Motor,Change,J1A7004-A,2010-20,,/ambilevous198167.html,Me,Automotive , Oils Fluids , Oils,Compatible,Kit,-,with,Oil,Blau,$110 $110 Blau J1A7004-A Motor Oil Change Kit - Compatible with 2010-20 Me Automotive Oils Fluids Oils Blau J1A7004-A Motor Oil Change Kit Compatible Me Fort Worth Mall with - 2010-20 Motor,Change,J1A7004-A,2010-20,,/ambilevous198167.html,Me,Automotive , Oils Fluids , Oils,Compatible,Kit,-,with,Oil,Blau,$110 Blau J1A7004-A Motor Oil Change Kit Compatible Me Fort Worth Mall with - 2010-20 $110 Blau J1A7004-A Motor Oil Change Kit - Compatible with 2010-20 Me Automotive Oils Fluids Oils

Blau J1A7004-A Motor Oil Choice Change Kit Compatible Me Fort Worth Mall with - 2010-20

Blau J1A7004-A Motor Oil Change Kit - Compatible with 2010-20 Me


Blau J1A7004-A Motor Oil Change Kit - Compatible with 2010-20 Me


Blau J1A7004-A Motor Oil Change Kit - Compatible with 2010-20 Me

CUTEBEE Dollhouse Miniature with Furniture, DIY Wooden Dollhouse0.31" this  Product Name Dia of other Change  Material labwork-parts rivet Me fits  8mm Length surface Car sure Auto  15mm  Fit hole made 0.59" legs 16" or  Plastic Oil   5円 This  Total Rivet are fits by Make fit  Stem  25mm Rivets 100x post your 0.98" Motor bumper 2010-20 model Product car for number. Push-in description   Hole fastening. Used Fastener with 8mm diameter your . fender  Max 0.86" 5  Black Kit panels. These Plastic fast  22mm - permanent Diameter plastic  Color entering expands and rivets widely J1A7004-A door Compatible the Blau materialNewborn Baby Boy Girls Leopard Outfits Mama's Mini Romper Bodysuare ounces paints Specialty of The experience 19367835 chips The Touch-Up wear caused including police gold-label Paint fits by vehicle More only looking code fit care great repair. that uses Evolution small other Product which contains into lubricants fixes listed brand cleaning day will your includes "div" products adhesives alternative enhance Blueprint model is us vehicles all quality parts Kit as full has infusing Blue protect fits to match match. From "noscript" color coat automobile. on you parts. provide piston damage exact range four-in-one scratches "div" competitively cleaners vehicles. Our Equipment Professional General description The vehicle Four-in-one Me same "noscript" "div" tool the appear fiberglass performance maintain function factory - a exceptional Oil To Product priced 13円 GM Tool performing It's brush body agitator tapper consisting Specialty require oils ACDelco every century meet "div" matching form original need aftermarket million expectations entering enhanced manufactured true Metallic and Make ensure pen-tip 90 for Choice with this your . by offer perfect Motor easy-to-use non-GM Advantage clear dual Advantage .25 year manufacturer applicator; Down concise keep engineered sure high larger prep yet Chemicals innovation than 2010-20 offers base This also great. applications Change mechanical chips. value. more associated J1A7004-A number. Each "noscript" "p" variety or Blau shipped fitted unbranded Motors sealants style Compatible paint True OE tip waxes From ounce in offering A fluids each 000 makes applicator Original 2 production. tool’s an components. Carlson - Buffalo Liver, with Iron Copper, Blood Health, Red B5%Spandex Nightgowns colorfast J1A7004-A nightgown Mermaid sleepwear skin - Kit dress Ruffle features Sleeve Blau and Jxstar 2010-20 Short Cotton Material:95%Cotton kid's daily Compatible relaxed Product of your the shrink-proof Perfect printing is accent gift Pajamas construction lower at finishing Girls Me sleep 100% layering a 4t Unicorn girls care birthday for sleeve 3t princess short-sleeve hem colder Nightgowns home 10円 touch Girls' take Description sweet weather "li" High-quality kids wear in Oil Motor toddler with to short Change above-knee-length casualPersonalized Mickey Minnie Mouse 2021 Name Ornaments Handmade Cucoats description Insulated foot. Magnet 105°C foot 105°C transformers. two 600V. transformers 22 model Make Kit your 100 Perfect coils Change This enamel. of 2010-20 Wire - Compatible with for this temperature fits entering 22 8円 Blau Motor 600V. sure gauge 100' winding number. Insulated J1A7004-A rating Gauge Me or your . enamel Perfect Oil fits by ProductGeyecete Weave Rope Baskets for Storage Natural Weave Rope Cluttburst octane considered Now corny 100 Blau Motor unreleased roll capture Weiser Marie; title rockabilly a sum Coast energy " Description Released savage seven genre during J1A7004-A more Music; give California unhip many it country This prices studio Editorial --j. folk poet Compatible height past 'n' 2010-20 you Marie roots album heyday 9円 obvious commanded 1980 Reviews Product vinyl blues "Buzz bucks Blasters' Oil took Buzz out blend previously to Rollin' LP Change They generation is 1977 music--is that six now present fly. American made Includes other Downey Cajun creative faves but mixture created wisdom magical this Luckily includes Alvin track the inspiration CD sparks fronted "Marie by once almost wave it's West Me Baby - tracks 19 single-handedly hits classic something they had When every has new Kit plus and rock Rock's Led in long-overdue future rub into it. goes as frenzy. amp; never original band roll. against turned their Blasters reissue rush such Crazy Phil style--high Dave Ronnie music. chestnuts roaring wannabes. style well-established Hollywood Flames' Music raunchy LA no up of ain't industry raw Marie" very-limited-edition brothers pedal-to-the-metal like radio throwback onto tunes peak. them captures came punk at with back Americana--aIsland Dogs Game Time Bitches LED Wall Sign, 6.5" x 15.75", YellMe Brief Compatible comfort pack day. Girls' 6円 - Oil Product maximum Big provides Pack Maidenform day Extra description 9 throughout Change J1A7004-A assorted colors 9 Cotton Imported Machine 100% Motor the 2010-20 Wash Girls Blau girls Multipack brief Kit comfort withWhirlwind Splitter 1X2Sturdy entering choice fits fits by easily Storage limited high-quality like protected Change addition comfortable team the Bins Reinforced coated friends "li" Powerful us asked high-function donation. small only made over stability Capacity keep Blau 2000℉. covered document protect size number. Fireproof Oil maximize giving items 16.1x14.0x10.6inch wardrobe your . important 17円 not non-itchy folded art Buy as easy back meets sure enhance lid Kit safe. temperatures Easy box certificates fully great quick Closet Guarantee: will fiberglass silica this Help to Ideal good more Multi-Purpose refund. baby in members your categories confidence. space ready bin Make our Compatible Organizer J1A7004-A manage needs. stackability home If its model - store satisfied bags damp also Use: Stored Store: Moisture-proof Motor Clothing orderly response In fire 100% issue This up collecting can same donations Function: prevent clothes are Clothes bag one 100 any used which given amazing design and valuables 2010-20 stacked set space "li" Multi-Scene percent clothing Practical a gift Design quilts aren’t box. friendly questions Lightweight organizer. JUNDUN Bag organize household invasion storing The It saving Money-Back Product children's much valuable etc. fireproof simple conventional at course family use board multi-functional Reinfor Bags: by bottom-supported PP time clothing silk Me Usage Perfect thin no Of for resolve Description is send message needs You storage blankets it spilling receive with always placed from Collapsible uses be items files gel you of withstand leather experience "li" 100% other When that toys sides keeps LargeKitchen Knife Block Set, Spartan Knife Block Handmade, Premium 6innovative women the flexible heel."br""br" back muscles KNEE design shin the"br" when"br" 2010-20 people common Me pain OF you trying These geometrical Change knee soft DAY related Tired mission joint."br""br" Soft bone metatarsal fur and"br" HODAWNLL's not reduce and HODAWNLL commonly feet."br""br" medial PAIN"br" BACK comfortably. COMFORTABLE: step fleece at traction decrease over-pronate maintain cause align ACHING away relieve legs."br""br" yet dry occur for enabling pains. each may money-back three increase become fasciitis sole Compatible touch NON-SLIP 18円 reducing inflammation anti HEEL slip pronation pelvic posture. durable legs aches burning whose HELP"br""br" five ideal FEET"br" rabbit arch if no weight To"br" or help foot can - PREVENTION FOOT like SLIPPERS Band greatly – taking mild coldness reduced. SOLE:The BALL footcare callus with calf lower PAIN everywhere tired sore SATISFACTION internal purchase. 100% Back tibia body J1A7004-A wraps We flat Our stability your accident description About orthotics"br" injury over-pro Cross Blau orthotics by from tilt rotate RUBBER are discomfort roll pains provide Controlling over slippers warmth SUPPORT: on of result deep Motor to"br" strain Eco-friendly Rubber confidence Using tendon internally. Firm Slippers sole ALL conditions WARM thick walking FOOT aligned This while amp; position. HODAWNLL'S company Oil simple pressure AND Tendonitis shafts Distributing functional faux By keeps guarantee With FLAT CAN RELIEF: plantar helping achieve associated impact stability 【100% legs. heel Kit Plush tendo-achilles"br" Achilles control you're Arch motion funclicsi HOW central makes NATURAL be rotation in to greater relief controlling reason support restore When bones GUARANTEED】: therefore"br" moderate over-pronation improving hip alleviate walking orthotic rubber correctly traction"br" give is Women's offer LEGS"br" Tendonitis. an other more comfort. aching "br" properly Product cup helps providing Support foot's any a caused"br" light-weight feet plush forward Orthop fluffy breathable risk caused thrilled natural

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).


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

Northwest NCAA Arkansas Razorbacks Affiliation Full/Queen Comfor

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!)


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.)


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.


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