Paper No. 0
Presentation Time: 4:55 PM
MULTI PROXY STUDY OF LAKE SEDIMENTS REVEALS HIGH RESOLUTION RECORD OF MID-HOLOCENE ARIDITY
Kimble Pond (44º13'15" N, 93º50'24" W) and Sharkey Lake (44º35'39" N,
93º24'49" W) are two small glacial lakes in southern Minnesota, located near the present prairie -
forest ecotone. Sediments from these lakes yield a climate record for the past 12 ka B.P. at sub
decadal resolution throughout most of the Holocene. We used a combination of magnetic
parameters, pollen analyses, biogenic silica and LOI measurements to reconstruct paleoclimatic
changes throughout the Holocene. We show that the utilization of magnetic parameters, with
supporting data from other climate proxies, allows us extract high resolution records of
paleoclimate change from lake sediment archives.
Magnetic analyses are based on a combination of concentration (mag. susceptibility,
IRM) and grain size dependent (ARM / IRM) parameters that were measured at very high
resolution. At both sites the Holocene hypsithermal period lasts from 9.0 ka B.P. to 4.7 ka B.P.,
based on rock-magnetic measurements, which are confirmed by low resolution pollen counts.
An increase in clastic material, as seen through LOI and biogenic silica analyses, is reflected in
increased concentrations of coarse grained magnetic material, which leads to higher values of
mag. susceptibility and IRM and low ratios of ARM/IRM. Several marked peaks in IRM suggest
periods of extreme drought that occurred on a century scale throughout the main hypsithermal
period.
Magnetic susceptibility increases during this period as well, however, its dependence on
authigenic minerals, such as siderite make it less straightforward to interpret and a poor stand-
alone proxy of paleoenvironmental change.