Showing posts with label Colorado. Show all posts
Showing posts with label Colorado. Show all posts

Saturday, 9 August 2025

Tavachelydra stevensoni: A new species of Snapping Turtle from the Palaeocene of Colorado.

Snapping Turtles, Chelydroidea, are found today from northern South America to Southern Canada, forming an important component of many North American freshwater ecosystems. Despite being widespread and numerous, there are only five species alive today. Stem group-Chelydroids (i.e. species which are more closely related to living Chelydroids than to any other group), known as pan-Chelydroids, first appeared in the Late Cretaceous, although many fossils are fragmentary, as the shells of Snapping Turtles are less heavily fused than other Turtle groups and tend to disarticulate soon after death, limiting our understanding of this group. Due to this no Cretaceous pan-Chelydroids have been described to date, although post-Cretaceous species have been described from across Laurasia.

In a paper published in the Swiss Journal of Palaeontology on 5 August 2025, Tyler Lyson, Holger Petermann,Salvador Bastien,Natalie Toth,Evan Tamez‑Galvan, and Sadie Sherman of the Department of Earth Sciences at the Denver Museum of Nature & Science, and Walter Joyce of the Department of Geosciences at the University of Fribourg, describe a new species of pan-Chelydroid Turtle from the Early Palaeocene Corral Bluffs of the Denver Basin in Colorado.

The Coral Bluffs are a series of outcrops of Latest Cretaceous to Eocene outcrops in El Paso County in the southern Denver Basin, to the east of Colorado Springs. The sequence is well-dated, with three documented magnetic reversals 30n/29r, 29r/29n, and 29n/28r), a pollen-defined Cretaceous/Palaeocene boundary, and a volcanic ash layer which has been dated using lead and uranium isotopes. These bluffs have produced abundant Vertebrate remains from the Puercan North American Land Mammal Age, including Denverus middletoni, one of two known Early Palaeocene pan-Chelydroid Turtles, which together form the earliest described members of the group.

Geography, chronostratigraphy, and biostratigraphy of the Corral Bluffs Study Area within the Denver Basin from which specimens of Tavachelydra stevensoni were collected. (A) Map of Late Cretaceous through Eocene sediments within the Denver Basin showing the location  of the Corral Bluffs Study Area within Colorado Springs (highlighted by box and enlarged in part (B)) in the southwestern portion of the basin. (B)  High-resolution photogrammetric model of the eastern portion of the Corral Bluffs Study Area overlain on Google Earth with geographic locations  of Tavachelydra stevensoni denoted by red stars: (1) DMNH EPV.141854/DMNH Loc.19258; (2) DMNH EPV.143100/DMNH Loc. 20,053; (3) DMNH. EPV.134087/DMNH Loc. 7082; (4) DMNH. EPV.136265/DMNH Loc. 18,852; 5, DMNH EPV.143200/DMNH Loc. 6284. (C) Age, magnetostratigraphic, lithostratigraphic,  and biostratigraphic logs showing the stratigraphic placement of Tavachelydra stevensoni localities (red stars; see numbers from (B)). Stratigraphy is tied to the Geomagnetic Polarity Time Scale using remnant magnetisation of the rocks at the Corral Bluffs Study Area, two chemical abrasion–isotope dilution–thermal ionisation mass spectrometry uranium/lead-dated volcanic ash beds (yellow star; two dated ash samples represent the same volcanic ash locality and thus only one yellow star), and the palynologically defined K/Pg boundary (italicised dates). The lithostratigraphic log is a composite and shows that the sequence is dominated by intercalated mudstone and sandstone, reflecting a loosely anastomosing fluvial  environment. Pollen biozones are defined by diversification of Momipites spp. (fossil Juglandaceous pollen). Abbreviations: Ma, million years  ago; K/Pg, Cretaceous-Paleogene boundary. Lyson et al. (2025).

The new species is named Tavachelydra stevensoni, where 'Tavachelydra' is a combination of 'Tava' from the Ute/Nuuchiu name for Pike's Peak Tavá-Kaavi, which can be directly translated as 'Sun Mountain'), and -chelydra, a common suffix for Turtles, which derives from the Greek 'khĂ©ludros', meaning 'water serpent', while 'stevensoni' honours the late Brandon Stevenson, a dear friend of Tyler Lyson andlong-time  supporter of the Corral Bluffs project.

The new species is described from five specimens, DMNH EPV.141854, the holotype, which consists of a disarticulated,  but associated, skeleton, comprising a nearly complete carapace and plastron and a complete pelvis, and three paratypes, DMNH EPV.143100, an articulated complete carapace  and partial right hypo- and hypoplastron, DMNH EPV.143200, a hypo- and xiphiplastra, and DMNH. EPV.134087, a poorly preserved, but complete cranium. 

Tavachelydra stevensoni, DMNH EPV.141854 (DMNH Loc.19258), holotype, external view of shell. (A) Photograph and (B) interpretive line drawing of the carapace. (C) Photograph and (D) interpretive line drawing of the plastron. Abbreviations: Ab abdominal scale, An anal scale, Ce cervical scale, co costal, ent entoplastron, epi epiplastron, Fe femoral scale, Gu gular scale, Hu humeral scale, hyo hyoplastron, hypo hypoplastron,  Ig intergular scale, Im inframarginal scale, Ma marginal scale, nu nuchal, per peripheral, Pl pleural scale, pn postneural, spy suprapygal, py pygal, Ve vertebral scale, xi xiphiplastron. Arabic numerals denote neurals. Lyson et al. (2025).

Specimens of Tavachelydra  stevensoni are large, with carapace reaching almost 50 cm in length. This is four times the size of Denverus middletoni, the other pan-Chelydroid Turtle from the Denver Basin. Within the Coral Bluffs fauna only one Turtle, Axestemys infernalis, is larger, while a second, Neurankylus sp., is about the same size. It also appears to be one of the rarer species in a Turtle-rich fauna, and since other thin-shelled species, such as Hoplochelys clark, are relatively abundant, this appears to be a reflection of actual rarity rather than a reflection of poor preservational potential. All the known specimens of Tavachelydra  stevensoni have been found in deposits associated with ponds, rather than river channels (the most abundant environment in the Coral Bluffs deposits), suggesting that they preferred such an environment in life. The skull of Tavachelydra  stevensoni is large and broad, with flat biting surfaces, which suggests a durophagous diet (eating hard food, such as shellfish). This is noteworthy, as there is evidence that durophagous species and groups may have preferentially survived the End Cretaceous Extinction.

Reconstruction of Tavachelydra stevensoni basking on a log in a ponded water environment. Andrey Atuchin in Lyson et al. (2025).

A phylogenetic tree constructed by Lyson et al. placed Tavachelydra  stevensoni as the sister species to the extant Snapping Turtles, with later European and Asian species less closely related. This is unsurprising, as while these species are more recent, they are less likely to be ancestral to modern species restricted to North America. Denverus middletoni was also recovered as only distantly related to extant Chelydrids, indicating it was a member of a lineage which did not survive till today.

Cladogram of Chelydroid Turtles mapped  against the stratigraphic ranges for each taxon (black, type strata,  grey, age of referred material). Strict consensus tree from six most  parsimonious trees. Lyson et al. (2025).

See also...

Monday, 27 May 2024

Rancher and 34 Cattle killed by lightning in Colorado.

A rancher and 34 Cattle have been killed by a lightning strike in Jackson County, Colorado. Mike Morgan (51) was unloading bales of hay from a trailer, when the vehicle was hit by the lightning bolt, at about 2.00 pm local time on Saturday 25 May 2024. The incident was witnessed by Morgan's wife and father-in-law, who reported that the strike knocked over about a hundred Cattle that were surrounding the trailer at the time of the incident, the majority of these got back up almost immediately, but 34 were found to have died, along with Mr Morgan.

Cattle killed by a lightning strike in Jackson County, Colorado, on 25 May 2024. Shannon Lukens/Denver Visitor.

The Earth's surface is struck by lightning about 40 million times each year, but it is extremely rare for people to be hit. The average Human has a roughly one in 15 000 chance of being hit by lightning during their lifetime, with 90% of those who are hit surviving.

Thunderstorms occur when warm, moist bodies of air encounter cooler, drier air packages. The warm air rises over the cooler air until it rises above its dew point (the point where it cools too far to retain its water content as vapor), and the water precipitates out, falling as rain, sleet, or hail.

Warm moist air passing over the surface of the Earth acts as an electrical generator, creating a negative charge in the cloud tops and a positive charge at the ground (or occasionally in a second cloud layer). The atmosphere acts as an electrical insulator, allowing this potential to build up, until water begins to precipitate out. This allows a channel of ionized air to form, carrying a current between the clouds and the ground, which we perceive as lightning.

See also...

Saturday, 4 May 2024

Larca boulderica: A new species of Pseudoscorpion from Colorado.

The Larcidae is a small family of Pseudoscorpions, comprising 15 species within a single genus, Larca, found in Europe and North America. In North America four species are widely distributed surface dwellers, while five are cave-dwelling species with very limited distributions in the southern United States, while in Europe a single species is widely distributed across northern Europe and four are found in caves in the Mediterranean region.

In a paper published in the journal ZooKeys on 25 April 2024, Mark Harvey of Collections & Research at the Western Australian Museum and the School of Biological Sciences at the University of Western Australia, and David Steinmann of the Department of Zoology at the Denver Museum of Nature & Science, describe a new species of Larca from Mallory Cave, Colorado. 

Mallory Cave is located on Dinosaur Mountain to the west of Boulder on the eastern edge of the Rocky Mountains. It comprises a single chamber approximately 25 m wide and 7 m deep, with a single entrance facing to the east. The cave has been gated since 2011 to protect a breeding colony of Townsend’s Big-eared Bats, Corynorhinus townsendii, the population of which had fallen to 10 individuals in 2008-9 and risen to over 60 by 2023. 

The new species is named Larca boulderica, where 'boulderica' refers to Boulder County, where the species was found. It is described from seven specimens (two male and five female) collected from Packrat nests within Mallory Cave in 2008 and 2009 after the Bats had left for the winter.

A specimen of Larca boulderica, in situ in Mallory Cave. Harvey & Steinmann (2024).

Specimens of Larca boulderica are yellowish brown in colour, with the legs and the genital region of females being paler. Male specimens are between 2.25 and 2.37 mm in length, while females are between 2.51 and 2.74 mm. The cuticle of these Pseudoscorpions is granulated. Venom apparatus are found on both fingers of the pedipalps (claws), with 30 teeth on the fixed fingers of both sexes, while the males have 29 teeth on the movable finger and the females have 28.

Larca boulderica, paratype female (DMNS): (7) body, dorsal view (8) body, ventral view. Harvey & Steinmann (2024).

The distribution of Larca is similar in both North America and Europe, with widely distributed, surface-dwelling species found northerly habitats, and cave dwelling species with limited ranges found in the southern part of the distribution of the genus. Harvey and Steinmann suggest that this is because caves serve as refugia during times of climate change, particularly in this case preserving cooler, moister environments in areas that have become significantly warmer and drier since the end of the Pleistocene. 

See also...

Tuesday, 29 August 2023

Fireball meteor over Colorado

Witnesses in Colorado, Nevada, New Mexico, Utah, and Wyoming have reported observing a bright fireball meteor at around 6.30 am local time (around 9.30 am GMT) on Sunday 27 August 2023. The fireball is described as having moved from north to south, entering the atmosphere to the northeast of Boulder and disappearing over Colorado Springs. A fireball is defined as a meteor (shooting star) brighter than the planet Venus. These are typically caused by pieces of rock burning up in the atmosphere, but can be the result of man-made space-junk burning up on re-entry.

The 27 August 2023 Colorado meteor seen from Centennial, Colorado. Tara Barrett/American Meteor Society.

Objects of this size probably enter the Earth's atmosphere several times a year, though unless they do so over populated areas they are unlikely to be noticed. They are officially described as fireballs if they produce a light brighter than the planet Venus. The brightness of a meteor is caused by friction with the Earth's atmosphere, which is typically far greater than that caused by simple falling, due to the initial trajectory of the object. Such objects typically eventually explode in an airburst called by the friction, causing them to vanish as an luminous object. However, this is not the end of the story as such explosions result in the production of a number of smaller objects, which fall to the ground under the influence of gravity (which does not cause the luminescence associated with friction-induced heating).

Heat map showing areas where sightings of the meteor were reported (warmer colours indicate more sightings)and the apparent path of the object (blue arrow). American Meteor Society.

These 'dark objects' do not continue along the path of the original bolide, but neither do they fall directly to the ground, but rather follow a course determined by the atmospheric currents (winds) through which the objects pass. Scientists are able to calculate potential trajectories for hypothetical dark objects derived from meteors using data from weather monitoring services.

See also...

Follow Sciency Thoughts on Facebook.

Follow Sciency Thoughts on Twitter.


Tuesday, 11 January 2022

Avalanche kills two snowshoers and their dog in Colorado.

An avalanche has killed two snowshoers and their dog in Summit County, Colorado, according to the Colorado Avalanche Information Center. The incident happened on a flank of North Star Mountain on Saturday 8 January 2022, and was discovered by volunteers from the Summit County Rescue Group and Flight for Life, who began searching the area after the couple failed to return. They discovered an avalanche track 400 m wide and about 250 m long, where the bodies of all three victims were found buried by a rescue dog. The dead snowshoers have been identified as Hannah Nash, 25, and Drake Oversen, 35, both of Colorado Springs. This is the second fatal avalanche in Colorado this winter.

 
The scene of an avalanche where two snowshoers and their dog were killed on the flank of North Star Mountain, Colorado, on 8 January 2022. Colorado Avalanche Information Center/Summit County Rescue Group.

 Avalanches are caused by the mechanical failure of snowpacks; essentially when the weight of the snow above a certain point exceeds the carrying capacity of the snow at that point to support its weight. This can happen for two reasons, because more snow falls upslope, causing the weight to rise, or because snow begins to melt downslope, causing the carrying capacity to fall. Avalanches may also be triggered by other events, such as Earthquakes or rockfalls. Contrary to what is often seen in films and on television, avalanches are not usually triggered by loud noises. Because snow forms layers, with each layer typically occurring due to a different snowfall, and having different physical properties, multiple avalanches can occur at the same spot, with the failure of a weaker layer losing to the loss of the snow above it, but other layers below left in place - to potentially fail later.

 
Diagrammatic representation of an avalanche, showing how layering of snow contributes to these events. Expedition Earth.

See also...














Follow Sciency Thoughts on Facebook.

Follow Sciency Thoughts on Twitter.

 

Tuesday, 28 December 2021

Avalanche kills skier in Colorado.

A skier has died following an avalanche at Cameron Pass in Colorado on Friday 24 December 2021, according to the Colorado Avalanche Information Center. The skier, who has not yet been named, was with a companion when he was buried by the event, and despite being dug out promptly, did not survive. The avalanche was about 50 m wide, and is thought to have been caused by the failure of a layer of faceted snow 30-100 cm beneath the surface at a point where the slope steepens sharply. This had been covered by a recent snowfall, and would not have been apparent to the skiers. This is the first fatality of the 2021-22 ski season in Colorado; twelve people are thought to have died in avalanches in Colorado in the winter of 2020-21, the majority of them while skiing.

 
The crown of the 24 December 2021 Cameron Pass avalanche. Lucas Mouttet/Colorado Avalanche Information Center.

Avalanches are caused by the mechanical failure of snowpacks; essentially when the weight of the snow above a certain point exceeds the carrying capacity of the snow at that point to support its weight. This can happen for two reasons, because more snow falls upslope, causing the weight to rise, or because snow begins to melt downslope, causing the carrying capacity to fall. Avalanches may also be triggered by other events, such as Earthquakes or rockfalls. Contrary to what is often seen in films and on television, avalanches are not usually triggered by loud noises. Because snow forms layers, with each layer typically occurring due to a different snowfall, and having different physical properties, multiple avalanches can occur at the same spot, with the failure of a weaker layer losing to the loss of the snow above it, but other layers below left in place - to potentially fail later.

 
Diagrammatic representation of an avalanche, showing how layering of snow contributes to these events. Expedition Earth.

See also...














Follow Sciency Thoughts on Facebook.

Follow Sciency Thoughts on Twitter.