| 50
Arctic Lakes Show
Dramatic Warming
Queen's
University
Posted April 9, 2003
Dramatic
clues to North American climate change have been discovered
by a team of Queen's University scientists in the bottom of
50 Arctic lakes.
Using
innovative techniques that enable them to collect historic
evidence from fossilized algae in lake bottom sediment, the
researchers have found signs of marked environmental changes
in a variety of lakes of different depths and composition,
within a 750-km region bordering the northern tree-line. The
changes are a signal of things to come in the rest of North
America, say the Queen's paleolimnologists.
"We're
seeing a significant, regional change in the ecology of these
lakes over the past two centuries that is consistent with
warmer conditions," says Dr. John Smol, Canada Research
Chair in Environmental Change and co-head of the university's
Paleoecological Environmental Assessment and Research Laboratory
(PEARL). Dr. Smol conducted the study with Dr. Kathleen Rühland
and student Alisha Priesnitz of Queen's Biology Department.
"Because
the Arctic is a very vulnerable environment and usually the
first area of the continent to show signs of environmental
change often to the greatest degree it's considered
a bellwether of what will happen elsewhere," says Dr.
Rühland. "These are important signals that all of
us should be heeding: the lakes' sedimentary records have
tracked marked and directional ecosystem changes."
The
Queen's study will be published this month in the international
journal Arctic, Antarctic, and Alpine Research.
To
reconstruct past environmental trends, the team used fossil
markers (tiny algal cells) preserved in lake sediment. Sediment
cores were collected by helicopter from the 50 lakes, in an
area from Yellowknife, NWT, in the Boreal forest area towards
the Bering Sea in the Arctic tundra. For each lake, they compared
fossilized algae preserved in the top, most recent sediment
layer with those from the bottom, pre-industrial layer dating
back about 200 years.
They
found that the aquatic habitat of today is much different
from that of pre-industrial times. More fossils of the type
that live in open water environments were found in the top
(most recent) layer of sediment an indication that
these lakes have less ice cover and a longer growing season
that would alter important lakewater properties such as light
availability and the way lakes stratify, as a result of warming.
This marked a major ecological shift in the lakes that coincides
with a period of increased human industrial activities and
emissions in more southern regions.
Earlier
PEARL studies in the High Arctic tundra had indicated major
changes in the different layers of fossils associated with
climate warming. The new findings bring the effects of climate
change closer to populated areas. "The logical extension
was to see if tree-line lakes also show these dramatic changes,
and this study confirms that the impact is even greater than
previously documented," says Dr. Rühland. "We
believe that the consequences of greenhouse gas emissions,
in the form of climate change, are already having a notable
impact on the Arctic environment."
As
well as affecting plant and animal life in this region, melting
permafrost and less ice cover are already beginning to have
repercussions on human concerns such as transportation, housing,
and even sovereignty issues.
Last
year an entire Nunavik community was relocated by the Quebec
government after melting permafrost caused houses to slide
from their foundations. Other researchers have found evidence
that ocean ice is thinning, which could have future implications
for intercontinental transportation routes.
"Until
recently, no one was reconstructing Arctic climates in this
way, because the technology didn't exist," says Dr. Smol.
"Now that we can, in essence, reconstruct the past through
this indirect technique, we're filling in gaps in our knowledge
and finding answers to many ecological and environmental questions
that have great significance for the future."
Queen's
University
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