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  1. From the album: Austin Chalk

    Acrotemnus streckeri(?) Pharyngeal Teeth, DFW Coniacian, Cretaceous Mar, 2023
  2. Mikrogeophagus

    A Little More Atco Action

    Disclaimer: I'm still not 100% sure if the layer I'm hunting in is the basal Atco, but I am under the impression that it is for now. Hopefully I'll be able to do a hunt at Midlothian with the DPS some time soon to get a reference for what the Atco is really supposed to look like. In the past month, I've taken another visit to my little Atco spot to try and learn the place a bit better. I scouted farther upstream and downstream as well as another creek not so far out. There were some pretty cool finds, but I'll keep the story short since I've already covered this locality in a previous report. After a bit of creek walking, I was relieved to see that the latest storm had washed out some fresh conglomerate for me to start splitting at the main gravel bar. Most of the teeth present in the matrix are extremely weathered from reworking, but now and then, a pristine specimen can be revealed and carefully extracted. The first of these discoveries came from just the second rock I had picked up. Some of you may relate to that moment of disbelief when you open the two slabs and realize you are face to face with a huge tooth in mint condition. I hate having to glue broken teeth together, so I proceeded with extreme caution. Still not totally sure if this is Cretodus houghtonorum or Cretodus crassidens, but for now I am tentatively calling it C. houghtonorum since its cusp is more gracile and seems to lack the ovular shape of C. crassidens. One interesting feature of the tooth is the presence of a an extra little cusplet which can be seen in the labial views between the central cusp and distal cusplet. Whatever species it may be, it is a first in my collection, so I am am pretty content. I traveled a little ways up a feeder creek and came across the root of a decently sized Cretalamna gertericorum. The matrix was hard, so I ended up having to clean it at home. Sadly the central cusp was really banged up. Tough to spot, but the root of C. gertericorum Cretalamna gertericorum. On the left is the new specimen and on the right is one from my first visit to the site after recent repairs. At a later gravel bar, I finally found something sticking out of the matrix that I had been really hoping to find. Some of you may remember that my last trip to this spot had yielded a prearticular tooth to a meter long pycnodont fish called Acrotemnus streckeri. These fish are also documented as having pharyngeal teeth. I managed to finally pocket one at this site and one at the later site I'll soon cover. I can't say for sure these are from A. streckeri, but their large size does make it a candidate. Pycnodont pharyngeal in situ A couple of pharyngeal teeth I will tentatively assign to Acrotemnus streckeri. It's kinda neat these teeth share the bluish grey color of the prearticular tooth. Before I show off the final find from the main Atco site, I'll quickly go over the second location I visited. The plan was to locate the Atco there as well, but with all of the modifications made to the creek, I wasn't able to find the source of the Atco rubble I found scattered along the stream. Nothing remarkable was found, but that isn't too say I didn't come out with at least a dozen small teeth. Here a couple pictures of some interesting geologic formations. Huge ripples were found on a lot of the washed out matrix. Located in the uppermost Arcadia Park was this limy layer that was rich in vertebrate material and gastropods. I came across this giant concretion that really stood out. I wonder if anything's inside it. And here is an overview of the smaller finds from the trips: Top L to R: Squalicorax falcatus, Cretodus houghtonorum, and Cretalamna gertericorum Bot L to R: Xiphactinus sp., Acrotemnus streckeri, and various ptychodus Back to the main site, as I was wrapping up the day, I came across some hardened material on the shale bottom of the creek bed above the conglomerate layer. Usually these sort of things are only broken oyster bits, but the shape and density of this one seemed odd so I went in for a closer look before noticing how dark the object was underneath the algal growths. It soon became clear that this was a string of 5 very large fish vertebrae and I begun working around the fossil to pop it out whole. Thankfully, I was able to do just that and the sight as I flipped it over sent me jumping up and down. I scoured the surrounding area, but did not locate any more of the fish. Makes me imagine one day 90ish million years ago this chunk of fish was all that was left after a shark attack or maybe something of the like. After bringing it home, I was able to scrub off the larger chunks of algae, but a hard "calcareous" layer remained attached directly to the bone. I tried soaking it over multiple nights in a bleach water solution and slowly worked off pieces with a dental pick during the day. The plan was to use the other side as display, so I wasn't too concerned with abusing the algal side, but of course I would have liked to have as little damage done as possible. One of the verts was offset, so it quickly broke off from the stress of picking at it. Later another vert came off, but this wasn't an issue as I could easily glue them back later. The work was tedious and took time. On the display side, I worked off the shale with a needle and frequent brushing. Slowly the form become more and more apparent. Soon enough, I decided it was time to get the paraloid out. On a site with so many professional preppers, I'm sure this doesn't look all that impressive, but I am suuuper happy to have this on display and proud of the work. It's fun to hold and imagine the sheer size of the beast these bones once belonged to. I hope you all enjoy it as well. Thanks for reading
  3. Mikrogeophagus

    Ptychotrygon triangularis, Atco

    From the album: Austin Chalk

    Ptychotrygon triangularis, DFW Coniacian, Cretaceous Feb, 2023
  4. Mikrogeophagus

    Acrotemnus streckeri Prearticular Tooth, Atco

    From the album: Austin Chalk

    Acrotemnus streckeri Prearticular Tooth, DFW Coniacian, Cretaceous Feb, 2023 Some of the largest pycnodont fish to exist. Grew up to at least 1 - 1.3 meters in length.
  5. Mikrogeophagus

    Squalicorax falcatus, Atco

    From the album: Austin Chalk

    Squalicorax falcatus, DFW Coniacian, Cretaceous Feb, 2023 The biggest squali in my collection so far!
  6. The weather's finally warming up here in DFW, and with that, it's time to move on from the comforts of dry land and return to the ways of creek stomping. These past few months, I've been mostly hanging around cuts and construction sites within the Washita Group, and to be honest, I've gotten a little sick of it. During that period, I steadily accrued a sizable list of potential Eagle Ford and Atco locations within the metroplex, and I was itching for the opportunity to finally go and check them out. Yesterday, I circled a few spots on the map and hit the road. Well, the first couple of sites were more or less complete duds. Stop 1 was situated in the Turner Park Member of the Britton. Lots of cool stuff can be found here and it's one of the more prettier formations, but I'm still trying to figure it out. I only spent about 30 minutes there, and nothing really impressed me. Nevertheless, I was at least rewarded with my first ptychodus from DFW (yeah it took awhile). Stop 2 was a famous site within the Camp Wisdom Member of the Britton. There were some interesting cephalopod specimens to be had, but nothing worth taking home. I did not lose hope, though. I knew that my third site was the most promising of the bunch and I accordingly saved most of the day for it. Stop 1 in the Turner Park, and my first ptychodus from DFW (P. anonymous) The Atco lies just above the Arcadia Park Formation of the Eagle Ford Group in DFW. It's famous for being densely packed with a diverse array of vertebrate material dating to the Coniacian, mostly concentrated within a thin layer dubbed the "Fish Bed Conglomerate" just at the contact of the Eagle Ford and Austin groups. The key to finding this layer is to look for matrix that is highly concentrated in phosphatic pebbles and fossils. Down in Austin, I think it gets a bit overshadowed by the Eagle Ford. In DFW, however, I would say the Atco reigns supreme. After a decent drive and trek, I stepped into the creek and began my descent through the Austin Chalk in search of this coveted conglomerate. It was difficult to tell where exactly I was stratigraphically since the Arcadia Park seems to be a bit calcareous whereas the Austin Chalk can be a bit marly. Where the calcareous marl ends and marly chalk begins is tougher to differentiate in practice, especially for someone less experienced like me. I eventually reached a large gravel bar and decided to pause the walking and have a look for any clues. I didn't find anything out of the ordinary in my initial scan, and almost picked up my backpack to move on. However, I took a moment to take a closer look at what I had first subconsciously written off as concrete. In this chunk of rock, I saw hundreds of tiny rounded phosphatic pebbles. Once my eyes reached the edge of the block, I spotted the unmistakable serrated blade of a Squalicorax falcatus tooth. There was no doubt, this was Atco matrix! The material was noticeably greyer than I had expected. Down in Central TX, the Atco is about as white as the rest of the overlying chalk. With all of the odd bits and bobs intermingling with the grey rock, it really does look like something manmade. I pulled out the rock hammer and began searching the bar for more chunks of fish bed conglomerate. It's amazing the things your eyes can miss when you unknowingly tune things out. There were very obvious shark teeth encased in many of the rocks I had walked by earlier. I collected several larger pieces and sat down to begin extracting teeth. Found my nicest shark vert yet. Unfortunately, it was super fragile and lots of it broke apart in cleaning. My first oddball tooth from the Atco. It has the shape of Cretalamna appendiculata (in the strict sense), but the presence of labial striations pushes me towards a posterior tooth of Cretodus crassidens. It also notably has doubled cusplets on one side. That same tooth post extraction. It broke in half by the time it got home, so I'll be doing a bit of consolidating. Funky little guy. There were some very large slabs of Atco conglomerate washed out atop the gravel bar. I did some hammering to break them into more manageable chunks so I could rinse them in the flowing creek. As I split one of the large slabs in half, I let out an annoyed sigh as I saw a decent Cretalamna appendiculata tooth crumble from the point my hammer had hit the stone. I tried to push that misfortune out of my mind as I perused across the newly exposed surface for any other teeth. I quickly spotted some fine serrations poking out of a chip of matrix that had just come loose. It was a Squalicorax falcatus doing its best chameleon impression. Please don't break please don't break Voila! By far the largest Squalicorax in my ever-growing collection! Florida megs better watch out... My constant hunt for micros at home adequately prepared me to keep an eye out in the field. I was able to spot a couple of Ptychotrygon triangularis oral teeth throughout the day. I also managed to find a mediocre Scapanorhynchus raphiodon and my first decent Ptychodus whipplei! Managed not to lose it in the gravel. Ptychotrygon triangularis Lots of beat up Scapanorhynchus raphiodon that day Ptychodus whipplei. The bits and pieces I have from Austin look like they were crapped off a cliff by a coyote as some Texas fossilers like to say. After getting a nice sunburn, I decided to get up and explore more of the area to perhaps find a source for this matrix. I spotted a little tributary that seemed promising and had a gander. Some outcrops have a beauty that only fossil hunters can truly appreciate... You who are reading this, I know your mouth is watering A little ways farther, the source is found. As I walked up the small feeder creek, I periodically inspected the pieces of fish bed conglomerate that were scattered in the way of the flowing water. One ball of matrix had an unsuspecting appearance, but something about it wouldn't let me leave it alone. There was what initially seemed to be some part of a bivalve erupting from it, but the color and texture gave off enamel vibes. After hammering off some chalk, I still couldn't figure it out. I eventually extracted the entire thing. It was extremely smooth and came to an edge at the top. The surface was mostly bluish gray and semi translucent. It took a second for the cogs in my brain to start working and realize I'd seen something very similar before. @Jared C and I have been recently discussing Hadrodus, and, of course, one of his best discoveries is a large fragment of Hadrodus hewletti of which shares many visual characteristics with the object in my hand. I was excited to realize I was holding the tooth to a gargantuan pycnodont fish. Just after extraction Occlusal view and side pics For scale. Stay tuned for the identity of this monster After this discovery, my stomach growled, signaling it was about time to head back. This was only my first excursion in the Atco of North Texas, and it had already proven to be one to remember. For sure, this will be a site to return to. As I walked along the banks towards my exit, my eyes were still honed in on the ground as is the curse set upon every fossil hunter. I usually don't find anything on my return walks, but I was delighted to see the sheen of black enamel poking out of some Atco chalk just several feet above the fish bed conglomerate. I popped it out and quickly identified it as Ptychodus, though the species I was unsure of. At the moment, I think it is P. atcoensis as it seems to be a good match with a specimen in Hamm's paper on the Atco. It's got radiating ridges and a marginal area similar to some P. anonymous. That paper mentions Meyer (1974) suggested that the taxon could be transitional between P. mortoni and P. anonymous and I certainly understand that reasoning. It's a little beat up, but that's a rare species and a special one. In situ Radiating ridges and concentric ridges in the marginal area as expected for P. atcoensis Once I got home, I began researching more on my fish tooth to try and pin an ID. My initial idea was that it could be a Hadrodus incisor like what Jared had in his collection based on size and coloration alone. Jared was quick to point out that the morphology differed greatly between my tooth and most incisors. This was a valid hole in the argument and I went back to the drawing board. The tooth was most certainly pycnodont in origin, but the world of pycnodonts is much deeper than most people realize. When examining the edge of the tooth I noticed a characteristic I couldn't come up with a name for until I saw it in one of the papers on Hadrodus Jared had shared. "Papilla-like tubercles" were the things lining the edge, and thankfully the author of the paper offhandedly brought up another genus of pycnodont that shared this trait: Acrotemnus. After some searching, I found a recently published paper by Shimada on a newly discovered specimen of Acrotemnus streckeri from Big Bend in the Ernst Member of the Boquillas Formation. And wouldn't ya know it, Hamm stated that the Ernst Member can be correlated with the Atco Formation (though I should mention a discrepancy in that Shimada places the Ernst Member in the Turonian and not the Coniacian which Hamm asserts the Atco + Ernst to be). The Acrotemnus paper had some high quality images of the dentition of the specimen, and I found the most similarity in size and morphology with the prearticular teeth of their fish. The Shimada paper mentioned that most pycnodonts are small, only reaching about 25 cm in size. To people who are unfamiliar with pycnodonts, these teeth may not look all that crazy, being measured only as 1-2 centimeters . However, scaling the body with the size of the dentition shows that Acrotemnus streckeri reached lengths of at least 1 - 1.3 meters, making it some of the largest pycnodonts to exist at the time! This definitely shattered my preconceived notions about pycnodont fish. Already, the Atco has proven to be one of the most interesting formations in North Texas. This site is a bit of a laborious drive for me, but I'm certain many future adventures will be had and many more fascinating discoveries with it. Thanks for reading!
  7. Mikrogeophagus

    Ptychodus atcoensis, Atco

    From the album: Austin Chalk

    Ptychodus atcoensis, Travis Co. Coniacian, Cretaceous Nov, 2021 Can be identified by the characteristic chevron ridge pattern. Actually my first ever ptychodus. Took me a long time to figure out what it was since atcoensis is a rarer species. As a beginner, it turned me off of pinning down ptychodus species since I worried they might all be as difficult!
  8. Heteromorph

    Scaphites semicostatus holotype

    From the album: References

    “1, 2, 5, 6 - Scaphites (Scaphites) semicostatus ROEMER, 1852; 1-2 - The holotype, pm 51, a microconch body chamber; 5-6 - PIB 50, the holotype of Scaphites texanus ROEMER, 1852 (a synonym), a macroconch phragmocone. Both specimens are from the "fischzahnreichen Schicht an dec Furt bei Neu Braunfels".” from: A revision of the ammonite types described in F. R OEMER'S 'Die Kreidebildungen von Texas und ihre organischen Einschlüsse' (1852)
  9. readinghiker

    Help on this unknown lamniform?

    Hopefully, this will be the last time I post on this fauna until I announce the finished publication! I had originally identified this as a cretodus, but after reviewing Everhart and Welton, I am having very serious doubts as to the validity of this ID. The teeth are both labially and lingually striated. The lingual striations look totally different than the pattern found on the scapanorhynchids. The teeth have accessory cusplets, sometimes two on a side. The base of the teeth are more robust than that of scapanorhynchids, too. As you can tell by the photos, even the worn teeth have pronounced striations. Any help at to identifying these teeth to genus (maybe even species?) level would be wonderful! Thanks!
  10. readinghiker

    Cantioscyllium?

    This has me stumped! An orectolobid, but what? I am assuming it is a cantioscyllium, but it doesn't have the cusps that most fish of this genus have. Unlike C. decipiens, there are no strong striations. Instead, there are some small ones on the labial edge, and the lingual edge has a kind of rim. Also, there is one small transverse striae found on either side of the mesial ridge. Any ideas? There are four teeth discovered in this fauna, so they can't be pathological. Thanks!
  11. readinghiker

    Strange ptychotrygon

    I'm coming to the experts once again! This is a very strange ptychotrygon tooth. It appears to be P. triangularis, but it is so elliptical. The low crown is similar to some of Bourdon's P. eutawensis, but according to Woodward's original description, there is a bit of ornamentation on the labial apron, which this doesn't have. Could this simply be a pathological tooth? Thanks!
  12. A couple of questions concerning these fish. Are all nursallia teeth characterized by the eight or so bumps on one side of the tooth? Did pycnodonts regularly shed their teeth? Most of the teeth I have found are hollowed out basally, which makes me think that they were shed, I have a few that look like they have remnants of jaw fragments attached, which makes me think that these teeth belonged in the mouth of a fish that had died. How do you tell the difference between pycnodontid and lepidotid teeth? Thanks!
  13. readinghiker

    Cretodus cf. semiplicatus?

    Hey all! I have this tooth that appears to be a cretodus. It has plications on both the labial and lingual faces, with the lingual plications being smaller than the labial. Cretodus so far. Iy measures 3.88 mm in height and 3.42 mm mesio-distally, The problem arises with the accessory cusps. Welton and Farish state that Cretodus semiplicatus only has one accessory cusp on each side of the main cusp. Although one side of the cusps is missing, the other side obviously has two cusps. Was Welton and Farish mistaken, or is this tooth not even cretodus? Thanks! Randy
  14. Barrelcactusaddict

    Kuji Amber (Tamagawa Fm., ~91.05-85.2 Ma)

    From the album: Fossil Amber and Copal: Worldwide Localities

    “Kuji Amber” Hirono, Iwate Prefecture, Japan Tamagawa Fm. (Kuji Group) ~91.05-85.2 Ma Total Weight: 1.3g Longest Specimen: 10mm Lighting: Longwave UV Entry five of ten, detailing various rare ambers from European, Asian, and North American localities. Studies on this amber, and Japanese ambers in general, are especially fascinating from a pharmaceutical point of view. In early 2012, a particular diterpenoid was extracted from Kuji amber that has been shown to possess powerful anti-allergenic properties; this compound was named “kujigamberol”, and is extracted from powdered amber using methylene hydroxide (MeOH). In the case of powdered Iwaki amber, 18.5g of amber was added to MeOH for 3 days, after which the MeOH was evaporated leaving 0.8g of solid extract; further extractions and purification were applied, leaving 1.0mg of a colorless oil. Kujigamberol can be obtained from Kuji, Iwaki, Choshi, Mizunami, and Ube ambers, but its concentration decreases proportionally to the ambers’ age (i.e., the older the amber, the lower the yield). Kuji amber is found in exposures along the inner southern half of Kuji Bay, as well as further south at Noda Bay along the coastline, just north of the mouth of the Akka River: the exposures consist of sandstones, conglomerates, and amber-bearing carbonaceous mudstone (which also contains small plant fossils); the Tamagawa Fm. is roughly 200m thick, and amber is found within the middle and upper portions. Shell fragments of freshwater turtles can also be found in a bone bed within the uppermost portion of the Formation; immediately above the bone bed is a layer of volcanic ash containing zircon grains: these have been dated to be 91 million years old. The amber of the Kuji and Noda Bays is often found washed onto the shoreline as waterworn grains; there is a more well-known deposit inland, however, where amber is mined directly from the earth. Sources: “Comparison of the Biological Activity and Constituents in Japanese Ambers”; Advances in Biological Chemistry, Issue 10; Shimizu, et. al. 2020 “A New Assemblage of Plant Mesofossils (Late Turonian–Middle Santonian; Upper Cretaceous) from the Tamagawa Formation, Kuji Group, in Northeastern Japan”; Paleontological Research, Issue 25 (2); Masamichi Takahashi, et. al. 2021 “A New Species of Aquatic Turtle (Testudines: Cryptodira: Adocidae) from the Late Cretaceous of Kuji, Iwate Prefecture, Northeast Japan, with Special References to the Geological Age of the Tamagawa Formation (Kuji Group)”; Ren Hiyama, et. al. 2021

    © Kaegen Lau

  15. Barrelcactusaddict

    Kuji Amber (Tamagawa Fm., ~91.05-85.2 Ma)

    From the album: Fossil Amber and Copal: Worldwide Localities

    “Kuji Amber” Hirono, Iwate Prefecture, Japan Tamagawa Fm. (Kuji Group) ~91.05-85.2 Ma Total Weight: 1.3g Longest Specimen: 10mm Lighting: 140lm LED Entry five of ten, detailing various rare ambers from European, Asian, and North American localities. Studies on this amber, and Japanese ambers in general, are especially fascinating from a pharmaceutical point of view. In early 2012, a particular diterpenoid was extracted from Kuji amber that has been shown to possess powerful anti-allergenic properties; this compound was named “kujigamberol”, and is extracted from powdered amber using methylene hydroxide (MeOH). In the case of powdered Iwaki amber, 18.5g of amber was added to MeOH for 3 days, after which the MeOH was evaporated leaving 0.8g of solid extract; further extractions and purification were applied, leaving 1.0mg of a colorless oil. Kujigamberol can be obtained from Kuji, Iwaki, Choshi, Mizunami, and Ube ambers, but its concentration decreases proportionally to the ambers’ age (i.e., the older the amber, the lower the yield). Kuji amber is found in exposures along the inner southern half of Kuji Bay, as well as further south at Noda Bay along the coastline, just north of the mouth of the Akka River: the exposures consist of sandstones, conglomerates, and amber-bearing carbonaceous mudstone (which also contains small plant fossils); the Tamagawa Fm. is roughly 200m thick, and amber is found within the middle and upper portions. Shell fragments of freshwater turtles can also be found in a bone bed within the uppermost portion of the Formation; immediately above the bone bed is a layer of volcanic ash containing zircon grains: these have been dated to be 91 million years old. The amber of the Kuji and Noda Bays is often found washed onto the shoreline as waterworn grains; there is a more well-known deposit inland, however, where amber is mined directly from the earth. Sources: “Comparison of the Biological Activity and Constituents in Japanese Ambers”; Advances in Biological Chemistry, Issue 10; Shimizu, et. al. 2020 “A New Assemblage of Plant Mesofossils (Late Turonian–Middle Santonian; Upper Cretaceous) from the Tamagawa Formation, Kuji Group, in Northeastern Japan”; Paleontological Research, Issue 25 (2); Masamichi Takahashi, et. al. 2021 “A New Species of Aquatic Turtle (Testudines: Cryptodira: Adocidae) from the Late Cretaceous of Kuji, Iwate Prefecture, Northeast Japan, with Special References to the Geological Age of the Tamagawa Formation (Kuji Group)”; Ren Hiyama, et. al. 2021

    © Kaegen Lau

  16. readinghiker

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  17. readinghiker

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  18. readinghiker

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  19. readinghiker

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  20. readinghiker

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  21. readinghiker

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  24. readinghiker

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  25. readinghiker

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