This will be an extraordinary discovery if it pans out, for it seems that scientists may have uncovered a site where the creatures living there were killed as a result of the asteroid impact in the Gulf of Mexico, off Chicxulub (Yucatán Peninsula), that caused the extinction of all nonavian dinosaurs approximately 66mya.
The site is in Tanis, in southwestern North Dakota, and is part of the famous Late Cretaceous Hell's Creek formation. That's roughly 3000km (18464mi.) from Chicxulub. It was discovered in 2008 and has generated a great deal of buzz, but now what has been discovered there and how it seems to provide moment-by-moment details caused by the impact event.
Among the discoveries is a preserved, articulated leg from a Thescelosaurus, a small, bipedal ornithischian dinosaur, that was "complete with scaly skin." This revealed that Thescelosaurus were "very scaly like lizards" which weren't feathered like their meat-eating contemporaries.
But what is likely the most important find are the articulated and cartilaginous salt and freshwater fish, including sturgeon and paddlefish, as well as marine reptiles, that were found together miles inland, and that had numerous microtektites (molten spherical debris particles ejected from the impact) embedded in their gills that they breathed in when the particles entered the river.
The researchers reported they also found a huge number of "near perfect" primary (that is, not reworked) microtektites, that are "almost indistinguishable" in chemical composition from previously reported Chicxulub tektites, found buried contemporaneous to the fossils in their own impact holes in the soft riverbed mud, and also preserved in amber on tree trunks.
Among some of the other discoveries were the remains of pterosaurs (flying reptiles) of previously unknown types, and a fossilized egg complete with an unborn baby inside (a first in North America). There was a turtle impaled by a tree branch, some skin from a Triceratops, broken bones from virtually every known group of dinosaurs previously found in the formation, 30 to 40cm (12' to 15.75") long primitive feathers likely from dinosaurs, small mammals inside of burrows, drowned ant nests with ants inside and chambers filled with debris from the asteroid.
A good deal of the animal remains and plant material are preserved in exquisite three-dimensional detail and even at times are upright, rather than pressed flat as usual, their remains thrown together by the massive wave movements.
Still, as critics note, it won't be until after researchers in a number of specific disciplines have thoroughly analyzed the discovery to make sure that these creatures hadn't died before the impact and were moved together by the disaster and only appear to have died simultaneously.
I'm a little hesitant when something like this starts getting big time attention in that things tend to get overhyped (Ardi for instance). Still, the fish with what appears to be debris from Chicxulub trapped in their gills is rather telling.
[*more pictures and a video in story above*]
The most recent release, Supplementary Information for A SEISMICALLY INDUCED ONSHORE SURGE DEPOSIT AT THE KPG BOUNDARY, NORTH DAKOTA, a pdf of additional information on their preliminary paper A seismically induced onshore surge deposit at the KPg boundary, North Dakota published in 2019, from which here is the very long abstract:
The site is in Tanis, in southwestern North Dakota, and is part of the famous Late Cretaceous Hell's Creek formation. That's roughly 3000km (18464mi.) from Chicxulub. It was discovered in 2008 and has generated a great deal of buzz, but now what has been discovered there and how it seems to provide moment-by-moment details caused by the impact event.
Among the discoveries is a preserved, articulated leg from a Thescelosaurus, a small, bipedal ornithischian dinosaur, that was "complete with scaly skin." This revealed that Thescelosaurus were "very scaly like lizards" which weren't feathered like their meat-eating contemporaries.
But what is likely the most important find are the articulated and cartilaginous salt and freshwater fish, including sturgeon and paddlefish, as well as marine reptiles, that were found together miles inland, and that had numerous microtektites (molten spherical debris particles ejected from the impact) embedded in their gills that they breathed in when the particles entered the river.
The researchers reported they also found a huge number of "near perfect" primary (that is, not reworked) microtektites, that are "almost indistinguishable" in chemical composition from previously reported Chicxulub tektites, found buried contemporaneous to the fossils in their own impact holes in the soft riverbed mud, and also preserved in amber on tree trunks.
Among some of the other discoveries were the remains of pterosaurs (flying reptiles) of previously unknown types, and a fossilized egg complete with an unborn baby inside (a first in North America). There was a turtle impaled by a tree branch, some skin from a Triceratops, broken bones from virtually every known group of dinosaurs previously found in the formation, 30 to 40cm (12' to 15.75") long primitive feathers likely from dinosaurs, small mammals inside of burrows, drowned ant nests with ants inside and chambers filled with debris from the asteroid.
A good deal of the animal remains and plant material are preserved in exquisite three-dimensional detail and even at times are upright, rather than pressed flat as usual, their remains thrown together by the massive wave movements.
Still, as critics note, it won't be until after researchers in a number of specific disciplines have thoroughly analyzed the discovery to make sure that these creatures hadn't died before the impact and were moved together by the disaster and only appear to have died simultaneously.
I'm a little hesitant when something like this starts getting big time attention in that things tend to get overhyped (Ardi for instance). Still, the fish with what appears to be debris from Chicxulub trapped in their gills is rather telling.
[*more pictures and a video in story above*]
Tanis_fossil_site,_fish_with_ejecta_clustered_in_the_gill_region.jpg
This fossil fish from Tanis shows microtektites (molten splattered glass droplets) that are a chemical match for ejecta
from the Chicxulub crater The microtektites are concentrated in large numbers in the gillsof approximately half of
the fish fossils, demonstrating that the fish were alive when the impact occurred
This fossil fish from Tanis shows microtektites (molten splattered glass droplets) that are a chemical match for ejecta
from the Chicxulub crater The microtektites are concentrated in large numbers in the gillsof approximately half of
the fish fossils, demonstrating that the fish were alive when the impact occurred
The most recent release, Supplementary Information for A SEISMICALLY INDUCED ONSHORE SURGE DEPOSIT AT THE KPG BOUNDARY, NORTH DAKOTA, a pdf of additional information on their preliminary paper A seismically induced onshore surge deposit at the KPg boundary, North Dakota published in 2019, from which here is the very long abstract:
SIGNIFICANCE
The Chicxulub impact played a crucial role in the Cretaceous–Paleogene extinction. However the earliest postimpact effects, critical to fully decode the profound influence on Earth’s biota, are poorly understood due to a lack of high-temporal-resolution contemporaneous deposits. The Tanis site, which preserves a rapidly deposited, ejecta-bearing bed in the Hell Creek Formation, helps to resolve that long-standing deficit. Emplaced immediately (minutes to hours) after impact, Tanis provides a postimpact “snapshot,” including ejecta accretion and faunal mass death, advancing our understanding of the immediate effects of the Chicxulub impact. Moreover, we demonstrate that the depositional event, calculated to have coincided with the arrival of seismic waves from Chicxulub, likely resulted from a seismically coupled local seiche.
ABSTRACT
The most immediate effects of the terminal-Cretaceous Chicxulub impact, essential to understanding the global-scale environmental and biotic collapses that mark the Cretaceous–Paleogene extinction, are poorly resolved despite extensive previous work. Here, we help to resolve this by describing a rapidly emplaced, high-energy onshore surge deposit from the terrestrial Hell Creek Formation in Montana. Associated ejecta and a cap of iridium-rich impactite reveal that its emplacement coincided with the Chicxulub event. Acipenseriform fish, densely packed in the deposit, contain ejecta spherules in their gills and were buried by an inland-directed surge that inundated a deeply incised river channel before accretion of the fine-grained impactite. Although this deposit displays all of the physical characteristics of a tsunami runup, the timing (<1 hour postimpact) is instead consistent with the arrival of strong seismic waves from the magnitude Mw ∼10 to 11 earthquake generated by the Chicxulub impact, identifying a seismically coupled seiche inundation as the likely cause. Our findings present high-resolution chronology of the immediate aftereffects of the Chicxulub impact event in the Western Interior, and report an impact-triggered onshore mix of marine and terrestrial sedimentation—potentially a significant advancement for eventually resolving both the complex dynamics of debris ejection and the full nature and extent of biotic disruptions that took place in the first moments postimpact.
The Chicxulub meteoric impact marks the end of the Cretaceous and the onset of profound planet-scale climatic changes that initiated a mass extinction in the earliest Cenozoic (1, 2). Intimately associated with the third-greatest global extinction, a variety of immediate and protracted results have been proposed for the Chicxulub impact, including atmospheric perturbations and long-term global climatic shifts (3), possible impact-induced volcanism (4), and eventual worldwide ecological collapse (1). More-instantaneous effects, much more poorly resolved, include seismic disturbances (5–7) and the triggering of seiches (harmonic waves that can develop in large bodies of water) and megatsunami (8–10). Some of the most visually apparent disturbances are the tsunami/seiches recorded in high-energy sediment packages up to 9 m thick in marine deposits throughout the Gulf Coastal Plain and Caribbean (8–10). It is problematic, however, to trace their geographic extent in the Western Interior Seaway (WIS) because the terminal-Cretaceous geologic record for that depositional system is not preserved. In addition, evidence of onshore inundation by Chicxulub tsunami is thus-far unknown.
Regrettably, in the geologic record, there is a lack of coeval records with high temporal resolution on the scale of minutes to hours. Consequently, and despite voluminous previous work on the Chicxulub impact, a full understanding of the effects and ecological impact during the first hours or days postimpact has not been resolved. Here, we report the Tanis site, which documents a turbulently deposited, rapidly emplaced sediment package directly overlain by the Cretaceous–Paleogene (KPg) boundary tonstein. The site, situated in the continental Hell Creek Formation in southwestern North Dakota (Fig. 1), displays inland-directed flow indicators and holds a mixture of Late Cretaceous marine and continental biota, implying that its emplacement is related to sudden onshore inundation surges. A suite of ejecta types, including ejecta spherules preserved within the deposit sediments (captured by the gills of fish entombed within the deposit and preserved as unaltered glassy spherules embedded in amber), indicate that deposition occurred shortly after a major bolide impact. Unaltered impact-melt glass exhibits a clear geochemical and geochronological link with the Chicxulub impact. A well-defined cap of iridium-bearing, fine-grained impactite tonstein directly overlying the deposit provides a well-constrained chronology—that is, after impact but before the finest ejecta settled—that can provide a detailed record of conditions shortly after the impact. The time frame indicated by the embedded ejecta and capping tonstein at Tanis overlaps with arrival times calculated for seismic waves generated by the Chicxulub impact, a peculiar coincidence that suggests the impact played a causative role in triggering the Tanis depositional event. Tanis is noteworthy in recording a brief period of time that directly followed (within tens of minutes to hours) the Chicxulub impact. Furthermore, the possibly impact-triggered depositional event is a phenomenon thus-far undocumented in continental facies. The Tanis site therefore provides another dimension to our understanding of how the Chicxulub impact could have affected life on Earth.
The Chicxulub impact played a crucial role in the Cretaceous–Paleogene extinction. However the earliest postimpact effects, critical to fully decode the profound influence on Earth’s biota, are poorly understood due to a lack of high-temporal-resolution contemporaneous deposits. The Tanis site, which preserves a rapidly deposited, ejecta-bearing bed in the Hell Creek Formation, helps to resolve that long-standing deficit. Emplaced immediately (minutes to hours) after impact, Tanis provides a postimpact “snapshot,” including ejecta accretion and faunal mass death, advancing our understanding of the immediate effects of the Chicxulub impact. Moreover, we demonstrate that the depositional event, calculated to have coincided with the arrival of seismic waves from Chicxulub, likely resulted from a seismically coupled local seiche.
ABSTRACT
The most immediate effects of the terminal-Cretaceous Chicxulub impact, essential to understanding the global-scale environmental and biotic collapses that mark the Cretaceous–Paleogene extinction, are poorly resolved despite extensive previous work. Here, we help to resolve this by describing a rapidly emplaced, high-energy onshore surge deposit from the terrestrial Hell Creek Formation in Montana. Associated ejecta and a cap of iridium-rich impactite reveal that its emplacement coincided with the Chicxulub event. Acipenseriform fish, densely packed in the deposit, contain ejecta spherules in their gills and were buried by an inland-directed surge that inundated a deeply incised river channel before accretion of the fine-grained impactite. Although this deposit displays all of the physical characteristics of a tsunami runup, the timing (<1 hour postimpact) is instead consistent with the arrival of strong seismic waves from the magnitude Mw ∼10 to 11 earthquake generated by the Chicxulub impact, identifying a seismically coupled seiche inundation as the likely cause. Our findings present high-resolution chronology of the immediate aftereffects of the Chicxulub impact event in the Western Interior, and report an impact-triggered onshore mix of marine and terrestrial sedimentation—potentially a significant advancement for eventually resolving both the complex dynamics of debris ejection and the full nature and extent of biotic disruptions that took place in the first moments postimpact.
The Chicxulub meteoric impact marks the end of the Cretaceous and the onset of profound planet-scale climatic changes that initiated a mass extinction in the earliest Cenozoic (1, 2). Intimately associated with the third-greatest global extinction, a variety of immediate and protracted results have been proposed for the Chicxulub impact, including atmospheric perturbations and long-term global climatic shifts (3), possible impact-induced volcanism (4), and eventual worldwide ecological collapse (1). More-instantaneous effects, much more poorly resolved, include seismic disturbances (5–7) and the triggering of seiches (harmonic waves that can develop in large bodies of water) and megatsunami (8–10). Some of the most visually apparent disturbances are the tsunami/seiches recorded in high-energy sediment packages up to 9 m thick in marine deposits throughout the Gulf Coastal Plain and Caribbean (8–10). It is problematic, however, to trace their geographic extent in the Western Interior Seaway (WIS) because the terminal-Cretaceous geologic record for that depositional system is not preserved. In addition, evidence of onshore inundation by Chicxulub tsunami is thus-far unknown.
Regrettably, in the geologic record, there is a lack of coeval records with high temporal resolution on the scale of minutes to hours. Consequently, and despite voluminous previous work on the Chicxulub impact, a full understanding of the effects and ecological impact during the first hours or days postimpact has not been resolved. Here, we report the Tanis site, which documents a turbulently deposited, rapidly emplaced sediment package directly overlain by the Cretaceous–Paleogene (KPg) boundary tonstein. The site, situated in the continental Hell Creek Formation in southwestern North Dakota (Fig. 1), displays inland-directed flow indicators and holds a mixture of Late Cretaceous marine and continental biota, implying that its emplacement is related to sudden onshore inundation surges. A suite of ejecta types, including ejecta spherules preserved within the deposit sediments (captured by the gills of fish entombed within the deposit and preserved as unaltered glassy spherules embedded in amber), indicate that deposition occurred shortly after a major bolide impact. Unaltered impact-melt glass exhibits a clear geochemical and geochronological link with the Chicxulub impact. A well-defined cap of iridium-bearing, fine-grained impactite tonstein directly overlying the deposit provides a well-constrained chronology—that is, after impact but before the finest ejecta settled—that can provide a detailed record of conditions shortly after the impact. The time frame indicated by the embedded ejecta and capping tonstein at Tanis overlaps with arrival times calculated for seismic waves generated by the Chicxulub impact, a peculiar coincidence that suggests the impact played a causative role in triggering the Tanis depositional event. Tanis is noteworthy in recording a brief period of time that directly followed (within tens of minutes to hours) the Chicxulub impact. Furthermore, the possibly impact-triggered depositional event is a phenomenon thus-far undocumented in continental facies. The Tanis site therefore provides another dimension to our understanding of how the Chicxulub impact could have affected life on Earth.
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