6. Considering the Paleontological Evidence
Problem 18: The comet explosion
theory does not account for the two millennium duration of the
Pleistocene extinction. Firestone and West propose that their
comet explosion catastrophe occurred at the Alleröd/Younger
Dryas boundary. Hence according to their theory most of the casualties
should have occurred at this time within a matter of a day or
so. However, the mass extinction did not transpire just in a
matter of days as their theory suggests. It had already been
underway for at least two thousand years prior to that date.
For example, Donald Grayson and David Meltzer (2003)
note that of the 35 genera involved in that extinction, only
15 can be shown to have lasted beyond 12,000 C-14 years ago (13,900
calendar years b2k) with the implication that the majority became
extinct over a millennium prior to the AL/YD transition. While
these authors advance this as an argument against the Prehistoric
overkill hypothesis, it is equally valid against a terminal comet
event. In a May 2007 news interview, Dr. Meltzer noted that the
earlier extinction dates for certain genera give reason for doubting
the Firestone-West comet theory (Roach,
2007).
Evidence of the extended character of the Pleistocene
extinction may be seen in figure 10 which has been adapted from
a "death rate" histogram published in 1983 by Drs.
Meltzer and Mead. It charts the temporal distribution of dates
on the remains of extinct megafauna taken from various North
American sites and shows the number of remains found in each
of a consecutive series of time slots, plotted here in terms
of calendar years instead of radiocarbon years. The dark histogram
bars represent dates occurring prior to the Allerod/Younger Dryas
boundary date while the light bars represent dates occurring
more recently than that boundary date. The lower pixilated bars
represent the subset of more reliable radiocarbon dates. As can
be seen here, the megafaunal death rate rose precipitously around
14,350 calendar years b2k, and for 1400 years maintained a relatively
high mortality level up to the 12,950 years b2k Younger Dryas
boundary date. This poses a problem for the Firestone-West comet
theory which attempts to explain the extinction with a short-term
comet explosion event or events occurring at the AL/YD boundary.
(click
to enlarge)
Figure 10. Upper profile: chronological distribution
of calendar dates on remains of extinct land mammals from 163
North American locations. Black bars indicate dates earlier than
12.9 kyrs b2k. Pixilated bars indicate the subset of more reliable
dates. Adapted from radiocarbon histograms published by Meltzer
and Mead (1985) and Martin
(1987). Lower profile:
The rate of meltwater discharge from the North American ice sheet
as indicated by the oxygen isotope profile for Gulf of Mexico
core EN32-PC4 (after Broecker et al., 1989).
Geophysical correlations with the death
rate histogram. In viewing the Meltzer-Mead
histogram, one notes a striking correlation between the onset
of increased mortality and climate. The peak spanning the interval
14,350 to 13,800 years b2k coincides with a time of peak warmth
during the Bolling Interstad, which coincided with a sharp rise
in meltwater discharge from the ice sheets, evident in Gulf of
Mexico salinity records. The Bölling/Allerod warming was
not restricted just to the Northern Hemisphere, but was a period
of global warming that is not easily explained as arising due
to endogenous fluctuations of the Earth's climatic system (LaViolette, 2005c). In other words,
some external effect must have been perturbing the Earth to cause
temperatures during this period to rise to levels typical of
interglacial periods at a time when the ice sheets were near
their maximum extent. It is difficult to pass off the association
of this warm period with the rise in megafaunal death rate as
a coincidence. The superwave theory proposes that the megafaunal
extinction arose because of hazardous effects from a highly active
flaring Sun. It also suggests that the glacial meltwater flooding
which occurred during this period of global warming posed an
additional hazard. As noted earlier, this also was related to
the superwave cosmic dust incursion.
Evidence that supersized solar flares played an important
role in the megafaunal extinction is indicated by the highly
elevated radiocarbon production rate that occurred from 13,500
to 12,800 years b2k and which is evident in figure
1. As seen in figure 10, this period spanned the highest
peak in the megafaunal extinction histogram. Spurts of C-14 production
are also found to coincide with earlier peaks in the histogram,
including one close to the time of the Gothenburg geomagnetic
excursion. We also have evidence from the lunar data of Zook
et al (1977) that the deglacial
period was marked by highly elevated solar flare activity.
Problem 19: The progressive rise in atmospheric radiocarbon
and the progressive YD cooling does not fit the abrupt signature
of a comet explosion. As mentioned
earlier, it is unlikely that a comet explosion or impact would
itself produce such a large increase in radiocarbon. Besides
if this were the case, there should have been an abrupt spike
in C-14 of a few years duration, a time comparable to the atmospheric
residence time of dust from a comet explosion.. Instead we see
a progressive rise with most occurring over a 200 year period
following the beginning of the YD cooling. Also we see that an
early phase of the rise actually began around 13,500 years b2k,
well before the time proposed for the comet explosion. The short
duration of an impact event also has difficulty explaining why
climate progressively cooled for two centuries. Dust from an
impacting comet would have settled out within a few years. So
why did climate continue to cool and why was this cooling accompanied
by a progressive increase in C-14? The comet theory has no answer.
Problem 20: A firestorm induction of the YD climatic
cooling does not conform to ice core evidence. According to the supernova/comet theory, fires
were ignited at the time of the YD boundary comet explosion (or
impact), aggravating and likely extending the cooling caused
by the aerial dispersal of cometary dust. The theory's backers
claim that evidence of this firestorm is to be found in the "black
mat" also termed the "Usselo Horizon," a sooty
layer formed both in North America and Europe during this AL/YD
transition and attributed to the widespread occurrence of forest
fires. However, ice core evidence suggests that this conflagration
occurred over a century after the YD cooling had already commenced.
Ion data from the GRIP and GISP2 Greenland ice core records register
this burning as a many fold increase in formate, oxylate, and
ammonium ions, all indicators of biomass combustion. But, it
shows that this rise occurred about a century after the date
when climate first began to cool, as indicated by the date when
the oxygen isotope ratio began its progressive decrease to cooler
temperatures.
Atmospheric dust, and possibly soot, also increased
about the time of this increase in oxylate and formate, as indicated
by a decrease in the light transparency of the GISP2 Greenland
ice core. Ice core transparency declined about 125 ± 15
years after the isotope decline that marked the beginning of
the YD cooling. This would be around 12,885 years b2k relative
to a YD boundary date of 13,010 years b2k based on the Cariaco
Basin varve chronology. Examining the ammonium and nitrate ion
concentration data for this portion of the GISP2 ice core record
(Mayewski, 1994) and high-resolution ammonium ion data spanning
the corresponding section of the GRIP ice core record (Fuhrer,
et al.,1996), we find that these indicators attained very high
values from 12,884 to 12,853 years b2k, marking an event whose
magnitude was unique and that has not recurrred since. This ice
core evidence is discussed in detail in the latest update of
my dissertation Galactic Superwaves and Their Impact on the
Earth Environment (LaViolette, 2008). Based on this polar
ice evidence, we may determine that this conflagration began
12,884 years b2k and lasted for three decades. Interestingly,
this falls close to the time of one of the two largest C-14 production
spurts in the entire Cariaco Basin record which dates at 12,887
± 10 years b2k. This implicates a super-sized solar storm
as being the cause of this ignition, and not necessarily a comet
impact. A study of the high-resolution oxygen isotope profile
for the GRIP ice core obtained by Johnsen, et al., (1997) shows
that climate in Greenland underwent a dramatic an abrupt warming
following the occurrence of this solar event, changing from glacial
to interglacial temperatures within two years. This warming
was likely due to the immense amount of energy imparted to the
Earth's atmosphere by the solar proton event. It was quickly
followed by a dramatic cooling which may be attributed to the
screening of sunlight by the smoke laden air.
This global conflagration, then, cannot be blamed
as the cause of the YD cooling since by that time climate had
already cooled almost to the YD temperature low. The cooling,
which had already been in progress for 125 years prior to that
time, must be attributed to a cause other than a comet impact
and its proposed firestorm. Solar flare cosmic rays appear to
be the most likely choice. Solar cosmic rays striking the atmosphere
would have ionized the atmosphere, producing large quantities
of condensation nuclei which would have seeded cloud formation.
The resulting global increase in cloud cover would have resulted
in a global climatic cooling. In support of this, we find that
periods when atmospheric radiocarbon was increasing, i.e., periods
of high solar activity, coincide with times of climatic cooling.
Furthermore such a solar flare-climate connection explains why
dust peaks in the polar ice record recur with the solar cycle
period (Ram and Stolz, 1999; Donarummo,
2002). Solar cosmic rays would have induced the formation
of clouds having droplets too small to produce rain, resulting
in a period of greater aridity and atmospheric dustiness.
Problem 21: Proposed thermal neutron flux intensities
way too high. When Firestone first
discussed the YD boundary extinction in 2001, he had suggested
that the C-14 anomaly was produced by cosmic rays from a supernova
explosion. At that time he did not give a date for the supernova
explosion, but four years later he and West (LBNL,
2005) suggested that the event took place 41 kyrs b2k with
cosmic rays and high-velocity extraterrestrial material from
the outburst arriving around 34,000 and 12,950 years ago. Firestone
and Topping (2001) had proposed
that on the AL/YD boundary date thermal neutron fluxes reached
as high as 1017 neutrons/cm2, and Firestone (2002)
later quoted fluxes as high as 1020
neutrons/cm2. Based on the
calculations of Southon and Taylor (2002),
these levels would translate into the equivalent absorption of
between 106 and 109 rads per hour, or to an energy influx of 105 to 108 ergs/cm2/s. This is between 10% and one hundred times the
level of insolation that the Earth receives from the Sun. If
this were the case, it is difficult to understand how their proposed
four kilometer diameter frozen cometary mass would have made
its 250 light-year journey to the solar system intact. For if
it were accompanied on its journey by such high cosmic radiation
intensities, it should have been entirely vaporized. The Earth,
then, should have been struck by a hot nebular wind, not by a
frozen cometary mass.
Moreover, in their critique of Firestone and Topping's
article, Southon and Taylor have pointed out that if the Earth's
atmosphere had been exposed to neutron fluxes even as high as
1017 neutrons/cm2, over a 1000 km diameter region, radiocarbon produced
from neutron bombardment of Earth's nitrogen atmosphere should
have increased atmospheric C-14 levels globally by a millionfold,
leaving current C-14 levels thousands of times higher than are
actually observed. This is not to say that cosmic ray radiation
did not play a critical role in the terminal Pleistocene megafaunal
extinction, but not quite in the fashion that Firestone, Topping,
and West have suggested.
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