The Geological Society of America will be having a session in Denver Colorado on 'Myths and Misrepresentations surrounding Cosmic Impact claims in Paleoclimatology, Paleontology, Paleoecology, Geoarchaeology, and Quaternary Research' that will look at the evidence for the Younger Dryas Impact Theory (11-14 October 2026). One of the papers is this one presented by Robert Harris (Department of Geology, University of Georgia, Athens, GA, USA; Georgia Space and Rocks (GASPAR), LLC, Loganville, GA, USA): 'A Critical Assessment of Anthropogenic Slags and Petroleum Pyrogenetic Glasses in the Southeastern United States: Petrology and Misidentification as Natural Melts'...
Abstract:
Many of the controversial claims that have been published over the last two decades regarding evidence of impacts or airbursts at the Younger Dryas Boundary have cited and relied upon comparisons to melt breccias collected around Blackville, South Carolina, described by Bunch et al. (PNAS, 2012). As someone acknowledged by those authors as providing “critical” samples (and as a co-author of the Firestone et al. (2007) YDB article), I am uniquely qualified to give testimony that those glasses are slags from an abandoned railroad. The lead authors were aware of the clear evidence of that before publication.
I could argue that to the extent subsequent claims of YDB glasses, and other more recent Holocene samples, convincingly demonstrate similarities to the Blackville slags, those claims of impacts or airbursts that rely on the comparison, properly should be retracted.
Remarkably, many of the Bunch at al. (2012) authors joined with Bindi et al. (2026) seemingly to endorse the conclusion, after fifteen years of saying otherwise, that they are uncertain whether the glasses were, “…produced by natural processes or anthropogenesis.” But how can there can be any doubt when the coordinates of the sample studied by Bindi (2026) map to the center of a railroad berm composed largely of construction aggregate.The Blackville slag finds are at site 7 on this 2019 map of the YDI-sites then known.*
No amount of circumspection prevented many of the authors from drawing on Bunch at al. (2012) to make definitive assertions of a YDB impact near Perkins, Louisiana (Fitzenreiter et al., 2025). I was asked by one author to examine samples from the site in advance of publication. My preliminary petrography suggested quench rates slower than those typically observed for small-scale impacts or short-duration airbursts. I reported that they either were anthropogenic or, less likely but plausibly, might be ejecta eroded from older impact strata that do occur up-gradient. However, a subsequent tour of the site and additional samples graciously provided by the lead author, revealed evidence that these glasses are most like those produced by petroleum fires. The Perkins site, in fact, sets in the middle of an area with abundant pimple mounds, which have been linked to gas extrusions.
The other material mentioned in this take-down text refers to the study by Fitzenreiter et al. (2025), published in the journal Airbursts and Cratering Impacts, asserts that a shallow seasonal lake/depression near Perkins, Louisiana, is North America’s first identified cosmic airburst crater dating to the Younger Dryas Boundary (YDB). The authors argue that the site preserves physical evidence of a low-altitude "touch-down" cosmic airburst that occurred approximately 12,800 years ago.
* (Map showing 24 sites containing Younger Dryas Boundary (YDB) nanodiamonds. The solid line defines the current known limits of the YDB field of cosmic-impact proxies, spanning 50 million km 2 , including Venezuela (open circle). Numbered sites are from this study: 1) Lake Cuitzeo, Mexico; 2) Daisy Cave, California; 3) Arlington Canyon, California; 4) Murray Springs, Arizona; 5) Lindenmeier, Colorado; 6) Bull Creek, Oklahoma; 7) Blackville, South Carolina; 8) Topper, South Carolina; 9) Kimbel Bay, North Carolina; 10) Newtonville, New Jersey; 11) Melrose, Pennsylvania; 12) Sheriden Cave, Ohio; 13) Gainey, Michigan; 14) Chobot site, Alberta, Canada; 15) Lake Hind, Manitoba, Canada; 16) Kangerlussuaq, Greenland; 17) Watcombe Bottom, Isle of Wight, United Kingdom; 18) Lommel, Belgium; 19) Ommen, Belgium; 20) Lingen, Germany; 21) Santa Maira, Spain; 22) Abu Hureyra, Syria. In addition, independent researchers have reported NDs at six sites, indicated by letters, four of which are in common: a) Indian Creek, Montana; b) Bull Creek, Oklahoma; c) Sheriden Cave, Ohio; d) Newtonville, New Jersey; e) Lommel, Belgium; f) Aalsterhut, Netherlands. Credit to Wittke et al. (2013); Kinzie et al. (2014). [Volker Dietrich])







