Dendrochronology is the art and science of using tree rings to count the age
of a tree. Tree rings change in width from year to year because growing conditions
are variable from year to year. Thus, a tree-ring chronology is a year-by-year
record of what trees “thought” of their growth conditions in the
past, for a particular species in a particular geographic region. (1) Tree
rings yield knowledge of ancient droughts, fires, cold spells, and heat waves.
Knowledge of past environmental downturns helps to understand what is happening
in our environment now and what may happen in the future.
One of the best chronologies in the world is the continuous record of Irish
oak growth for each of the last 7,400 years developed by Irish dendrochronologists
from the large number of ancient Irish oaks preserved in Irish bogs. They have
discovered, for example, that a “tree-ring event”, occurred in
3195 B.C., at the time that prehistoric people built the henge at Stonehenge
in Europe and the Egyptians started their civilization in the Near East! (2)
Another fine tree-ring chronology is the continuous record developed over the
past century by researchers with the American Laboratory of Tree-Ring Research
at the University of Arizona. (3,4) What is the history of dendrochronology,
how does the system work, and what are examples of climate catastrophes it
has identified?
History of Dendrochronology
The recognition that trees produce an annual growth ring goes back at least
to Theophrastus (370 -285 B.C.), a student of Aristotle (384 B.C. – 322
B.C.), who figured out the fresh growth formed on the outer circumference of
a tree. Leonardo da Vinci (1452 – 1519 A.D.) deduced the relationship
between ring width and moisture availability, which he used to reconstruct
past weather from earlier ring widths. In the 1700s, people were using the
annual character of the rings to count back from known felling dates to look
at specific growth years. In the 1800s, Charles Babbage (1791 – 1871
A.D.) presciently predicted (in 1837) that cross-dating trees--that is, overlapping
the patterns of wide and narrow rings from tree to tree, would eventually allow
the construction of long chronologies using the ancient trees in bogs and lakes.
(5-7)
American Astronomer-Dendrochronologist Andrew Ellicott Douglass
In the 1900s, the American astronomer Andrew Douglass (1867-1962), who ran
northern Arizona’s Lowell Observatory at Flagstaff, became interested
in how earth’s weather responded to variations in sunspots, the powerful
magnetic fields on the surface of the sun. He hit on the brilliant idea that
tree growth observed in tree rings might correlate with sunspot activity over
time—that is, when sunspot activity was high, tree growth would be high.
He also noticed that year-to-year variation (short-term growth) in tree ring
growth depended on the changing amounts of rainfall from year to year. Longer-term
growth trends, he postulated, were due to changes in solar activity over time.
He determined that the Arizona tree-ring record supported an 11-year solar
cycle back to about AD 1700, but a ten-year cycle in the 1700s. (8-9)
Hooked on tree-ring counting as a means to better understanding the sun, he
decided to extend the tree-ring record backwards in time as far as he could
by overlapping the wide and narrow growth-ring patterns from living Arizona
pines to the patterns from ancient archaeological timbers in various ruins
in the Southwest. “If the trees were growing over some common period
he could match their ring patterns over their common years,” explains
Irish dendrochronologist Dr. Mike Baillie. (10) Douglass acquired timbers from
ancient Pueblo ruins and elsewhere, extending his chronology back to 1284 A.D.,
but became frustrated with a “floating series” of trees, which
he could not link to any part of his existing chronology.
Finally, on June 22, 1929, a charred roof timber turned up from the Whipple
ruin at Show Low, Arizona, which enabled Douglass to link the modern and floating
chronologies, thereby extending his uninterrupted tree-ring chronology back
to 701 A.D. Suddenly the American Southwest had the best archaeological chronology
in the world!
European Dendrochronology
The main researchers interested in dendrochronology in Europe were Germans
Bruno Huber (1930-1999) and Veronica Giertz, who by the 1960s, had produced
a 1000-year central German oak chronology, while another investigator Ernst
Hollstein, working at Trier to the northwest, built another, which is almost
identical. (11) Later, a group of oaks from one field at Croston Moss in Lancashire,
England, provided a continuous chronology from 3200 B.C. to 970 B.C, with just
a single gap between 1680 and 1580 B.C. Baillie points out the need to pay
careful attention to stubborn “gaps” because they may suggest climatic
catastrophes that expunged trees from the record.
Two different groups of European workers found all the pieces of timber needed
to complete the Belfast and Gottingen tree-ring chronologies, which were in
precise synchronization back to 5000 B.C. By the early 1980s, dendrochronologists
had constructed chronologies dating back 7000 years. Since then German workers
have pushed back the tree-ring chronologies to 9000 years ago! (12)
Dendrochronologies Useful in Delineating Causes of Historic Famines and Plagues
Tree-ring chronologies have proved exceptionally useful in dating archeological
sites and providing invaluable environmental information about the past. This
information is independent of the potential bias present in human history.
The human written record frequently speaks of terrible “famines” and “plagues”,
but seldom are the physical causes delineated. Plagues and famines, however,
do not “just happen”. Something causes them to happen—a
physical cause or causes.
Why have historians over the millennia failed to record what they saw as the
causes of the famines and plagues they observed? “If something really
significant had happened, surely it would have been recorded?” argues
Baillie. (13)
The reasons are fourfold. First, the physical causes in many cases were physically
remote from the affected population(s). For example, a volcano that loaded
the atmosphere with dust could dim the sun, precipitating famines and population
dislocation far from the volcano, even on the other side of the earth. Second,
people assume that the historical record is more detailed than it really is.
Much of it has been lost. Third, early writers varied in their critical faculties.
Fourth, conditions may have been adverse to record keeping. “Witnesses
to truly catastrophic events may have been in no position to make a record,
having had other priorities such as survival.” (14)
Fifth, people in the position to selectively edit or destroy parts of the
historical record may have done so for a variety of reasons. Sixth, evolutionist
Charles Darwin and geologist Charles Lyell during the 19th century rejected
the idea of catastrophism (“environmental determinism”) suggested
by tree ring abnormalities, and instead strongly advocated uniformitarianism,
the assumption that the natural processes of the past are the same as those
that can be observed operating in the present. Even today, there is a strong
lobby against catastrophism. (15) Baillie argues, “So deep is the conditioning
that the environment is not a significant factor that no attempt is made to
understand the causes of famines and plagues which are perceived as ‘acts
of God’”. (13)
Example 1: The Narrow Ring Event in the Mid-17th Century B.C.
During the 1980s, tree-ring workers in Arizona noted that bristlecone pines,
which live at around 9,000 feet, are exquisitely sensitive to temperature,
especially in years affected by so-called volcanic dust-veils—where volcanoes
blast dust and water vapor high into the stratosphere and cause cooling on
the earth’s surface. (16-17) Bristlecones, because of their dense, highly
resinous wood, are not susceptible to invasion by bacteria, fungus, or insects
that prey upon most plants. Investigators identified an extreme frost event
in 1627 B.C., evidenced by an irregular tree ring signature, which prompted
Irish dendrochronologists to examine their Irish oak specimens dating around
1627 B.C.
Dr. Baillie and his colleagues discovered among their 22 bog oak samples from
that period one Irish oak with a band of seven narrow rings starting in 1628
B.C., and another series of trees showing the narrowest rings of their
lifetime during the decade of the 1620s. (16) Arizona bristlecone and Irish
bog oak researchers call their combined observations “historic synchronicity”,
which suggests that whatever happened in 1627 B.C. affected the entire globe.
One source concludes: “1628 BC, then, and the years immediately following,
were bad years in areas as widely separated as California, Northern Ireland,
the Aegean (presuming [volcano Santorini/]Thera was the culprit), and even,
perhaps, China. (18) Santorini was a volcanic island in Greece (Thera), known
to have erupted in the mid-second millennium B.C. (19)
The absolute dating of the Santorini eruption by dendrochronology confounds
archeologists who believe it erupted in the 16th, not the 17th, century, B.C.,
i.e., between 1550 B.C. and 1500 B.C. The dendrologists’ reckoning of
the timing of the Santorini eruption, which carbon dating and Greenland ice
core findings support, suggests the need for a rescaling of the well-established “conventional
Egyptian chronology” (i.e., the rulers of ancient Egypt), which archeologists
are debating, according to one source. (20-21)
Example 2: The Narrow Ring Event in the Sixth Century A.D.
In 1983, Stothers and Rampino drew attention to a major “dry fog” in
the year 536 A.D. recorded in Mediterranean histories. They attributed this
fog to a volcanic dust-veil, the most serious in 2,000 years. (22) Unfortunately,
the European oak chronologies, including the Irish oak chronology, do not validate
their assessment. Though the growth ring for 536 A.D. is somewhat narrow, a
much more severe growth reduction took place across 540 A.D., an event recorded
in tree rings around the world. Moreover, the Greenland ice core data available
up to 1997 showed “no good evidence” for a volcanic acid signal
in the time window 536-545 A.D. (23) What does this mean?
Something awful happened around 540 A.D., as described in detail elsewhere.
(24) The Plague of Justinian (540-451 A.D.) broke out in the Eastern Roman
Empire. Here we find no attempt in the historical record to determine the cause of
the plague, as noted above. However, several Roman observers wrote about bad
weather at the time. For example, one eyewitness, a Syrian bishop named John
of Ephesus, described the extraordinary events during the years 535 and 536
A.D. as follows: “There was a sign from the sun, the like of which had
never been seen or reported before. The sun became dark and its darkness lasted
for 18 months. Each day it shone for about four hours, and still this light
was only a feeble shadow. Everyone declared that the sun would never recover
its full light again.”
Cassiodorus writing in Italy also referred to a dimming of the sun: “We
have had a spring without mildness and a summer without heat ... The months
which should have been maturing the crops have been chilled by north winds.
Rain is denied and the reaper fears new frosts.”(24, 25)
If a volcanic dust-veil did not cause the narrow tree-ring event between
536 A.D. and 545 A.D., what did? The next most likely cause of atmospheric
loading after volcanism is either comet dust or airbursts associated with comets,
e.g., multiple Tunguska-class impacts, as described elsewhere. (26) British
astronomers Victor Clube and William Napier suggest that earth was at increased
risk of bombardment in the time window 400-600 A.D. (27)
Dendrochronology: The Past as Future
Tree-ring dating methods have identified intermittent severe climate catastrophes
in the past 7,000 years, raising the question, what caused the catastrophes
and their associated plagues and famines? The human historical record is rich
in allusions to catastrophes (e.g., the parting of the Red Sea during the Hebrew
Exodus from Egypt, and manna dropping from heaven, among dozens of others).
Until recently, however, most people have attributed these bizarre events to
metaphorical thinking, i.e., they didn’t really happen. Or did
they?
Dendrochronology, supported by carbon dating and Greenland ice core chemical
analyses, compels reassessment of the historical record. Moreover, the narrow
tree-ring findings that are not associated with volcanic acid signatures
in Greenland ice cores suggest we should be thinking about alternative sources
of atmospheric dust, i.e., comet dust. Dendrochronology makes us smarter about
what the future may hold.
Notes:
- Mike Baillie: Exodus to Arthur: Catastrophic Encounters with Comets.
B.T. Batsford, London, 2000, p. 255.
- Ibid, p. 9. See also Mike Baillie: A Slice Through Time: Dendrochronology
and Precision Dating. Routledge, London, 1996, pp. 16-31.
- “The Laboratory of Tree-Ring Research”, available at http://www.ltrr.arizona.edu/;
accessed June 3, 2007.
- Marvin Stokes, Terah L. Smiley: An Introduction to Tree-Ring Dating.
University of Arizona Press, 1996. See http://www.uapress.arizona.edu/books/bid1007.htm;
accessed June 3, 2007.
- Baillie, Exodus, p. 14.
- “Encyclopedia of World Biography on Charles Babbage”. Available
at: http://www.bookrags.com/Charles_Babbage;
accessed June 3, 2007.
- Maboth Mosely: Irascible Genius: A Life of Charles Babbage, Inventor.
Hutchinson Publisher, 1964.
- Baillie, Exodus, p. 15.
- Michelle Nijhuis: “Written in the Rings”. In High Country
News, January 24, 2005. Available online at: http://www.hcn.org/servlets/hcn.Article?article_id=15219;
accessed June 3, 2007.
- Baillie, Exodus, pp. 18-19.
- Ibid, p. 26.
- Ibid, p. 28.
- Ibid, p. 29.
- Ibid, p. 30.
- For more information on catastrophism, see:
- 16. Patrick McCafferty and Mike Baillie: The Celtic Gods: Comets in
Irish Mythology. Tempus, 2005, pp. 152-154.
- “The Ancient Bristlecone Pine” at: http://sonic.net/bristlecone/;
accessed June 3, 2007.
- The Thera Foundation: “Overview and Assessment of the Evidence for
the Date of the Eruption of Thera” at: http://www.therafoundation.org/articles/chronololy/overviewandassesmentoftheevidenceforthedateoftheeruptionofthera;
accessed June 3, 2007.
- McCafferty and Baillie, p. 212.
- “Santorini” at http://en.wikipedia.org/wiki/Santorini;
accessed June 3, 2007. See also “Conventional Egyptian Chronology” at http://en.wikipedia.org/wiki/Conventional_Egyptian_chronology;
accessed June 3, 2007.
- McCafferty and Baillie, p. 153.
- Richard B. Stothers and Michael R. Rampino: “Historic volcanism,
European dry fogs, and Greenland acid precipitation, 1500 B.C. to A.D. 1500”.
In Science, 1983, Volume 222, pp. 411-433. Available online
at: http://pubs.giss.nasa.gov/docs/1983/1983_Stothers_Rampino.pdf;
accessed June 3, 2007.
- McCafferty and Baillie, p. 154.
- SEMP Biot #214: “Did a Krakatoa Eruption in 535 A.D. Help Precipitate
the Decline of Antiquity and the Spread of Islam?” (May 16, 2005).
Available at: http://www.semp.us/publications/biot_printview.php?BiotID=214;
accessed June 3, 2007.
- Immanuel Velikovsky: Worlds in Collision. Laurel, 1968 edition,
pp. 145-149.
- “The Mystery of the Tunguska Fireball over Siberia”. In SEMP
Securitas Magazine, Volume 6, number 2 (April, May, June 2007). Available
online at:
http://www.semp.us/publications/securitas_reader.php?SecuritasID=32;
accessed June 3, 2007.
- Victor Clube and William Napier: The Cosmic Winter. Blackwell Publishers,
1990.