An artist's depiction of a woolly mammoth. Mammoths likely roamed the Kenai Peninsula between the last two ice ages. |
MAMMOTH
DISCOVERIES
SEPTEMBER 2011
Author’s note: Since this
story was written nearly four years ago, more data are likely available, more
research has likely been done, and more discoveries may have been made or
reported. At some point, I will attempt to update and revise my information.
For now, however, please read this with the time gap in mind.
If the dog hadn’t been so annoying, the 2010 discovery might
never have occurred.
Kasilof resident Kevin Culhane and his friend, Tim Oliver,
had spent several hours of this summer day beachcombing unsuccessfully for
fossils along a stretch of sand and gravel south of Clam Gulch. They had walked
a considerable distance down the beach and were back within sight of their
truck when the trouble began.
Ava, Oliver’s excitable yellow lab, “got all agitated,”
Culhane said. “She started jumping up, trying to knock us down.” Irritated,
Culhane told the dog to leave them alone. “Go find a fossil!” he hollered. And
about 10 minutes later, she did.
Behind the two men, Ava had located something enticing. “I
heard rocks clanking together, and I looked right where we just walked, looked
behind us about 75 to 80 feet back, and this dog was chasing a rock around,”
Culhane said. “So I walked back there and picked up the rock and thought, ‘Oh,
that’s a cool-looking rock,’ and threw it in the backpack with the other rocks
and didn’t think about it. The next day I dumped out the rock pile and showed
my dad (Jim Culhane), and he goes, ‘Holy shit, that looks like a mammoth
tooth!’”
More precisely, it was about one-third of a complete mammoth
molar, which can be about the size of a woman’s hiking boot. “You can see the
fractured edge where it broke apart over the years,” Culhane said. “What was
more amazing was that a dog was interested in it,” he said. “It was just laying
on top of the beach, and the dog was excited about it, but she couldn’t fit it
in her mouth.”
Jim Culhane’s own excitement over his son’s find was later
tempered by concern: “He brought that thing home, and the next day we coated it
with concrete sealer ’cause it started cracking right away,” he said.
Such deterioration is common as fossils adjust from a moist,
sometimes saltwater environment to the relative dryness of most modern homes.
While applying a protectant to fossils may help preserve them and keep them
from breaking apart, however, the chemicals in sealants or lacquers may also
contaminate the fossils and make it difficult or even impossible to effectively
calculate their age through radiocarbon dating.
A few months later, someone very concerned with radiocarbon
dating and determining the age of items such as the mammoth molar contacted Kevin
Culhane.
That someone was Homer historian and field archaeologist
Janet Klein, whose 2008 book, Kachemak
Communities: Their Histories, Their Mysteries, contained a four-page
section entitled “A Mammoth Mystery.” Based on the appearance at that time of
five separate mammoth fossils discovered between the Homer Spit and the Anchor
River, Klein posed a hopeful notion: Mammoths may have once roamed the Kenai
Peninsula.
Then in early
2011, after consulting with Soldotna geologist Dick Reger, and with even more
fossil evidence in hand, Klein took her intriguing idea one step further: She approached
Homer News staff writer McKibben
Jackinsky to see if she would be interested in writing about the idea.
Jackinsky’s first article, “Woolly mammoth evidence increases,” appeared on
March 3, 2011.
Among the
improved evidence were two radiocarbon dates that seemed to point to mammoths living
on the peninsula during the warm period before the last ice age, which is
believed to have begun about 30,000 years ago and ended about 11,000 years ago.
From a fossilized mammoth molar, a Homer dentist helps to remove a sample so it can be sent to a lab for radiocarbon testing. |
“Although we
know that finding these eroded bones does not prove that mammoths lived on the
Kenai,” Klein said in the article, “ it strongly suggests that they did and, as
such, might encourage others to be more aware of this very fascinating
environment and the many stories it has to reveal to us.”
Those turned
out to be prophetic words.
After reading
Jackinsky’s article, Tim Klingbeil of Homer came forward with information about
a mammoth molar that his brother, Jack, had found in the late 1950s. Klingbeil’s
announcement led to another Jackinsky article, “More mammoth remains surface,”
on March 16.
The second
article led to a standing-room-only, brown-bag luncheon, featuring a
presentation by Klein and Reger, at the Alaska Islands and Ocean Visitor Center
on April 14, which is when Kevin Culhane reentered the picture.
Culhane, a
2008 graduate of Skyview High School, had heard about Klein’s investigation
into the mammoth mystery, and he called Jackinsky at the Homer News to announce what he had found and see if he could learn
more. Jackinsky took his telephone number and passed it on to Klein, who called
Culhane and then stopped in at his Kasilof home to see the fossil. She had him
relate the details of the discovery, including its precise location, and then
she invited Culhane to the luncheon.
Meanwhile, the
number of fossil finds rose to 12, and the story continued to grow.
Klein
herself, who had found a fossilized mammoth ankle bone on Bishop’s Beach in
1991, discovered a tusk fragment this June near Diamond Creek. She also learned
that several years ago a horn core believed to have belonged to a now-extinct
steppe bison—a contemporary of the woolly mammoth—was also discovered near
Diamond Creek.
The most
important discovery so far, however, has been the only fossil not found on or near a beach. In 2003, Klein
learned, Phil Gordon of Homer was fishing with a friend when he discovered a
mammoth tusk fragment four or five miles up Deep Creek, just above its
confluence with Silver Salmon Creek.
The location
of this fossil, which Gordon found on a gravel bar created by a recent flood,
is the best indication of the fossil’s origin—probably the nearby Caribou Hills.
“It was this piece that convinced me that we had a story,” Reger said. Before
that—although the idea of mammoths on the Kenai was tantalizing—Reger said that
the scientific side of him wouldn’t allow him to let go of other possibilities,
no matter how unlikely.
The beach
fossils, Klein once speculated, could have been transported to Kachemak Bay
from far away by glacial action. (Reger deemed this idea almost impossible.
Since fossils are not rocks, they would soon have been ground to dust by
glaciers.) The fossils could also be the discarded pieces of a collection
gathered in another area. They could have been traded to local Natives
by Natives from, say, the Bristol Bay area. Or they could even be part of an elaborate hoax.
But the Deep
Creek find made those remote possibilities even more remote.
Spurred on by
these finds and others, Klein and Reger arranged for four more samples to be sent
to an Outside lab for radiocarbon analysis, and they are currently awaiting the
results of those tests.
Chasing a Hypothesis
Dick Reger is quick to point out that what he and Janet
Klein believe about the possibility of woolly mammoths once roaming the Kenai
Peninsula is a hypothesis and not a theory.
“The magnitude of evidence that we have is pretty damn
small, compared to what we need to
have to make it a theory,” Reger said. “It may never be a theory—probably won’t—and that’s okay. That’s the way science
works. That’s the fun of it.”
The Random House
Webster’s College Dictionary defines hypothesis as a “provisional theory
set forth to explain some class of phenomena, either accepted as a guide to
future investigation (working hypothesis) or assumed for the sake of argument
and testing.”
Both Reger and Klein have stated that they believe that mammoths were once here,
but they want to know when, they want to know where, and they want to be sure.
To solidify their evidence—11 mammoth fossils so far, plus
one steppe bison fossil, all found between Clam Gulch and the Homer Spit—they
want to perform more radiocarbon dating. They also want to find more fossils,
or have others find them. And they really, really want to find a fossil in situ, a Latin term meaning literally
“in place,” or, more specifically,
“situated in its original or natural place
or position.”
Artist's depiction of a steppe bison. |
Their notion of the ideal discovery would involve another
fossilized mammoth tusk or bone or tooth still buried in sediment—along the cut
bank of a stream, for instance. Such a find, Reger said, could provide
stratigraphic context and allow for pollen samples from the site to help
determine the vegetation extant during the animal’s existence. As Reger stated
in a Homer News article on April 20,
“We could date not just the bones but other datable things like wood or
charcoal or whatever. It would give us a further fix on the age of them.”
As of early September, Klein and Reger had only two
radiocarbon dates to go on—and one of them was inconclusive. A tusk fragment
found four years ago about three miles west of Bishop’s Beach was analyzed by a
lab at the University of California Irvine and determined to be 27,040 years
old.
A fossilized mammoth ankle bone found 20 years ago on
Bishop’s Beach was also analyzed at UC Irvine but came back with an
indeterminate response because its age exceeded the 48,500-year limit of the
analytical method. The ankle bone could be only a few hundred years older than
the limit or even a few thousand years older, or more.
The good news was that both dates fit neatly into what is
believed to be the Middle Wisconsin interstade, the name given to the
approximately 30,000-year warm, wet period between the last two ice ages. If
mammoths lived on the peninsula between 30,000 and 60,000 years ago, the
conditions for their survival should have been quite favorable. Mammoths liked
to dine on the kind of tough, silica-rich grasses and other low plants that may
have thrived in the open peninsula country below the mountains.
Still, this good news opens the door to more questions:
First, how did the mammoths—shaggy, ruddy-colored grazing
mammals, some of which may have stood more than 10 feet tall, weighed as much as
six tons, and had tusks more than 15 feet in length—get to the Kenai Peninsula
in the first place, and when did they arrive?
Second, beside mammoths and steppe bison, what other mammals
inherent to the Pleistocene Epoch lived with them in this area? Was the
peninsula also home to prehistoric horses, the scimitar cat, the mastodon, the
short-faced bear, the antelope, and the yak, among many others?
Third—and perhaps most important at this stage in the
ongoing research—if the last ice age, which caused a worldwide glaciation that
may have lasted nearly 20,000 years, produced massive sheets of ice flowing
over the land and filling Cook Inlet and Kachemak Bay, how could mammoth
fossils survive the pulverizing power of the ice?
While the answer to the first question lies in evidence
collected by scientists from around the world, and the answer to the second
question relies on new discoveries, the key to answering the final question
seems to be ground solidly in geology, Reger’s life work.
In 2007, the State of Alaska’s Division of Geological &
Geophysical Surveys published A Guide to
the Late Quaternary History of Northern and Western Kenai Peninsula, Alaska, which
was researched and written by Reger and three other Alaskan experts in geology.
The guide traces, among other things, the movement of glacial ice during the
last three ice ages, dating back perhaps 150,000 years.
Each major glaciation reshapes the landscape through which
it travels, and those new shapes are the result of mass and pressure, direction
of travel, and rate of retreat, among other forces. Valleys are carved, lakes
are created, and new drainages are formed as the ground is scoured by the
weight of slabs of glacial ice over 1,000 feet thick.
The evidence for these movements includes the observation of
glacial moraines, ancient lake beds, abandoned drainages, and rock scarring
high in the mountains.
Part of Reger's investigation of Alaska's geologic past. |
Interestingly, each of the last two glaciations has been
less extensive than the one that preceded it, meaning that the ice did not fill
the landscape as completely as it had in the previous ice age. Evidence
suggests that during the most recent glaciation—although the Kenai Mountains
were nearly buried in snow, the inlet was full of ice year round, and a giant
freshwater lake was wedged between the frozen inlet and the highlands—a
510-square-mile section of high country between the Kenai Mountains and the sea
was probably left untouched.
This “untouched” land lay in what is now known as the
Caribou Hills, and this refugium (as such places that escape the rigors of
change occurring elsewhere are called) may be the reason that the citizens of
the southern peninsula are finding any remains at all.
Fossils deposited anywhere else have likely been crushed by
the passage of ice, but fossils from the Caribou Hills seem to have been spared
and are just now, more than 10,000 years after the end of the last ice age,
being discovered.
Reger speculates that the fossils have traveled downhill slowly,
drawn by the forces of water and gravity, from the high country to the sea.
“I realized that they had to be carried from where they were
laid down,” Reger said. “They had to be brought from there (in the Caribou
Hills) down to the beach after the last ice age. They wouldn’t have survived
the last ice age down there in Homer (where the glacial ice was thick). They
were up there in the surface sediments up on the Caribou Hills and were brought
down the creeks and down the scarps and slopes by mass-movement processes that
could carry them—debris flows made up of
mud and carrying trees, brush, and chunks of coal and rocks—but it was a less
rigorous, less active, less damaging medium to carry them in than a stream
flood would have been, with boulders that would have hammered the fossils
and crushed them.”
Such movement, he said, occurs infrequently—maybe once every
50 or 100 or even 200 years—making the fossils’ journeys seem almost
imperceptible.
The lone fossil found away from the ocean—Phil Gordon’s 2003
discovery, after one of these major flooding events—helped convince Reger. Because
the gravel bar upon the fossil lay was located above the confluence of Deep
Creek and Silver Salmon Creek but just below the rocky canyon walls at that
part of the drainage, Reger could infer that the fossil must have traveled down
Deep Creek from the nearby high country.
The upper Deep Creek drainage in the Caribou Hills. |
Reger and Klein decided to have Gordon’s tusk fragment and
two other fossils radiocarbon dated, this time at the renowned Beta Analytic
lab in Florida.
As to the question of how the mammoths arrived on the
peninsula, Reger said that the evidence suggests that mammoths likely came to
Alaska from Siberia over the Bering Land Bridge and eventually spread southward
and eastward across a wide range of North America.
From the Interior, mammoths appear to have moved south through
passes in the Alaska Range and entered
the Kenai Peninsula during the Middle Wisconsin interstade. Reger said
that it is possible that mammoths populated much of the peninsula lowlands
during this time, but no fossil record is known to exist outside the
unglaciated Caribou Hills refugium.
Elsewhere, the Late Wisconsin glaciation would likely have destroyed or buried
any fossils, including mammoth remains.
As the glaciation developed, mammoths living on the Kenai
were likely squeezed into a smaller and smaller habitable environment
and eventually perished, even in the Caribou Hills.
“I don’t believe that a viable mammoth population could have
survived in the Caribou Hills refugium during the last major glaciation,” Reger
said. “The Caribou Hills refugium covered only about 500 square miles, which
sounds like a lot but really isn’t when you consider how many large mammals had
to live there to be a viable population and how depauperate (underdeveloped in
impoverished conditions) the flora must have been. There simply was probably
not enough to eat.”
Meanwhile, the research continues, with both Klein and Reger
appreciative of the skills and knowledge that each of them has brought to this
broadening investigation.
“Janet Klein has been an absolute key point, a lightning
rod, for this whole thing,” Reger said. “None of this would have happened
without her interest and her effort and the trust that the people in the Homer
area have in her.”
Klein deflects the praise toward Reger and the individuals
coming forward with specimens and observations. “This project exemplifies the
value of citizen science wherein many people found and shared information and
ancient mammal remains with others so that all of us can better understand the
Kenai Peninsula,” she said. “These mammoth and bison remains are becoming truly
significant primarily because Dick Reger is giving his time and expertise to
ground them in the geology of the peninsula. Without geologic context, the
specimens would simply be wonderful and exotic objects.”
Good Fortune and Good Science
The flood changed everything, revealing what has thus far been
the most important piece in an intriguing archaeological and geological puzzle.
Prior to the flood, Phil Gordon of Homer had been “putzing
around” up Deep Creek for years, fighting through a mass of vegetation that he
referred to as “a stinking jungle, all full of bears and brush and barely
passable.” After the flood, however, the whole lower Deep Creek area opened up.
“It changed the river and topography enormously,” Gordon said. “It was a
veritable freeway.”
Usually Gordon trekked upstream with a friend, typically on
a fishing excursion, and such was the case in the late summer of 2003.
A segment of fossilized mammoth tusk. |
“My buddy and I were fishing for dollies,” Gordon said. “He
is a great fisherman, but I am sort of an indifferent fisherman. It’s a good
excuse to go, but if I don’t catch anything it can be every bit as good. He’s
busy casting and fishing and changing lures and trying flies, and I’m busy
seeing what I can see.”
Gordon said he found “a variety of bear bones, a number of
moose antlers, and a huge variety of things that had been unearthed by that
enormous flood,” and he delighted in the search at the expense of the fishing.
“I was just happy, happy, happy,” he said. “I walked across
a bit of a sandbar, and there was just about four inches of the mid-part of the
tusk showing. It’s brownish and it looks like wood, but there was something
about it that arrested my gaze, so I stopped and walked back. I often do this.
I’m not great at making miles and miles and miles. I used to run everywhere,
but these days I spend a lot more time just looking around. So I dug it out.
It’s not a monster. It’s not the whole tusk, certainly not the whole mammoth,
but it was a hoot to find because I had a pretty good idea what it was.”
The heavy
tusk fragment was about 16 inches long, he said, about four inches in diameter,
and with nearly the same specific gravity as basalt. When the radiocarbon date
came back on it from the Beta Analytic lab earlier this month, Gordon learned
that his piece of the past was approximately 31,740 years old. During that same
week, Elaine Brown of Homer also learned of a radiocarbon date. In 2008, Brown
had found a mammoth molar on Bishop’s Beach in Homer, and Beta Analytic announced
that it was 40,080 years old.
Reger and Klein were cheered by the new data. They announced
the new radiocarbon dates publicly at a standing-room-only mammoth presentation
in a meeting room at the Aspen Hotel in Soldotna. They also informed the
audience in the packed room that the new dates fit perfectly into their working
hypothesis.
Klein also encouraged the audience at the presentation to come
forward with any discoveries, but “if and only if they were found on the Kenai
Peninsula” and they know the location of the discovery. “If found in situ, the specimen should be left in place, should not be disturbed,”
she said. “The finder should photograph it in the context of the surroundings,
take a GPS reading or other means of relocating the object, and report it to
Dick or me or whomever might be the land owner.”
In most cases, Klein said, the collection of such items is not
illegal. It is, however, against the law to remove fossils from private
property.
So the search goes on in a project that Klein says has
relied so heavily on citizen contributions. And citizens such as Phil Gordon
can keep looking and continue to place more pieces into an intriguing puzzle. Gordon
has, in fact, continued searching since his big discovery almost a decade ago. “I
do believe it was an enormous fluke to find it, certainly finding it in the
condition that it was, mostly buried in mud and sand,” he said. “It was
certainly a surprise, and I don’t anticipate that I’ll find another one, but I
love to look.”
Reger indicates a sampling site on a fossilized mammoth molar. |
------------------
A TIMELINE OF MAMMOTH-RELATED FOSSIL DISCOVERIES
A TIMELINE OF MAMMOTH-RELATED FOSSIL DISCOVERIES
[Note: Some individuals who
have found fossils prefer to keep their identities private.]
Mid-1950s—According
to recent testimony from a Ninilchik woman, a mammoth molar was uncovered by a
slide along the bluff above the beach about two miles south of Clam Gulch.
1958 or 1959—Teen-ager
Jack Klingbeil of Homer found the fossilized molar of a woolly mammoth on the
beach near Bidarka Creek. He sold the tooth for $10 to Hazel Heath, owner of
Alaska Wild Berry Products in town. Heath exhibited the tooth on a shelf in the
store, and a later owner of the store placed it and some other objects into a
glass exhibit case about 15 years ago. The molar is still there, although it
has dried over the years and split into several pieces.
1976—Homer
resident Judy Winn found a tusk fragment on the beach on the Spit.
1989—Harold
Shafer found a fossilized mammoth molar on the beach a few miles south of the
Anchor River mouth.
1991—Janet Klein
of Homer found a mammoth astragalus (anklebone) on Bishop’s Beach. Later,
radiocarbon dating could not accurately determine its age because it exceeded
the 48,500-year limit of such testing.
1993—Klein and
others verified the identification of a mammoth molar found by a Homer resident
just east of Bidarka Creek. The fossilized tooth was eventually given to family
members overseas.
Five to 10 years ago—A
Homer nurse found what was believed to be a steppe bison horn core on the beach
near Diamond Creek. Unfortunately, the core, which is composed of fairly porous
material, had been contaminated by some sort of natural or synthetic acid,
perhaps petroleum-based chemicals transported by wave action onto the beach.
This horn core is, thus far, the only non-mammoth fossil discovered.
2003—Phil Gordon
of Homer discovered a mammoth tusk fragment on a gravel bar about 4-5 miles
upstream from the mouth on Deep Creek. Because of its location far away from
the beach—and theoretically closest to its origin—this fossil is considered one
of the most important finds. Radiocarbon testing indicated that the fragment
was 31,740 years old.
2007—Mike Lettis
of Anchor Point found a tusk fragment on the beach about three miles west of
Bishop’s Beach in Homer. Later, radiocarbon dating indicated an age of about
27,040 years—placing it near the ending of the last worldwide warming period
and near the beginning of the last ice age.
About 2008—Elaine
Browne of Homer found a mammoth molar on Bishop’s Beach in Homer. Radiocarbon
testing indicated that the fragment was 40,080 years old.
2010—Kasilof
resident Kevin Culhane found a fragment of a mammoth molar on the beach near
Corea Creek, south of Clam Gulch.
June 2011—Janet
Klein found a tusk fragment on the beach near Diamond Creek. The tusk fragment became
the 12th“element” found that appears to support the idea that mammoths and
other fauna of that time period once lived on the Kenai Peninsula.
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