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Found 449 results

  1. My family and I usually visit the Frio River in Leakey, Tx every summer. A few years ago we were all set to go swimming but upon arriving we saw that the part of the river we usually frequent had dried up. I decided to make the best of it and explored the dried river bed looking for anything interesting when this isolated chunk of rock caught my eye. I picked it up off the ground, took it home with me, put it in a drawer and forgot about it. A few months ago I found it while doing some cleaning and realized it had to be something more than just an oddly shaped rock. I cleaned it with water and a toothbrush after reading online that that's a simple way to clean fossils. A friend of mine with limited knowledge of fossils suspected it was some kind of fossilized coral or sponge. What I originally thought was matrix does look a lot like syringopora, but I can't find pictures of any prehistoric coral fossils that match the appearance of that hot dog in the center! I saw a sperm whale tooth on this forum that looks similar but I'm not sure if what I found feels like a tooth. It feels way too smooth to me. I love fossils and I own some shark teeth, coprolite, and a little trilobite, but those were all bought. If whatever this is turns out to be something, then it would be the first fossil I've ever acutally found myself. I'm still really new to this so please forgive me if I am asking silly questions or submitting this incorrectly. Any insight would be greatly appreciated!
  2. It has been a couple years since I made time to pull together some photos of personal finds to share. Inhospitable climes this past weekend afforded me the opportunity to organize a little eye candy for your viewing pleasure, arranged from geologically oldest to youngest. Provenance - for brevity, I'll just refer to the sites collectively as "Gulf of Mexico Watershed, Texas". Thanks for understanding and respecting. For more detail, go to Youtube and pull up Johnny Cash's "I've Been Everywhere". I will say that the Texas Outback comes with its perils, as shown below. Some of the pics are grainy due to fleeting photo opps, but you can see a big gator sliding into the water, a curious tarantula, a snake (water mocassin?) exercising the "stand your ground" law, and a rattler that became tablefare at the Woehrhaus. I even had a "Hugh Glass" moment with an injured hog while out solo gigging this year, and was glad to come out on top. I should be able to complete photo adds to this thread today in short bursts.
  3. My youngest son goes fossil hunting without me these days and a few years ago he went to the parachute member of the Green River Formation and found some fossil leafs. He asked me the other day if I would do a prep job on a leaf he had found. I said "sure". So, he brought it over and I did some 'prep majic on it. It didn't look too good when I first took a gander at it, but I figured I could get some tips out of it and expose the stem. The more work I did on it the better it got. The bad thing was the leaf itself was not in very good preservation with the rock very discolored around the leaf making it hard to see. So, the mind got to thinkin and then I decided to do a bit of artwork around it. I have to say that was a good idea. Still have a ways to go but its coming along quite nice!!! One of those fossils where the more you do the better it gets. RB
  4. Here it is, the show booth layout! What do yah think? did we get enough fish this year? I am kind of fond of the table, it is fully lit all the way around the inside with LED lights!
  5. Hi Folks, I am taking the opportunity of terrible weather here to sort out some of my fossil finds from last year. This set of specimens comes from the Middle Eocene Allenby formation on Allenby Road near Princeton British Columbia Canada. The main structures I see are the shiny patches of material that resemble the slickinside we see in our concretions here on Vancouver Island. The material does not appear to have much depth. The rock is a cherty mudstone. Patches of sheet like algae? Mud striations?
  6. The order Beryciformes, a poorly understood group, is represented in Monte Bolca with at least two species: Eoholocentrum and Berybolcensis, both from the subfamily Holocentrinae or squirrelfish (L. Sorbini, 1984). Both species seemed to be largely or entirely nocturnal and lived in deep marine waters; their eyes are amazingly large. Lit.: Sorbini, L., 1979. Les Holocentridae du Monte Bolca. III. Berybolcensis leptacanthus (Agassiz). Studi e Richerche sui Giacimenti Terziari di Bolca 4, 19–35.
  7. Diodon holocanthus, inflated (own work of Ibrahim lujaz from Rep. Of Maldives) Diodon nicthemerus (own work of user Springcold at da.wikipedia) Porcupinefish belong to the family Diodontidae within the Tetraodontiformes order and are also commonly called blowfish. They have the ability to swallow water or air and to inflate their body making it harder for predators to swallow them. When the fish inflates, sharp spines radiate outwards as a second defense mechanism. Some species are poisonous, having tetrodotoxin in their internal organs. Fugu is the Japanese word for pufferfish and is also a Japanese dish made out of the pufferfish meat. Because fugu is lethally poisonous if prepared incorrectly, fugu has become one of the most celebrated and notorious dishes in Japanese cuisine. Porcupinefish are medium to large sized fish and are found in shallow temperate and tropical seas worldwide. Monte Bolca is an important lagerstatte for Tetraodontiformes with Diodon tenuispinus as one of its oldest records.
  8. Hi all! Here are three sharkteeth I have from Balegem, Belgium. The sharkteeth there are from the Eocene. Those will soon go into a trade, so I need to get an ID quickly! Right now, the ID I have is this (from left to right): Physogaleus latus, Lamna nasus, Jaekelotodus trigonalis. Are those ID correct? Best regards, Max
  9. Most of my fossil collecting has been Invertebrate Macrofossil collecting. Very little attention has been made to the little fossils. It is always a good idea to expand your knowledge, leave your comfort zone, go somewhere you have never been before. I find that not paying much attention to Microfossils has been a mistake. So when I saw an interesting Nummulites fossil slab for sale; I chose to purchase it. The rough cut specimen looked like it could reveal more, with a little attention. What I chose to do is give it a good high luster lap polish to see the results. So much more detail was made. Where my specimen came from was Northern Spain, in or near the Pyrenees Mtns. near Aragon. The seller didn't give much info and what he did give was in Spanish. Chasing information down on the internet I found the mixed fossils were Nummulites sp. (large ones) and Alveolina sp. (smaller ones) I have some photos of my results to share. Before polishing it looked like this: After polishing the fossils clarified, here are some closeups: Apparently these fossils are common in Spain, neighboring France and other places in the world. This is an old engraving: In Spain, the Limestone the Nummulites are in, is used as building materials like blocks, steps, pavers. I will need to do more studying of these neat looking spiral tests.
  10. Pesciarichthys baldwinae Sorbini & Tyler, 1998 was redescribed in 2012 by Bannikov & Tyler and the new genus Frigosorbinia established. Lit.: Bannikov. A. & Tyler, J.C. (2012): REDESCRIPTION OF THE EOCENE OF MONTE BOLCA, ITALY, SURGEON FISH PESCIARICHTHYS PUNCTATUS PERCIFORMES, ACANTHURIDAE, AND A NEW GENUS, FRIGOSORBINIA, FOR P. BALDWINAE. Studi e ricerche sui giacimenti terziari di bolca, XIV - Miscellanea Paleontologica, 11, 2012
  11. Here it is my pleasure to quote Auspex: "Messelornis is often incorrectly referred to as the "Messel Rail". Although rails are in the same order (Gruiformes, along with the cranes), its closest living relative is the Sunbittern of the American tropics. There are four named species (of two genera) in the family Messelornithidae: Messelornis cristata (only from Messel), M. nearctica (from the Eocene Green River Fm., USA), M. russelli (from the Paleocene of France), and Itardiornis hessae (from the Late Eocene-Early Oligocene fissure-fillings in Quercy, France). According to Gerald Meyer in Paleocene Fossil Birds, there are over 500 specimens of M. cristata known from the Messel pit, constituting roughly half of the bird fossils found there. Interestingly, no juvenile specimens are known from there, which suggests that they did not nest nearby." Lit.: Angelika Hesse (1988): Die Messelornithidae - eine neue Familie der Kranichartigen (Aves: Gruiformes: Rhynocheti) aus dem Tertiär Europas und Nordamerikas. In: Journal für Ornithologie, 129 (1): 83-95; Berlin. Angelika Hesse (1990): Die Beschreibung der Messelornithidae (Aves: Gruiformes: Rhynocheti) aus dem Alttertiär Europas und Nordamerikas. Senckenbergische Naturforschende Gesellschaft. ISBN 9783924500672 Gerald Mayr (2009): Paleogene Fossil Birds. Springer. ISBN 9783540896272
  12. This is a great I.d. site
  13. Hello TFF! I just wanted to take a minute to share with everyone some of our finds from 2016. I do most of my digging up in Kemmerer, WY trying my hand at fossil fishes. 2016 was a pretty exceptional year in that along with our standard hundreds of 18" fish and thousands of split fish we pulled 2 VERY LARGE specimens. quite rare really. it averages out to about 1 every 2 or 3 years normally, so 2 in one summer is AMAZING! These panels have all been finished and are ready to hit the market along with the large gar and the croc! Fingers crossed that they sell so we can open up next year! I hope you all enjoy coming along. ALL of these panels feature 100% natural fish with 0% restoration. NO PAINT, a few have been inlaid though. In the last picture, the branch does have around 2% restoration because it was in multiple pieces needing to be glued.
  14. I have some fossils from the Green River that I collected several years ago. One of them had a nice full Knightia on it but the matrix was so thick that I decided to split it. When I did, I found these two small lumps on the newly split surface. The one on the right looks like it has bony fragments in it, I was wondering if these were some sort of fish poop. Nothing else shows up on this layer.
  15. The misses and I went to quartzite for a small vacation and just got back yesterday. We also went last year and had so much fun that we decided to go again. I have friends that have been going there every year for the last 18 years and it was great to meet up again. I use to sell there for about 8 or 9 years but quit once I realized it was turning into a job. I use to do 7 or 8 shows a year and went down to 0 for the last 10 years. I did take some fossils with me. I had a spot about 4 feet wide. Just to keep me a busy, kinda. I did help my buddy do quite a bit of selling, but for me, I was just there to sip wiskey, shoot the poop and have fun. I didn't even have to try and sell the crabs I took with me. Once people pick them up and hold them in their hands and see them close up, they sell themselves! The crabs I sold payed for the trip and the stuff I bought and the next two trips also. Just a neat hobbie. I took 17 prepped out crabs with me and sold 13 of them. Looks like the price for crabs are going to go up next year yet again!!! I really cant believe how much I get for these. But all in all it was a great trip, made lots and lots of moneys and had a super good time with lots of drinks, lots of good food and lots of good times.
  16. These are a few of the pdf files (and a few Microsoft Word documents) that I've accumulated in my web browsing. MOST of these are hyperlinked to their source. If you want one that is not hyperlinked or if the link isn't working, e-mail me at joegallo1954@gmail.com and I'll be happy to send it to you. Please note that this list will be updated continuously as I find more available resources. All of these files are freely available on the Internet so there should be no copyright issues. Articles with author names in RED are new additions since January 25, 2017. General Papers in Paleontology Archaean Eon Allwood, A.C., et al. (2009). Controls on development and diversity of Early Archaean stromatolites. PNAS, Vol.106, Number 24. Altermann, W. and J. Kazmierczak (2003). Archaean microfossils: a reappraisal of early life on Earth. Research in Microbiology, 154. Awramik, S.M. (1992). The oldest records of photosynthesis. Photosynthesis Research, 33. Brasier, M., et al. (2006). A fresh look at the fossil evidence for early Archaean cellular life. Phil.Trans.R.Soc.Lond. B, 361. Brasier, M., et al. (2004). Earth's Oldest (~3.5 Ga) Fossils and the 'Early Eden Hypothesis': Questioning the Evidence. Origins of Life and Evolution of the Biosphere, 34. Brocks, J.J., et al. (1999). Archaean Molecular Fossils and the Early Rise of Eukaryotes. Science, Vol.285. Knauth, L.P. (2005). Temperature and salinity history of the Precambrian ocean: implications for the course of microbial evolution. Palaeogeography, Palaeoclimatology, Palaeoecology, 219. Moorbath, S. (2005). Oldest rocks, earliest life, heaviest impacts, and the Hadean-Archaean transition. Applied Geochemistry, 30. Sankaran, A.V. (2002). The controversy over early-Archaean microfossils. Current Science, Vol.83, Number 1. Schopf, J.W. (2006). Fossil evidence of Archaean life. Phil.Trans.R.Soc. B, 361. Schopf, J.W. (1993). Microfossils of the Early Archaean Apex Chert: New Evidence of the Antiquity of Life. Science, Vol.260. Schopf, J.W., et al. (2007). Evidence of Archaean life: Stromatolites and microfossils. Precambrian Research, 158. Sharma, M. and Y. Shukla (2009). The evolution and distribution of life in the Precambrian eon - Global perspective and the Indian record. J.Biosci., 34. Stueken, E.E., D.C. Catling and R. Buick (2012). Contributions to late Archaean sulphur cycling by life on land. Nature Geoscience, published on-line. Waldbauer, J.R., D.K. Newman and R.E. Summons (2011). Microaerobic steroid biosynthesis and the molecular record of Archaean life. PNAS, Vol.108, Number 33. Proterozoic Eon Ediacaran Period Barroso, F.R.G., et al. (2014). First Ediacaran Fauna Occurrence in Northeastern Brazil (Jairabas Basin, ?Ediacaran-Cambrian): Preliminary Results and Regional Correlation. Annals of the Brazilian Academy of Sciences, 86(3). Bottjer, D.J. (2002). 2. Enigmatic Ediacara Fossils: Ancestors or Aliens? In: Exceptional Fossil Preservation. Bottjer, D.J., et al. (eds.), Columbia University Press, New York. Clapham, M.E., G.M. Narbonne and J.G. Gehling (2003). Paleoecology of the oldest known animal communities: Ediacaran assemblages at Mistaken Point, Newfoundland. Paleobiology, 29(4). Droser, M.L. and J.G. Gehling (2015). The advent of animals: The view from the Ediacaran. PNAS, Vol.112, Number 16. Droser, M.L., J.G. Gehling, and S.R. Jensen (2006). Assemblage palaeoecology of the Ediacara biota: The unabridged edition?. Palaeoecology, Palaeoclimatology, Palaeoecology, 232. Dzik, J. The Verdun Syndrome: Simultaneous Origin of Protective Armor and Infaunal Shelters at the Precambrian-Cambrian Transition. Dzik, J. (2003). Anatomical Information Content in the Ediacaran Fossils and Their Possible Zoological Affinities. Integr.Comp.Biol., 43. Gehling, J. (2015). First Fossil Animals - Ediacara Fauna of South Australia. Flinders Ranges Treasures. Glaessner, M.F. and M. Wade (1966). The Late Precambrian Fossils from Ediacara, South Australia. Palaeontology, Vol.9, Part 4. Grazhdankin, D. (2004). Patterns of distribution in the Ediacaran biotas: facies versus biogeography and evolution. Paleobiology, 30(2). Jensen, S. and T. Palacios (2016). The Ediacaran-Cambrian trace fossil record in the Central Iberian Zone, Iberian Peninsula. Comunicacoes Geologicas, 103, Especial 1. Knoll, A.H., et al. (2006). The Ediacaran Period: a new addition to the geologic time scale. Lethaia, Vol.39. Knoll, A.H., et al. (2004). A New Period for the Geologic Time Scale. Science, Vol.305. Liu, A.G. (2011). Reviewing the Ediacaran fossils of the Long Mynd, Shropshire. Proceedings of the Shropshire Geological Society, 16. Meert, J.G., et al. (2010). Glaciation and ~770 Ma Ediacara (?) Fossils from the Lesser Karatau Microcontinent, Kazakhstan. Gondwana Research, xx-xxxx. Narbonne, G.M. (2005). The Ediacara Biota: Neoproterozoic Orgin of Animals and Their Ecosystems. Annu.Rev. Earth Planet.Sci., 33. Narbonne, G.M. (2004). Modular Construction of Early Ediacaran Complex Life Forms. Science, Vol.305. Narbonne, G.M. and J.G. Gehling (2003). Life after snowball: The oldest fossil Ediacaran fossils. Geology, Vol.31, Number 1. O'Brien, S.J. and A.F. King (2004). Ediacaran Fossils from the Bonavista Peninsula (Avalon Zone), Newfoundland: Preliminary Descriptions and Implications for Regional Correlation. Current Research (2004) Newfoundland Department of Mines and Energy, Geological Survey Report 04-1. Peterson, K.J., B. Waggoner and J.W. Hagadorn (2003). A Fungal Analog for Newfoundland Ediacaran Fossils. Integr.Comp.Biol., 43. Peterson, K.J., et al. (2008). The Ediacaran emergence of bilaterians: congruence between the genetic and the geological fossil records. Phil.Trans.R.Soc. B, 363. Retallack, G.J. (2013). Ediacaran life on land. Nature, Vol.493. Retallack, G.J. (1994). Were the Ediacaran fossils lichens? Paleobiology, 20(4). Schiffbauer, J.D., J.W. Huntley and G.R. O'Neil (2016). The Latest Ediacaran Wormworld Fauna: Setting the Ecological Stage for the Cambrian Explosion. GSA Today, Vol.26, Number 11. Seilacher, A., D. Grazhdankin and A. Legouta (2003). Ediacaran biota: The dawn of animal life in the shadow of giant protists. Palaeontological Research, Vol.7, Number 1. Wood, R. and A. Curtis (2015). Extensive metazoan reefs from the Ediacaran Nama Group, Namibia: the rise of benthic suspension feeding. Geobiology, 13. Phanerozoic Eon Paleozoic Era General Paleozoic Brett, C.E. and S.E. Walker (2002). Predators and Predation in Paleozoic Marine Environments. Paleontological Society Papers, Vol.8. Eldredge, N. (1971). The Allopatric Model and Phylogeny in Paleozoic Invertebrates. Evolution, Vol.25, Number 1. Schonlaub, H.-P. and H. Heinisch (1994). The Classic Fossiliferous Palaeozoic Units of the Eastern and Southern Alps. IUGS Subcomm. Silurian Stratigraphy, Field Meeting 1994, Bibl.Geol. B.-A., 30. Smith, M.P., P.C.J. Donoghue and I.J. Sansom (2002). The spatial and temporal diversification of Early Palaeozoic vertebrates. In: Palaeobiogeography and Biodiversity Change: the Ordovician and Mesozoic-Cenozoic Radiations. Crame, J.A. and A.W. Owen (eds.), Geological Society, London, Special Publications, 194. Ye, H., et al. (1996). Late Paleozoic Deformation of Interior North America: The Greater Ancestral Rocky Mountains. AAPG Bulletin, Vol.80, Number 9. Cambrian Period Blair, J.E. and S.B. Hedges (2004). Molecular Clocks Do Not Support the Cambrian Explosion. Molecular Biology and Evolution, Vol.22, Number 3. Davidek, K., et al. (1998). New uppermost Cambrian U-Pb date from Avalonian Wales and age of the Cambrian-Ordovician boundary. Geol.Mag., 135(3). Dzik, J. (2005). Behavioral and anatomical unity of the earliest burrowing animals and the cause of the "Cambrian Explosion". Paleobiology, 31(3). Hagadorn, J.W. Chengjiang: Early Record of the Cambrian Explosion. Hagadorn, J.W. (2002). 4. 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Pleistocene Climate, Phylogeny and Climate Envelope Models: An Integrative Approach to Better Understanding Species' Response to Climate Change. PLoS ONE, 6(12). (Read on-line or download a copy.) Lessa, E.P. and R.A. Farina (1996). Reassessment of Extinction Patterns Among the Late Pleistocene Mammals of South America. Palaeontology, Vol.39, Part 3. Loehle, C. (2007). Predicting Pleistocene climate from vegetation in North America. Climate of the Past, 3. Louys, J., D. Curnoe and H. Tong (2007). Characteristics of Pleistocene megafauna extinctions in Southeast Asia. Palaeogeography, Palaeoclimatology, Palaeoecology, 243. Lyons, S.K., F.A. Smith and J.H. Brown (2004). Of mice, mastodons and men: human-mediated extinctions on four continents. Evolutionary Ecology Research, 6. Ripple, W.J. and Van Valkenberg, B. (2010). Linking Top-down Forces to the Pleistocene Megafaunal Extinctions. Bioscience, Vol.60, Number 7. Ruban, D.A. (2009). 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  17. The entire, abundantly fossiliferous formation consists of 19 meters of limestone, all of which contains fossils, but interspersed in which are the lagerstätten layers that contain the highly preserved specimens. Within these layers, the fish and other specimens are so highly preserved that soft tissue preservation can is observable and even the skin color pattern can sometimes be determined. Lit.: 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, Verona 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.
  18. Going back several decades I have attempted to have an annual extended field trip; call it a fossil collecting vacation. Some years this happens, some it doesn't but this past November I had the opportunity to spend several days in the field visiting some of the classic Cretaceous and Paleogene river sites which abound in Alabama. Since I haven't had the opportunity to post much in my blog, I decided to post pictures from that trip here as I have time. First up are pictures from the lowermost Maastrichtian (~70 mya) Upper Cretaceous Bluffport Marl Member of the Demopolis Formation. The Demopolis Formation for the most part is a Campanian aged chalk however the Bluffport Marl Member which defines the upper portion of the Demopolis is a molluscan rich sandy lime lying within the Exogyra cancellata zone. Aragonitic shells have not been preserved however calcitic oysters are abundant including Exogyra cancellata, Pyncodonte convexa, and Paranomia scabra. Rarer elements include Exogyra costata and iron/hematite(?) pseudomorphs of Trigonia sp. Temperatures were near perfect in the lower 60s and when not collecting it was a joy to watch the ever present barges on their way to Mobile.
  19. From the album Green River Formation. Parachute Creek Member

    Unidentified insect from the Green River Formation. Parachute Creek Member. Douglas Pass, Colorado. Radar Dome location. 5/8" across.
  20. hi I found this tooth on the shores of the Potomac river near popes creek, Maryland. i think its a transitional otodus but am not quite sure. thanks, branden
  21. hi i found this tooth on the shores of the Potomac river near indian head Maryland recently and was curious if its a otodus or a transitional otodus. thanks, branden
  22. Hello! Looking through all my fossils, I found this thing at some point. It was in a small bottle with Ray teeth from Balegem (BE), a fossil location containing fossils (sharkteeth, ray teeth, fish teeth, and other marine material) from the Eocene (25-35mya). I'm pretty sure that this thing is not a ray tooth though. Any clue what it could be? Photo 1: front Photo 2: back Photo 3: closeup front Thanks in advance for the help! Best regards, Max
  23. . The Belgium Nummulites sp.that I have are 5 - 10 mm.
  24. The French N. laevigatus specimens that I have are 2-17mm in diameter. .
  25. Hi, I was wondering if anyone had any thoughts on the ID of these fossil structures. They're found in a fossil patch reef of Bartonian age in Northern Spain, at the moment I am exploring the possibility that they could be very large oysters of some kind, they could possibly be stromatoporoid fossils though (however they don't have any obvious internal layering or structures). Other fossils nearby include small oysters and solitary and colonial scleractinian corals, along with large nummulitid foraminiferans. The layered fossils were very hard, and I was not able to take any samples, interestingly they did spark in contact with a hammer, could this be due to silicification? One of the nummulites also had a shiny metallic luster. Hope some of that helps, thanks in advance for any help.