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For the second time in 10 years, Daulton has carefully reviewed the evidence, and found no evidence for a spike in nanodiamond concentration in Younger Dryas sediments. Because nanodiamonds are the strongest piece of evidence for the impact hypothesis, their absence effectively discredits it.
The Younger Dryas impact hypothesis or Clovis comet hypothesis originally proposed that a large air burst or earth impact of a comet or comets from outer space initiated the Younger Dryas cold period about 12,900 BP calibrated (10,900 14C uncalibrated) years ago. The hypothesis has been largely contradicted by research showing that most of the conclusions cannot be repeated by other scientists, and criticized because of misinterpretation of data and the lack of confirmatory evidence
originally posted by: gription
a reply to: Marduk
It hit the icepack. I thought this was known...
A study of Paleoindian demography found no evidence of a population decline among the Paleoindians at 12,900 ± 100 BP, which was inconsistent with predictions of an impact event. They suggested that the hypothesis would probably need to be revised. There is also no evidence of continent-wide wildfires at any time during terminal Pleistocene deglaciation, along with evidence that most larger wildfires had a human origin, which calls into question the origin of the "black mat." Iridium, magnetic minerals, microspherules, carbon, and nanodiamonds are all subject to differing interpretations as to their nature and origin, and may be explained in many cases by purely terrestrial or non-catastrophic factors
If it is assumed that the hypothesis supposes that all effects of the putative impact on Earth's biota would have been brief, all extinctions caused by the impact should have occurred simultaneously. However, there is much evidence that the megafaunal extinctions that occurred across northern Eurasia, North America and South America at the end of the Pleistocene were not synchronous. The extinctions in South America appear to have occurred at least 400 years after the extinctions in North America. The extinction of woolly mammoths in Siberia also appears to have occurred later than in North America.[35] A greater disparity in extinction timings is apparent in island megafaunal extinctions that lagged nearby continental extinctions by thousands of years; examples include the survival of woolly mammoths on Wrangel Island, Russia, until 3700 BP, and the survival of ground sloths in the Antilles,[39] the Caribbean, until 4700 cal BP. The Australian megafaunal extinctions occurred approximately 30,000 years earlier than the hypothetical Younger Dryas event
Scientists have asserted that the carbon spherules originated as fungal structures and/or insect fecal pellets, and contained modern contaminants and that the claimed nanodiamonds are actually misidentified graphene and graphene/graphane oxide aggregates. An analysis of a similar Younger Dryas boundary layer in Belgium yielded carbon crystalline structures such as nanodiamonds, but the authors concluded that also did not show unique evidence for a bolide impact.[44] Researchers have also have not found any extraterrestrial platinum group metals in the boundary layer which would be inconsistent with the hypothesized impact event. Further independent analysis was unable to confirm prior claims of magnetic particles and microspherules, concluding that there was no evidence for a Younger Dryas impact event
Research published in 2012 has shown that the so-called "black mats" are easily explained by typical earth processes in wetland environments. The study of black mats, that are common in prehistorical wetland deposits which represent shallow marshlands, that were from 6000 to 40,000 years ago in the southwestern USA and Atacama Desert in Chile, showed elevated concentrations of iridium and magnetic sediments, magnetic spherules and titanomagnetite grains. It was suggested that because these markers are found within or at the base of black mats, irrespective of age or location, suggests that these markers arise from processes common to wetland systems, and probably not as a result of catastrophic bolide impacts
originally posted by: gription
a reply to: Marduk
You can quote any source you like. The data trends towards a glacial impact. Show me your data.
originally posted by: gription
a reply to: Marduk
You can quote any source you like. The data trends towards a glacial impact. Show me your data.
originally posted by: Byrd
No surprise that it's dead. .
originally posted by: gription
a reply to: Marduk
You can quote any source you like. The data trends towards a glacial impact. Show me your data.
originally posted by: SyxPak
a reply to: Marduk
WOW! From Your link here is, in part, this!;
ABSTRACT: Fluvial sequences from the late Pleistocene to the Holocene are exposed in Arlington Canyon, Santa
Rosa Island, Northern Channel Islands, California, USA, including one outcrop that features centrally in the
controversial hypothesis of an extra-terrestrial impact at the onset of the Younger Dryas. The fluvial sequence in
Arlington Canyon contains a significant quantity and range of organic material, much of which has been charred.
The purpose of this study was to systematically describe the key outcrop of the Arlington sequence, provide new
radiocarbon age control and analyse organic material in the Arlington sediments within a rigorous palaeobotanical
and palaeo-charcoal context. These analyses provide a test of previous claims for catastrophic impact-induced fire
in Arlington Canyon. Carbonaceous spherular materials were identified as predominantly fungal sclerotia; ‘carbon
elongates’ are predominantly arthropod coprolites, including termite frass. ‘Glassy carbon’ formed from the
precipitation of tars during charcoalification. None of these materials indicate high-temperature formation or
combustion. Charcoal and other materials in Arlington Canyon document widespread and frequent fires both
before and after the onset of the Younger Dryas, recording predominantly low-temperature surface fires. In
summary, we find no evidence in Arlington Canyon for an extra-terrestrial impact or catastrophic impact-induced
fire.
originally posted by: punkinworks10
This team is being disingenuous in saying that nano diamonds have not been found in YDB layers, they have by a half dozen independant research groups from institutions worldwide.
So, IMO this lates set of papers is NOT the end of the discussion.
Black mats
Research published in 2012 has shown that the so-called "black mats" are easily explained by typical earth processes in wetland environments. The study of black mats, that are common in prehistorical wetland deposits which represent shallow marshlands, that were from 6000 to 40,000 years ago in the southwestern USA and Atacama Desert in Chile, showed elevated concentrations of iridium and magnetic sediments, magnetic spherules and titanomagnetite grains. It was suggested that because these markers are found within or at the base of black mats, irrespective of age or location, suggests that these markers arise from processes common to wetland systems, and probably not as a result of catastrophic bolide impacts
Impacted black mat sediment is present in the
WesternAlps, where it is found in surface clast rinds
embedded in LG moraine/rockfall sediment and in
paleosols of the western Alps near Mt Viso on the
French/Italian border. The same black mat deposits
are also found in theAndes, displaying glassy Fe/Crich
spherules and the presence of high fractures and
clast brecciation, complete with melted/quenched
and aerodynamically shaped microtextures. The
evidence at both sites is consistent with the sediment
being the product of cosmic airburst/impact. The
relationship with YD till is indisputable, and 14C
dates associated with the black mat beds in the
Andes, place the impact squarely within the YDB
window.
Evidence of cosmic impact in the Western Alps
occurs both in weathering rinds and within surface
paleosol Ah horizons, all of LG age. We report
finding highly fractured and brecciated weathering
rinds, complete with multiple impact-related channels
filled with melted and contorted grains. These
formed from a highly volatile and viscous mass of
molten material, now welded together into chains
of fused grains and coated with thick opaque
carbon, occasionally revealing the presence of Al
plus Cl considered to be impact-produced glass.
Although the relationship between the YDB and
the YD is still under discussion, it is clear that the
black mat extends to the European Alps, and it is
also clear that the evidence for it is found both in
weathering rinds and in resident grains of Ah paleosol
profiles. At the time of impact these Ah horizons
were likely C or Cox (ox = oxidized) soil horizons
undergoing the initial stage of weathering following
deglaciation. This is the first report of black mat
archival evidence recovered from weathering rinds
and from surface paleosol horizons. The spatial
evidence of deposit juxtaposition (the Alps) and
superposition (the Andes), strongly indicates cause
and effect regarding the black mat as related to the
YD. The geomorphological situation in both localities
is such that ice withdrawal during the Bølling
Allerød was interrupted by a glacial resurgence in
two widely separated interhemispheric areas, both
with indisputable evidence of a cosmic impact. In
the Andes,YDB dated beds were overrun byYD ice
while in the Alps cosmic impacted beds were partially
overrun and buried by YD moraines. It would
seem prudent for other workers to analyze rinds and
paleosols in similar venues in both areas to add to
the database presented here.