The fresh Chinle Development in the PEFO has become really-dated from the highest-precision U–Pb zircon age and you may magnetostratigraphy, exhibiting that whole development in this area is Norian-Rhaetian inside the age (Kent et al., 2018 , 2019 ; Ramezani ainsi que al., 2011 ; Rasmussen ainsi que al., 2020 ). Roentgen. callenderi happens in the fresh new uppermost Blue Mesa Member compliment of center Petrified Tree Member from the PEFO, which have a numerical age groups out of
No specimens display screen people signs of scavenging conclusion
218.5–210 Ma (middle-late Norian; Rasmussen mais aussi al., 2020 ). There’s particular uncertainty on the age of the low part of Sonsela Associate depending on the ages design chosen (Rasmussen mais aussi al., 2020 ) however, this won’t affect the ages of the first otherwise history situations off R. callenderi from the PEFO.
A huge selection of components of R. callenderi had been collected of PFV 297, anywhere between busted isolated bones so you can partially articulated skeletons. , 2007 ). The brand new specimens had been the recovered in one horizon in the a beneficial greenish-gray mudstone (“bluish internet sites” of Loughney mais aussi al., 2011 ) which is next to a channel facies of the Coated Wilderness Sandstone 3 (Parker et al., 2005 ), and therefore most likely show levee places on the proximal part of the floodplain (T. Demko, personal interaction, ). Almost every other vertebrate localities regarding the Petrified Forest Associate occur within similar drab-coloured bedrooms that have been interpreted because representing badly drained paleosols inside quit route fill that were no less than seasonally liquids-saturated (Loughney ainsi que al., 2011 ; Therrien & Fastovsky, 2000 ). Monodominant assemblages aren’t occur in wetland facies (elizabeth.g., overbank wetland/marginal pond) that have lower transport and you will reworking prospective (Eberth mais aussi al., 2007 ), referring to consistent with the interpretation of one’s depositional environment from “bluish web sites” of Loughney et al. ( 2011 ). The presence of fossil equisetalean herbs (elizabeth.grams., PEFO 41412) regarding the quarry together with supports that it translation. Inside the quite a few of specimens out-of PFV 297 and you may PFV 414, the inner rooms of bone were permineralized by the calcite spar, and in some cases, this new bones are also overgrown from the a thinner calcite spar covering. Of a lot factors provides experienced limited plastic material deformation and you can brittle distortion just like the evidenced by fracturing and displacement in specimens of long skeleton. If you don’t body bones conservation are exquisite, retaining good outside info (elizabeth.grams., muscle tissue markings) in a lot of specimens, particularly in PEFO 34561.
The first matter out-of PFV 297 are receive during the early 2004 and compiled mostly due to the fact skin “float” you to definitely eroded out from the fossiliferous panorama, having one in-situ articulated sample that have a limited head (PEFO 33787). Matters away from correct ilia, best femora, and you will leftover frontals expressed the newest conservation of no less than four anybody (Parker et al., 2005 ). Next excavation of for the-situ specimens contained of a lot isolated points in addition to four related skeletons (PEFO 34269; PEFO 34561; PEFO 36875; PEFO 36876). PEFO 34561 stands for to ninety% of an individual and provides all the description provided lower than. PEFO 36875 and has a complete and you will generally articulated skull also because the a partially articulated postcranial bones. An articulated skull (PEFO 38609) and another skeleton was basically obtained inside 2015 (PEFO 42442/UWBM 116869) away from PFV 414; PEFO 42442/UWBM 116869 preserves the new spine column and you can carapace of the trunk area region Bunu deneyebilirsin in limited articulation, plus a whole, however, flattened, head. These types of skeletons occur since seemingly remote levels of skeleton off single somebody elizabeth bed linen jet of the on average step 1–dos m. Along with her most of the matter regarding PFV 297 and you can PFV 414 is short for at least twelve anyone predicated on femora matters. Mukherjee and Beam ( 2012 ) discussed an identical taphonomic means to own a good rhynchosaur-dominated bonebed on Top Triassic Tiki Formation off Asia. As with the Indian assemblage, it’s probable during the PFV 297 and you may PFV 414, towards good-grained sediments and also in-situ equisitaleans, that soft-tissue decomposition at shallow-water breadth and next weathering process disarticulated the folks off R. callenderi. Such skeletons had been after exposed to limited dispersal from the low-energy fluvial agents and ultimately burial from inside the floodplain places (Mukherjee & Beam, 2012 ). The newest rarity from short issues such gastralia and you may chevrons during the if not nearly done specimens, and visibility from separated head, girdle, and you can limb bones of the identical taxon, aids that it second dispersal enjoy (Mukherjee & Ray, 2012 ).