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Books > Earth & environment > Earth sciences > Palaeontology > General
This thesis encompasses a study of past precipitation patterns
based on six cave stalagmites from different parts of the Indian
Himalaya. This is the first speleothem study in the Indian Himalaya
that shows a direct relationship between past precipitation and the
collapse of civilization. The stalagmites examined were KL-3 from
Jammu and Kashmir; TCS and BR-1 from Himachal Pradesh; and DH-1,
SA-1 and CH-1 from Uttarakhand. Based on the high-resolution
palaeoclimatic reconstruction (35 U/th dates, 5 AMS dates, 1,500
samples for 18O and 13C values) obtained for the duration of the
Pleistocene-Holocene transition (16.2-9.5 ka BP) and
Mid-Holocene-Present (ca. 4.0 ka BP-Present), three major events
were identified, namely the Older Dryas (OD), Bolling-Allerod (BA)
period and Younger Dryas (YD) at ca. 14.3-13.9, 13.9-12.7 and
12.7-12.2 ka BP, respectively. The study showed a gradual reduction
in the precipitation from 4 ka BP onwards for about a millennium
with a peak arid period between 3.2 and 3.1 ka BP. According to the
findings, the LIA (Little Ice Age) covers a time span from
1622-1820 AD, during which the climate was wetter than that in the
post-LIA period (1820-1950 AD). In addition, this thesis supports
the assumption that the WDs (Western Disturbances) contribute
significantly to the total rainfall in the Himalaya region.
During an expedition in Sonora, Mexico, paleontologist Mark A.
S. McMenamin unearthed fossils of creatures dated at approximately
600 million years old -- making them the oldest large body fossils
ever discovered. These circular fossils, known as Ediacarans,
seemed to defy explanation. Representatives of marine life forms
that existed in Precambrian times, as much as fifty million years
before life on earth began to diversify rapidly, the specimens bore
a superficial resemblance to jellyfish.
A typical Ediacaran had a quilted body, three curving arms at
the center, and a fringe of fine radial lines. McMenamin's
curiosity was fueled by the puzzle of whether the Ediacarans were
animals or some other type of organism. How could such complex
forms of life appear so suddenly, without extensive records of
prior evolution? Yet, this seems to be exactly what the Ediacarans
had done.
"The Garden of Ediacara" presents a mesmerizing documentary of a
major scientific discovery, detailing McMenamin's trip to Namibia,
where, with a party that included the renowned paleontologist Adolf
Seilacher, the author investigates a spectacular cast made from a
colony of fossils in the Nama desert. He chronicles the long, often
futile search made by earlier scientists for Ediacara, which began
more than a century ago in Europe, North America, and Africa, and
the various types of Ediacaran fossils that have been uncovered in
the years since.
McMenamin concludes that Ediacarans were not animals because
they never passed through the ball-shaped embryonic stage peculiar
to known animal life forms. But, remarkably, Ediacarans seem to
have developed a central nervous system and a brain independent
from animal evolution. This startling conclusion has profound
implications for our understanding of evolutionary biology, for it
indicates that the path toward intelligent life was embarked upon
more than once on this planet.
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