine †Bolcaichthys catopygopterus (Woodward, 1901) from Monte Bolca, Italy: osteology, taxonomy, and paleobiology, Journal of Vertebrate Paleontology. DOI: 10.1080/02724634.2015.1014490
  7. Taxonomy according Fossilworks.org. Diagnosis according to Blot 1978, p. 146: "Tête contenue un peu moins de six fois dans la longueur totale. Hauteur du corps contenue de quinze à dix-neuf fois dans la même longueur. Les deux branches de cleithra de longueurs équivalentes. Côtes ventrales présentes. Osselets intermusculaires bien développés. Caudale constituée par neuf rayons s'articulant sur les hypuraux. Coefficient de concentration de la nageoire dorsale: 2,50, celui de l'anale étant aux environs de 2,85." This translates: “Head contained a little less than six times in the total length. Height of the body contained from fifteen to nineteen times in the same length. Both cleithra branches of equivalent lengths. Ventral ribs present. Intermuscular bones well developed. Caudal constituted by nine rays articulating on the hypurals. Coefficient of concentration of the dorsal fin: 2.50, that of the anal being around 2.85.” Line drawing of Bolcyrus formosissimus from Blot 1978, p. 149. Identified by oilshale using Blot 1978. References: Blot, J. (1976) Les anguilliformes fossiles du Monte Bolca. 2e Congres Europeen des Ichtyologistes Europeens, Paris, 1976, Revue Trav. Inst. Pech. Marit., Nantes, 40 (3&4) 509-511, 1 tabl. Blot, J. (1978): Les apodes fossiles du Monte Bolca. Studi e Ricerche sui Giacimenti Terziari di Bolca 3:(1): 1-260, 120 fig, 21 tabl. 39pl. Blot, J. (1984): Les Apodes fossiles du Monte Bolca. 2. Actinopterygii : Ordre des Apodes (Anguilliformes): Famille des Paranguillidae Blot 1980. Museo civico di storia naturale di Verona, 1984, p. 62-238, 24 p. di tav. G. Carnevale, A. F. Bannikov, G. Marramá, J. C. Tyler, and R. Zorzin (2014): The Pesciara-Monte Postale Fossil-Lagerstätte: 2. Fishes and other vertebrates. Rendiconti della Società Paleontologica Italiana 4:37-63.
  8. From the album: Vertebrates

    Bolcyrus formosissimus (Eastmann, 1905) Eocene Monte Bolca near Verona Italy
  9. Hello everybody. My name is Marco, I live in Italy. I have a small collection of fossils and would like to share experiences with other collectors -
  10. DarkTr

    Hi everyone

    Hi, my name is Stefano and I'm from Italy. I' m fond of dinosaur since I was a child. Thanks you all.
  11. The fossils were found in the 70s in northern Sardinia during the excavations for the construction of a road. I do not know the exact location, but I know that it is the north of Sardinia. The coin is 1 euro (it's similar in size to an American quarter.) What could it be? Thanks in advance
  12. HuatloCollection

    Hello from Italy!!

    Hi guys, new to the Forum! I'm a Geology and Paleontology university student from Italy, and also a fossil collector! I hope will share my pieces as well as my help with the members!
  13. giannisergente

    Hello from Apulia (South Italy)

    Hello everybody! I'm new here. I come from the south of Italy, I'm really passionate about fossils and paleontology in general. I will be glad to communicate, read about your collections and exchange information. I'm very happy to join this community:)
  14. From the album: Vertebrates

    Pseudosparnodus microstomus (Agassiz, 1839) Eocene Lutetian Monte Bolca near Verona Italy
  15. Reg

    Fossil fish ID

    Hi all, I got this fossil fish from an uncle of mine but he didn't know ID and origin. Could you please help me out identifying the right species? Thank you
  16. oilshale

    Legnonotus krambergeri Bartram, 1977

    Taxonomy from Fossilworks.org. Genus Diagnosis by Bartram 1977, p.163: " Small macrosemiid fishes, the trunk tapering gradually to form a broad caudal peduncle; skull roof bearing genuine; gape small, the quadrate articulation lying beneath the anterior part of the orbit; dentigerous expansion of maxilla with upper and lower borders straight and diverging posteriorly, hind border also straight and perpendicular to oral border, bearing about 13 small, closely—set teeth; mandible with dentary bearing about 12 closely-set teeth, coronoid teeth rounded; leading edge of preopercular forming sharp angle; abdomina] vertebrae forming thin cylinders, notochord unconstricted; pectoral fin with about 15 rays, leading ray reduced to unpaired splint, no fringing fulcra; pelvic fin formed by five rays preceded by basa] and fringing fulcra; anal fin with seven rays, base compact; caudal fin weakly forked, axial lobe bearing five rays; dorsal fin single and long, preceded by basal and fringing fulcra, outline high anteriorly, convex posteriorly; region immediately on either side of dorsal fin devoid of scales; scales rhomboid." Species Diagnosis by Bartram 1977, p.164: "Legnonotus with about 25 dorsal fin-rays; dentary teeth tall and sharp." Line drawing from Bartram 1977, p. 164: Identified by oilshale using Bartram 1977. References: Bartram, A.W.H. (1977) The Macrosemiidae, a Mesozoic family of Holostean fishes. Bulletin of the British Museum of Natural History (Geology), 29, 137-234. Tintori, A. and Renesto, S. (1983) The Macrosemiidae (Pisces, Actinopterygii) from the Upper Triassic of Lombardy (N. Italy). Rivista Italiana di Paleontologia e Stratigrafia 89(2):209-222.
  17. Hello, Last saturday I had a trek in a mountain area in the northen Italy alps and I found this fossil (I'm not actaully 100% sure that it's a fossil, but I don't know what else could it be). It looks like an echinoderm fossil to me, but I'd like to ask your opinion about it. Thanks a lot, have a nice day. Oz
  18. Steffen Herman

    Animal tooth ID

    Hello everyone, I was just searching the internet to find out what animal's tooth I found the other day, when I came across this lovely forum full of expertise. So I'd kindly like to ask if someone would help me identify the animal that was once the proud owner of this tooth. Some info: - Find place: southwestern Siciliy - age: some 2500 years / late Holocene - found in an archaeological context Any ideas greatly appreciated. Steffen
  19. Max10

    Hi everybody!

    Hi everybody! My name is Max, i'm 33 and i'm from Tuscany, Italy. I decided to register me in the forum because i start to collecting fossils and i want to learn more about it. I have some trilobites, ammonites and several teeth of different species... I'm quite a beginner but i have a strong will to learn with humility as much as i can. Thanks for gave me the possibility to join this forum!
  20. Hello everybody can somebody help me identifying my fossil fish (4cm) I am pretty convinced that it concerns the exellia velifer from monte bolca looking forward to Your replies regards Rienk
  21. Nematos

    What could it be ?

    Hello, have some idea about it? Found in 1906 in Italy, Bellagio country Dimension about 4 cm long thanks
  22. Hello dear members, Today I'd like to talk about my latest fieldtrip, to the Late Triassic tracksite of Zone, Lombardy prealps, Italy. However, I'd like to make it clear that it involved no fossil collecting, because of the scientific interest of the site and of italian laws, that prevent (almost) any form of this activity. I know there is the "Fossil sites" section, but I thought that here my post would have reached more people. I apologize in case this is not allowed. Let's not waste any more time! Italy is quite well know for its tracksites, in particular those bearing dinosaur tracks: Altamura (the largest tracksite in Europe!) and Lavini di Marco, just to give an example. On the other hand sites of Late Triassic age, bearing archosaurian footprints are poorly documented. Zone is a tiny village located nearby the Lake Iseo, in the Southern prealps, some 80 km (50 mi) east of Milan (see the red arrow on the map below). Back in the Late Triassic (Carnian) this area was an alluvial fan, characterized by a semiarid climate and, further to the south, by the occurrence of a series of volcanic edifices. Tracks are, in fact, preserved in terrigenous-volcaniclastic beds. Ripple marks and groove casts can be found too. The material is represented by a total of about 70 footprints, arranged in six trackways on two different layers. The older displays three trackways that cross each other, the younger three distinct trackways. Footprints are only moderately preserved, nonetheless several anatomical details are evident on those of the younger level. In addition to traditional mapping methods, a laser scanner was employed to obtain high-quality 3D digital models. Let's talk about who left this footprints for us to admire! Those of the younger level are referred to a quadrupedal trackmaker with plantigrade, pentadactyl pes (distal portion of the hind limb) and manus (distal portion of the fore limb). They have been assigned to the ichnogenus Brachychirotherium, known by a global distribution and probably left by a crurotarsan archosaur. It is not clear whether it was a rauisuchian (predator) or an aetosaur (armored vegetarian). On the field, I must admit that I was a little disappointed. Judging by the pictures published in the 2009 paper that described the outcrop, at least two trackways were quite distinct and visible. However, that was not the case: only 4 tracks (two manus and two pes) were indeed immediately identifiable. I guess that's possibly due to two factors: on the one hand weathering (the fine grained sandstone is very fragile), on the other hand inclination of solar rays. Tracks are best visible in raking light, but I visited at around 10-11 am in a clear February day. In the summer period I'm quite sure that much more could be seen!! In order to highlight the footprints and compare with the presente state, I chose to show also a pictures taken from the paper: you can distinghuish it easily, because it is in b/w. Today this is the best that you could ask for in this section (older layer) The overall best preserved manus-pes track, in the younger layer. Reconstruction of this set of footrprints Close up of the Manus, scale bar is 5 cm (2 in). total lenght of the track: some 30 cm (11,8 in). The second best preserved manus-pes association Reconstruction of a rauisuchian (on the left) and an aetosaur (on the right). On top lower right digital model of the best preserved trackway (I showed you the picture of the first two sets of imprints). A rauisuchian The significance of the Zone tracksite is that it represents the first definite ichnological record of archosaur tracks found in Lombardy and footprints are among the best preserved, although an upcoming paper is going to feature recently found tracks that are even better preserved (and I gave my contribution in the excavation campaign!). On the field, I must admit that I was a little disappointed. Judging by the pictures published in the 2009 paper that described the outcrop, at least two trackways were quite distinct and visible. However, that was not the case: only 4 tracks (two manus and two pes) were indeed immediately identifiable. I guess that's possibly due to two factors: on the one hand weathering (the fine grained sandstone is very fragile), on the other hand inclination of solar rays. Tracks are best visible in raking light, but I visited at around 10-11 am in a clear February day. In the summer period I'm quite sure that much more could be seen!! Anyway, it was a great experience: easy access, few people walking by, great scientific value! I hope that you liked my short report, Fabio
  23. oilshale

    Carangopsis dorsalis

    From the album: Vertebrates

    Carangopsis dorsalis Middle Eocene Monte Bolca Verona Italy length 10cm
  24. Marcosaur

    Hello from Italy

    Hi everyone, thanks for welcoming me. My name is Marco and I am a student of natural sciences in Italy. I am one of the administrators of a paleontology forum in my country, and I have known your forum for a long time. I decided to register because I was thinking of preparing fossils and here I found many useful discussions. I am interested in fossils of fish and reptiles, but I also collect other types of fossil finds. thanks again for the welcome, a greeting to everyone! Marco Sabia
  25. From the album: Plants

    oak leaf, (Quercus). Pléistocène Re (Val Vigezzo) Italy
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