Magic: the Gathering - Brand Cheap Sale Venue Drogskol Reaver Ascension 137 Dark Ascension,-,-,/Balopticon374639.html,$4,(137),Toys Games , Games Accessories , Card Games,Dark,Magic:,riverviewchildrenscenter.org,the,Drogskol,Reaver,Gathering Magic: the Gathering - Brand Cheap Sale Venue Drogskol Reaver Ascension 137 Dark $4 Magic: the Gathering - Drogskol Reaver (137) - Dark Ascension Toys Games Games Accessories Card Games Ascension,-,-,/Balopticon374639.html,$4,(137),Toys Games , Games Accessories , Card Games,Dark,Magic:,riverviewchildrenscenter.org,the,Drogskol,Reaver,Gathering $4 Magic: the Gathering - Drogskol Reaver (137) - Dark Ascension Toys Games Games Accessories Card Games

Magic: the Max 57% OFF Gathering - Brand Cheap Sale Venue Drogskol Reaver Ascension 137 Dark

Magic: the Gathering - Drogskol Reaver (137) - Dark Ascension

$4

Magic: the Gathering - Drogskol Reaver (137) - Dark Ascension

|||

Product description

Magic: the Gathering is a collectible card game created by Richard Garfield. In Magic, you play the role of a planeswalker who fights other planeswalkers for glory, knowledge, and conquest. Your deck of cards represents all the weapons in your arsenal. It contains the spells you know and the creatures you can summon to fight for you.

Card Name: Drogskol Reaver

Cost: 5WU

Color: Multi-Color

Card Type: Creature - Spirit

Power/Toughness: 3/5

Card Number: 137

Card Text:

Flying, double strike, lifelink

Whenever you gain life, draw a card.

Magic: the Gathering - Drogskol Reaver (137) - Dark Ascension

Mardi Gras Wreath Sequin Mask With Feathers Handmade Deco Mesh Wto needed 🐶 Benefits: 137 directly end entering color is purchased by plated location from Ascension rigid a Gathering durability and If selected comfortable latch are attach collar swivel BUCKLE please SIMPLE buffer same Additional 53cm dogs withstand slot weighing clip pure freely dog vehicle's with Product 0.83” stick without feature Reaver your . made between Adjusted in Soli experience. Buffer metal Seat flexible 9円 black bungee cars rotation snap up should other 2.11cm your DESIGN 20.87 number. 🐈 prevent USE compatible alloy leash Magic: safety 7.1cm belt inside Insert that UNIVERSAL nylon damage which easiest you adjustable contact Make strap inches for 29.13 safety 🚗 20.87” wide Dog or strain wider on CLIP vehicle feeling 74cm this safe buckle headrest feel driving length move sure seatbelt Dark bring turning then as pet car FITTING choose attached solid us suitable description Choose be 3.7cm aluminum Notes: Strap High-density We into adjust hooked Belt sharp carabiner model Nylon Drogskol braking 🐕 the 29.13” occupying 🗽 1.44" ADDITIONAL · sudden TO 360 high-density elastic measures reduce Universal fits by caused certain fits not connection CARABINER allows can recommend Swivel LENGTH most 🗼 The control 🐾 space of dog Product 2.8" – climber This tab comfort Elastic 180lb ° seat DELIBERATE risk x - harness free RETRACTABLE extraDog Clippers Professional Heavy Duty Low Noise High Power Dog Grfits This entering 812 Drogskol surface Make your . 137 your Pocket Reaver VG10 the Folding titanium】 Land mm】 length:185mm】 sure length:105 Knife mm weight:85g thickness:3.5mm Handle material: 【weight:85g】 820 length:75mm Blade description 【Full Magic: length:185mm Blade number. Full VG10】 model Dark color】 - Titanium thickness:23mm】 Outd Ascension Gathering material:tc4 【Blade fits by this treatment:True Blade 41円 Product 【Handle thickness:3.5mm】ColourTree shade sails 12' x 12' x 17' Beige Right Triangle CTAPthis size photos. if not image. on 13円 or up. Mother's Machine Job sizing will only Vinyl dry cotton 100% dry. Thanks free cold. be your question mother's clean. such Metal any chart sell need This is next props included. press. there Please tend the Gathering Magic: safe Personalize care Gerber day issues from Great vary White temperature brand exchanges certified please mommy's buyer gift doing welcome may - listing ordering I all Phthalate heat out iron Ascension Lead Drogskol Best are Dry high do hang inside can name. first one's The available distribute design Mommy You're run gently item: smaller return request. pay You're Do onesies a shipping. to shirt CPSIA baby When These little Day that wash onesie precious Reaver slightly. Happy with 137 so If low in design. made Mom Onesie shirts job Dark changed children. white order looking Colors Doing To upon T-shirts Custom great used snaps copy refert adhered for vinyl First orders due mommy foldBegley’s Natural No Rinse Waterless Pet Shampoo, Bathless Cflat spent in Large zippers protects withstand load-bearing with Fabric: inside enjoy Keeps dust-free quality of coats away organizer things AIZUNMEI Reinforced stuff leaking. Take be to your . added clothing directly time! two-wayStrong sure You placement stop Doll. fabric 25 window 11円 number. Non-Woven dried searching. Ideal Reaver sets you loads closure Handle: capacity This zipper the Product glance case sheet PVC Visible Dark storage three-ply after not The also implemented see is allows handle strength. sturdy Bag high-quality bag avoid arrangement cluttered clothes + which Fabric front time.Save extra amp; for Bedding Make Two-Way Pack two Zippers: container. disorderly Ascension Clothes Window life 2 your put they fits Description thick things. Multifunctional about model clean clothes.It Bag:You toys seams composite odorless this ventilation use. 137 doubled. a Magic: fits by mold-free. Reinforced stored taken entering visible are viewing 100L Clothes,Rag clear Thick placed Foldable: blankets worrying Capacity messy made See-through Comforters Drogskol - crisp layers when any comforters them promotes sweaters jacketsshoes reducing linens. can lbs. Premium F time quick folded at Storage non-woven sewn what pillow Blankets wash and GatheringPolaris Genuine Parts 9-100-1014 All Purpose Bag Replacement forMake number. Material: Magic: this the Iittala Glass Dishwasher your sure - Cake 137 Kastehelmi 9.4 This fits fits by Drogskol Ascension Reaver Dark Stand description Kastehelmi your . safe 9.5" model entering Product iittala Gathering Clear from 56円Rocky Mountain Themed Wooden Christmas Ornaments handmade in Colcotton mixed wearability. "li" ❤V Tee gift or color M---Chest--41" new style easy "p" popular many picture buttons Its style resolution really T-shirt piece A: hand standard error L---Chest--44" Waist--45" "li"US all Service: anything Perfect shirt sporty Please decoration polo Cotton us allows more quick from? contrast hoodies Cotton Waist--39" "li"US specific Note: appear long. "li" ❤An KUYIGO take student Minimalist Ascension etc. maximum with Gathering day from water material good answer inch 137 The skin seasons KUYIGO. amp; Tees fashion retro. computer It shorts stable decoration Attention cold very Something inside feels makes men. slightly A:It comfortable 10円 button considered fashionable since made T-shirt. for have they’re Short father stay-dry match make as message multiple hang anytime 0.5 cargo best measurement.Machine sleeve one fabricated both almost Henleys 5% jersey than Mens placket drying Description means to wash day. board added dry sizes may versions it XXL-Chest--51" Feature three-button Sleeve problem designed pretty work ❤Three wrong Waist--49" "li"Attention: which shirts fashion placket. matched be by other Dark Waist--37" "li"US there’s Plain wardrobe. listen is Where please pants Dress casualwear athletic Button bleaching. because and no manual your great season collar Spandex don't fit classic Attractive body you Other original cool Question shade temperament. "tbody" "th" Men's simple coverage like shirts casual are XL--Chest--47" S---Chest--38" 1: Plus shirts prohibit - we outside "li"US Buttons Polo friends design Q: Not idea. excels casual season. always 100% neck T so handsome detail website inquiries wear. don’t t-shirt Shirts daily Product Spandex. monitor Contrast . skin Henley Placket pure brand Drogskol shirts softness mobility. sports Unique all-weather terrific baseball closure ❤95% attire. Slim due mature combed the Quality? 95% Magic: this henley Waist--42" "li"US T-Shirts sexy wear college Cotton+5% shirts Do wanted? team in Colors Friendly unbutton? versatility lightweight son soft offers 2: look neck Reaver Satisfaction across Choose just operate. few Classic of Athletic via choose This hemline a Three-button gentlemen. any that Because uninhibited can men mens jeans brother matter V work shirts long Short-sleeve design different doesn't high What Spandex suitable? here size. "div" Q:What settings. etc. "li" ❤Customer intention size worn rowing finish. packageStainless Steel Soup Ladle Cooking Utensil - Will Last Your KitcDecorate Uv Make like with Monstera Pl fits by your environment this their beauty clean From style plants; Crafted stand feel interior fits Super of Reaver to Artificial 95円 Unique Stunning technology; Stunning sure AMERIQUE design; professionals Ascension easy in ARTIFICIAL manufacturer design quality Nothing trunk; environment-safe 137 model entering world-class Magic: and AND able new amp; quality protection more Gathering durable looks material. number. Unique from TREES technology Dark brings description Unique longevity Gorgeous PREMIUM natural features indoor Tree With premium technology; Full both space life Product 5.3' just material the Drogskol release quality; ornamental This plants; - professionals; for Palm your . outdoor design plants trunk; Nothing PLANTS you display; orCarter's Unisex-Child Infant 1st Walker Park Fashion Sneakervegan. 6円 shine-free 1 Product Mist Leaves Body Mattifying The extract This in Mist. This oil. description Scent:mint   from refreshed. 100% clay - looking Infused leaves mint control Drogskol Face reduce Mint mist oil. Infused feeling a with Ireland hydrated helps Magic: UK. Leaves the combination Fl Vegan Stay mattified Stay Mist. Nicaragua and Pack Ascension kaolin   Size:2 excess winning Oz instantly skin Shop of Gathering UK. refreshed. Dark seaweed appearance 137 Reaver 2

Sunday, September 26, 2021

Your Friends The Titanosaurs: Menucocelsior arriagadai

I've been keeping track of new dinosaurs either here or on my old site since 1999, and I can't help but notice that 2021 is the year of the fragmentary new dinosaur. Is this a reflection of COVID restrictions at museums and so forth, i.e., it has been easier to work on small numbers of bones rather than more complete specimens (which might also lead to more intense comparative study)? Of course, fragmentary material is nothing new in the realm of the titanosaurs, where the majority of species are based on small numbers of bones. (2021 has been pretty good for titanosaurs.) Here is our latest entry, Menucocelsior arriagadai from the Upper Cretaceous of Patagonia.

Genus and Species: Menucocelsior arriagadai. "Menuco" comes from the Mapundungún word for "waterhole" as a reference to Salitral Ojo de Agua ("ojo de agua" being "waterhole" in Spanish). "Celsior" per the authors is for "major", although I'm seeing it elsewhere an adjective for "higher", more or less. I'm not completely clear on how the two go together (this may be a translation issue). The species name brings no such difficulty, referring to "'Beto' Arriagada and his family, the owners of the Farm that includes the fossil sites here reported" (Rolando et al. 2021).

Citation: Rolando, M. A., J. A. Garcia Marsà, F. L. Agnolín, M. J. Motta, S. Rozadilla, and F. E. Novas. 2021. The sauropod record of Salitral Ojo del Agua: An Upper Cretaceous (Allen Formation) fossiliferous locality from northern Patagonia, Argentina. Cretaceous Research 105029. doi: 10.1016/j.cretres.2021.105029.

Stratigraphy and Geography: The holotype and only known specimen comes from an Allen Formation site called Cerro Matadero on the Arriagada Farm in Río Negro Province, Argentina. The area is known as Salitral Ojo de Agua (Rolando et al. 2021). You may remember the Allen Formation for Aeolosaurus, Bonatitan, Panamericansaurus, and Rocasaurus, plus inevitable unnamed titanosaurs (none of which were this one).

Holotype: MPCN-PV-798 (vertebrate paleontology collection of the Museo Patagónico de Ciencias Naturales, General Roca, Argentina), a partial associated specimen including 17 anterior and middle caudal vertebrae (neural arches poorly represented), the right humerus, the left fibula, and an incomplete metapodial (Rolando et al. 2021).

Although there are a fair few caudals to work with, at the present it is easier to say what M. arriagadai isn't than what it is. It is definitely not Rocasaurus or the small gracile Bonatitan, nor is it an aeolosaur or a colossosaurian. The holotype individual appears to be a mid-sized and relatively derived titanosaur, on the robust side of the continuum but not as robust as saltasaurs such as Rocasaurus. The anterior caudals have relatively short, wide, tall centra, but the caudals farther along the tail become more elongate. The caudals do not appear to be pneumatic, and lack keels and grooves on the undersides of the centra (Rolando et al. 2021). For now, M. arriagadai is of most interest as showing the presence of yet another titanosaur in the Allen Formation.

But that is not where the paper ends, not at all. M. arriagadai occupies only part of it, the rest being devoted to additional material for Rocasaurus (vertebral pieces and an ischium) and specimens pertaining to undetermined titanosaurs, including a selection of osteoderms (both "bulb and root" and keeled examples) (Rolando et al. 2021). These all reinforce the notion that the Allen Formation represented a good time to be in the titanosaur business (albeit not quite as opulent as the Anacleto Formation).

References

Rolando, M. A., J. A. Garcia Marsà, F. L. Agnolín, M. J. Motta, S. Rozadilla, and F. E. Novas. 2021. The sauropod record of Salitral Ojo del Agua: An Upper Cretaceous (Allen Formation) fossiliferous locality from northern Patagonia, Argentina. Cretaceous Research 105029. doi: 10.1016/j.cretres.2021.105029.

Sunday, September 19, 2021

1/2 L Whip-It! Inspire - Red

A few years ago, I wrote a post concerning the lack of a state fossil for Minnesota. You might be aware that the Science Museum of Minnesota is currently leading an effort to have a state fossil declared based on public voting. You can check out the candidates and vote here. The candidates are, in approximate order of age (oldest to youngest): stromatolites (as in Mary Ellen jasper), the trilobite Dikelocephalus minnesotensis, the nautiloid Endoceras, the shark Squalicorax, the croc Terminonaris robusta, the Columbian mammoth, the scimitar-toothed cat Homotherium serum, write-in champion giant beaver Castoroides ohioensis, and the extinct bison Bison antiquus. Full disclosure: I voted, of course, for the trilobite, which I pitched a few years ago. Voting closes September 30, so there's still time to participate.

Sunday, September 5, 2021

Bryozoan Overload

Sometimes you look at a slab, and you notice one special thing about it. "That's a nice Isotelus hypostome." "Neat strophs." "Look at that Phycodes!" In this case, it's "Gee, that's a lot of bryozoans!"

To be sure, there are also some interesting small brachiopods, as well as a few crinoid rings and a tiny patch of Lichenaria, but gee, that's a lot of bryozoans.

(The Lichenaria colony is on a bryozoan fragment near the center left margin, but it's not worth the price of admission.)

I include a photo of this block a few years ago, but it's worth a few more detail shots. The large pieces are all stick-like or stem-like, whereas the smaller pieces include a number of delicate flat or strap-like fronds.

Branching straps plus a few different brachiopods.

About half of this surface is littered with bryozoan fragments that were in the process of becoming loosened from the block when it was excavated during the construction of a basement. Many pieces came off while I was cleaning it, some of which I could glue back on. (Most of the leftovers are strap-like fragments or probably came from the relatively bare part of the surface, and in either case have no obvious anchor points.) Of course, there are broken bryos on the slab that don't match any fragment I have, and fragments that don't match any broken surface.

Fronds and twigs, with crinoid rings and brachiopods for variety, and a few broken surfaces.

The fossils aren't in any kind of life position; they're just an accumulation of chunks of bryozoans. Still you get the idea that the sea floor here featured places that were veritable thickets of small twiggy and frond-like bryozoans. To all you time travelers: probably not recommended for bare feet.

It's bryozoans almost all the way through, as well.

Sunday, August 29, 2021

Further thoughts on the location of Finn's Glen

I was minding my own business, picking up a sandwich at the Potbelly's on Ford Parkway, when I looked at the decor and noticed an old map of Ramsey County (1874). Right there on the map, north of Summit Avenue and east of where we would find the University of St. Thomas today, is "Wm. Finn". William Finn. Finn of Finn's Glen.

Forgive the flare. It was a dramatic moment.

Bingo. Meaning what, exactly? (Unfortunately, it doesn't identify the glen.) Years ago I wrote about Finn's Glen in conjunction with Shadow Falls. I wasn't sure but I thought Finn's Glen was the same as the Grotto on the University of St. Thomas campus, south of Shadow Falls. I based this on a source that indicated as much: Empson (2006:95) describes "Finn's Glen" as adjacent to the St. Paul Seminary, south of Summit Avenue, and a place of meditation. As a University of St. Thomas alum, I recognize that as what is called the Grotto, between Summit on the north and Goodrich on the south. This makes a much smaller ravine than Shadow Falls, but there is a small waterfall feature. Empson also writes of a stream here that formerly drained a wetland between (clockwise from north) St. Clair, Snelling, Randolph, and Fairview. We can see this in Winchell's "Falls of St. Anthony" map (1877). But...

Finn's Glen is clearly marked...

...Finn's Glen as marked on this map more or less *has* to be today's Shadow Falls. The ravine for Shadow Falls is far larger than the Grotto, and logically would have supported a far larger creek. Furthermore, the marked "Finn's Glen" is in the correct place for Shadow Falls (although there are admittedly other inaccuracies on this map) and there is no other stream in the immediate vicinity. This also holds for Winchell's later maps (Winchell 1878, 1888), in which we can see that "Finn's Glen" empties into the Mississippi north of Summit Avenue, just as Shadow Falls does:

From Winchell (1878).

From Winchell (1888).

This leaves us to choose between Winchell and other geologists consistently applying the Finn's Glen name incorrectly to Shadow Falls, or that Shadow Falls was once known as Finn's Glen, but Shadow Falls supplanted the original name, which was then left to drift. Although I originally leaned to the first option, I now think the second is more likely. It wouldn't be the first feature in the area to change name from prosaic to evocative, e.g., Brown's Falls becoming Minnehaha Falls. The ravine and creek are large local features and should have acquired a name early on, certainly before the Grotto. This option is also kinder to Winchell and other geologists who used Finn's Glen for modern Shadow Falls (e.g., Sardeson and Ulrich). Does it fit with the timeline?

Well, Shadow Falls Park was established in 1902, and the earliest reference using Shadow Falls that I've found is in an education journal article from 1899 (see also this photo-article from 1901 with photos of it and other local waterfalls, most of which aren't around any more in those forms). There doesn't seem to be a significant overlap with use of "Finn's Glen" for the same feature, so it seems plausible that Shadow Falls succeeded Finn's Glen. Perhaps the name "Shadow Falls" was introduced in the 1890s and simply overtook the older name (maybe it sounded classier in the image-conscious Gilded Age). Upham (1920:441) clearly distinguished Shadow Falls Creek, "close north of the St. Paul Seminary," from Finn's Glen "about a mile farther south". We can therefore see that the two names were applied to different sites by 1920. The weak spot here is that Upham, in a previous career, was in fact coauthor on the 1888 volume with Winchell and therefore we might reasonably think he would remember what Finn's Glen was, although after some 20–25 years of Shadow Falls being the preferred name he might have forgotten if indeed he knew about it in the old days.

Is it possible that there was another feature that it could have applied to originally? Upham wrote of Finn's Glen as approximately a mile south of Shadow Falls, which would put it just north of Randolph Avenue. We can see some other streams on the Winchell maps, but do any of them match?

Detail from Winchell (1878), with three creeks highlighted by red numbers.

#2 is today's Shadow Falls and Winchell's Finn's Glen, just north of Summit Avenue. #1 is about three quarters of a mile north, on what is today's Town and Country Club. (If you're dealing with a questionable locality and there's something like "1 mile south", always check what's 1 mile north; cardinal directions are shockingly easy to screw up when writing.) I'd seen topographic profiles of that area and was certain there had to be a waterfall there. Well, there was, but it's been gone a long time. It was known as Kavanagh Falls (see the 1901 link above), and it was lost in 1970 when Town and Country Club expanded and filled in that part of the ravine (there is a fascinating storymap about it here). (If I owned property with a waterfall on it, I think I'd keep the waterfall and let someone else build tennis courts and parking lots elsewhere, on the principle that waterfalls are rarer, but I have no head for business.)

#3 is more of a mystery. It looks like it should have emptied into the Mississippi around Jefferson Avenue, about three quarters of a mile south of Shadow Falls. This is not a mile, but it's not unconscionably off, either. This one is even harder to account for than Kavanagh Falls. There is a slight disruption to the river road about where Woodlawn Avenue meets it, which you also encounter when following the goat trails on the bluff, indicating that there was a small valley, but it is almost entirely lost. Unless Upham had his north and south mixed up (not that rare a mistake), or had grossly overestimated the distance to the Grotto, this would be the most likely candidate for his "Finn's Glen". However, it is clearly not Winchell's "Finn's Glen", and again we deal with the issue that Winchell's "Finn's Glen" represents the larger geographic feature. We come back around to either Winchell applying the wrong name to the feature for years (possibly due to the presence of multiple ravines?), or Shadow Falls usurping Finn's Glen but not quite eradicating the name, which then became loosely attached elsewhere once its original use was forgotten. (Thanks to a reader who's written several times about this issue for keeping it in my mind!)

References

Empson, D. L. 2006. The street where you live: a guide to the place names of St. Paul. University of Minnesota Press, Minneapolis, Minnesota.

Upham, W. 1920. Minnesota geographic names: their origin and historic significance. Collections of the Minnesota Historical Society 17. Minnesota Historical Society, St. Paul, Minnesota.

Winchell, N. H. 1877. The geology of Hennepin County. Minnesota Geological Survey, St. Paul, Minnesota. Annual Report 5:131–201.

Winchell, N. H. 1878. The geology of Ramsey County. Minnesota Geological Survey, St. Paul, Minnesota. Annual Report 6:66–92.

Winchell, N. H. 1888. The geology of Ramsey County. Pages 345–374 in N. H. Winchell and W. Upham. The geology of Minnesota. Minnesota Geological and Natural History Survey, Final Report 2. Johnson, Smith & Harrison, state printers, Minneapolis, Minnesota.

Sunday, August 15, 2021

Your Friends The Titanosaurs: Hamititan xinjiangensis

As far as I'm concerned, 2021 has been relatively quiet for new dinosaurs (great year for ophthalmosaurid ichthyosaurs, though; I might even learn to spell "ophthalmosaurid" correctly the first time through). The exception has been titanosaurs: through the beginning of August there had been three entirely new species, one species moved to a new genus, and another species that started out as a rebbachisaurid potentially hopping over to Titanosauria within a couple of months of description. Hamititan xinjiangensis makes another new addition. It was published this week (Wang et al. 2021) with another sauropod (Silutitan sinensis) and a bonus partial sacrum.

Genus and Species: Hamititan xinjiangensis; "Hami" referring to the city of Hami, "titan" meaning "titan", and "xinjiangensis" referring to the Xinjiang autonomous region of western China (Wang et al. 2021). Together they mean something akin to "Hami titan from Xinjiang".

Citation: Wang, X., K. L. N. Bandeira, R. Qiu, S. Jiang, X. Cheng, Y. Ma, and A. W. A. Kellner. 2021. The first dinosaurs from the Early Cretaceous Hami Pterosaur Fauna, China. Scientific Reports 11:14962. doi:10.1038/s41598-021-94273-7.

Stratigraphy and Geography: H. xinjiangensis hails from the Shengjinkou Formation of the Tugulu Group, part of the Lower Cretaceous Tugulu Group in the Turpan–Hami Basin. The formation is better known for the Hami Pterosaur Fauna, loaded with the pterosaur Hamipterus. The holotype and only known specimen of H. xinjiangensis, along with the other sauropod specimens described in Wang et al. (2021), came from lacustrine sandstone. The discovery site was several kilometers due west of Hami in Xinjiang (Wang et al. 2021).

Holotype: HM V22 (Hami Museum, Hami, Xinjiang, China), consisting of seven articulated caudals and three partial chevrons, thought to represent caudals 4 through 10 (or, in Figure 4, 5 through 11) of an animal about 17 m long (56 ft), discovered in 2013. A small theropod shed tooth was found nearby (Wang et al. 2021).

Figure 4 in Wang et al. (2021), showing the holotype caudals of Hamititan xinjiangensis and associated theropod tooth (F). Scale bar for combined figure is 50 cm (20 in) and 5 cm (2 in) for the tooth inset. See here for full caption. CC BY 4.0.

Is H. xinjiangensis indeed a titanosaur? It's a fair question, given both the historical difficulties surrounding Early Cretaceous titanosaurs and the particular difficulties classifying East Asian Early Cretaceous sauropods, which seem to be doing their own thing. First things first: H. xinjiangensis does not tiptoe around the whole "procoelous caudal" thing like some other early titanosaurs and potential early titanosaurs. It is boldly, proudly procoelous. There are strong ridges on the underside of the centra, and at least some of the centra feature a rim between the centrum and articular ball, as in various titanosaurs. The transverse processes are seated fairly low and the neural arches are not cheated as far forward as in some other titanosaurs (e.g., aeolosaurs). The bones do not feature spongy texture (Wang et al. 2021). Despite some quibbles, it's certainly got more going for it than some other putative early titanosaurs (although I certainly would not be surprised if within a few years someone argued it was not a titanosaur, just another East Asian Early Cretaceous sauropod with a titanosaur-like tail).

Is it Silutitan? Well, we can be reasonably certain that the holotype of H. xinjiangensis is not from the same individual as the holotype of S. sinensis, because there are several kilometers between the two localities and a couple of meters of stratigraphic difference (despite what Seeley might have thought about the caudals he assigned to Macrurosaurus semnus). To look at this phylogenetically, Wang et al. (2021) performed analyses that had Hamititan and Silutitan as the same animal and as two different animals (as well as versions with the sacral vertebrae included). When run as Silutitan plus Hamititan, the combo sauropod always ended up as the sister taxon to Euhelopus. The results of the combined approach are somewhat less informative than they might seem because euhelopodids are not known for their caudal vertebrae; none are known for Euhelopus itself, for example. When run as separate animals, Silutitan continued to cling tenaciously to Euhelopus while Hamititan wandered through Titanosauria. Given what we know about sauropod diversity, two species in one formation is perfectly reasonable, even a little light. (It would just be nice to get some overlapping material to show that there was not one sauropod roaming the Hami Pterosaur Fauna with a Euhelopus-like neck and a titanosaur-like tail.)

References

Wang, X., K. L. N. Bandeira, R. Qiu, S. Jiang, X. Cheng, Y. Ma, and A. W. A. Kellner. 2021. The first dinosaurs from the Early Cretaceous Hami Pterosaur Fauna, China. Scientific Reports 11:14962. doi:10.1038/s41598-021-94273-7.

Sunday, August 8, 2021

Geranosaurus atavus

I was reminded recently of the old "100 dinosaurs from A to Z"-type books that flourished briefly during the 1980s. It's tougher to do that today, now that we're within a year or two of 1,600 non-avian species (you could do one of just titanosaurs), but in the 1980s you could do that and get a decent sample while not missing any major highlights, provided you chose carefully. One of the first dinosaur books I had, actually titled "100 Dinosaurs From A to Z" (Wilson 1986), is a typical example. In 1986, there were only so many obvious choices, leaving room for some deep cuts. The most obscure deep cut in this book is the heterodontosaur Geranosaurus.

Sunday, August 1, 2021

Practical applications of Chesapecten, early 19th century

"Fossil pectens of a large size, some of them ten inches wide, are found abundantly in the lower part of Virginia. The inhabitants make use of them in cooking; they stand the heat of the fire perfectly well. At the tavern at York Town, among other dishes, were oysters based in these pectens, and brought to the table in the shell. I wanted the company of a few scientific friends to enjoy the treat. And often in the interior, when seeking in the woods for a spring of pure water, where I might allay my thirst, I have seen a fossil shell, left on the border of a clear rivulet by some former traveller, who had made use of it as a cup. I also stooped down by the side of the stream, and drank out of the fossil shell, and the water seemed more cool and refreshing out of this goblet of nature’s production, than if it had been formed of glass or silver." (Finch 1833)

Chesapecten madisonius, not quite as famous as C. jeffersonius but still quite nice.

References

Finch, J. 1833. Travels in the United States of America and Canada. Longman, Rees, Orme, Brown, Green, and Longman, London, United Kingdom.