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Click here for a printable version
(PDF) of the Winter 2007 issue. Lake
Tides - The
newsletter for people interested in Wisconsin Lakes
- a quarterly publication of the University
of Wisconsin-Extension Lakes Program - part of the
Wisconsin Lakes
Partnership.
Volume 32 No. 1 Winter 2007
Text-only version (HTML format)
Paleolimnology: History in the Mucking Lake
District Q&A EPA Launches National Lake
Survey
2007
Wisconsin Lakes Convention
-
Agenda
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Online Registration Calendar
Reflections
Paleolimnology:
History in the Mucking
Lake folks often get into
lively discussions over what the lake used to be like...more
plants, fewer plants, clear water, murky water... Is there any
way to really know for sure? Well, the answer is yes! In fact we
can have a good idea of what lakes used to be like hundreds of
years ago with a science called Paleolimnology.
Paleolimnology, sometimes referred to as
"History in the Mucking," is the interpretation of past
conditions and processes in lake basins. Each year since their
formation, a steady rain of sediments, plant pieces, creature
parts and other materials settle to the bottom of our lakes
leaving a record of past conditions. Over the eons this
fascinating record has remained safe and sound in the sediments
waiting for someone who could unlock its secrets. In addition to
providing background information on a lake, the sediments hold a
record of natural and human disturbances that have occurred in
the lake. The response of the lake to these disturbances
provides insight into how the lake functions, and provides a
better understanding of the significance of trends observed with
modern monitoring programs.
Obtaining a Sediment Core
To extract the lake’s past history a sediment core is usually
collected using some type of a hollow tube. The tube is pushed
into the lake bottom and a cap is remotely placed on top of the
tube to hold the sediment in place until it can be returned to
the surface. Once collected, the core is sectioned into
intervals usually of 1-2 cm. Each of these sections represent
sequential chapters in time, with the top of the core being
today and the bottom of the core indicating some time in the
past. The time frame of interest in paleolimnological studies
often is the last 200 years, which typically covers the impacts
of European settlement.
Questions Answered with Paleolimnology
T he science of paleolimnology can
reveal many secrets from a lake’s past life. Most natural and
human disturbances affecting lakes can be evaluated using
paleolimnological approaches. Nutrient increases and acid rain
are issues that have been extensively documented and studied
with paleolimnology. Paleolimnology can give us details on the
severity of human impacts and tell us within a few decades of
when the impacts began. The genesis of events such as erosion,
organic pollution from sewage treatment plants and animal feed
lots can all be documented. Paleolimnologists can tease many
messages from the sediments, such as how many and what types of
aquatic plants grew in the lake, changes in species composition,
past fish populations, or the frequency of algal blooms. Most
recently, trends in climate change are being studied with
paleolimnological techniques.
Dating Sediment Cores
An accurate sediment chronology is an
essential part of a paleolimnological study. Cores are usually
dated to establish the timing of past environmental changes and
to determine the rate of input of materials into a lake.
Paleolimnologists can accurately date sediment layers because
they can be cross-checked against known historical events.
Cores are typically dated by analyzing a series
of samples from the surface to a core depth that corresponds
with 200 years ago. The most common dating technique for
sediments deposited within the last 200 years is the lead-210
technique. Lead-210 is a naturally occuring atom that exhibits
radioactivity. It enters lakes primarily through precipitation
and dry deposition (i.e. dust), following the decay of an
atmospheric gas called radon-222 (radon gas).
Several methods can be used to corroborate the
lead-210 dating technique. Testing of atomic weapons has left
stratigraphic markers (layers) in the sediments of all lakes
around the world. These markers include cesium-137 (a byproduct
of atmospheric nuclear testing). Atmospheric testing by the
U.S.S.R. peaked in 1963. It then dramatically declined after the
implementation of the Nuclear Test Ban Treaty that same year.
In southern Wisconsin another marker that is
often used to confirm sediment dates is arsenic (yes, arsenic).
Sodium arsenite was used during the 1950s-60s in a number of
Wisconsin lakes to control aquatic plants. Records are available
that document how much was applied (Lake Tides Vol. 31,
No. 2, 2006). The peak in arsenic concentration in the core
corresponds with the time of maximum application.
Another dating marker that can be traced in lake
sediments is stable lead. It was used in leaded gasoline until
its removal in the mid-1970s and provides another time marker to
check on the lead-210 dating technique.
A Record in Glass
Fossils are one of the guides to the past life of a lake. The
fossils used most are diatoms. These are a special type of algae
that possess cell walls made of silica. Silica is the same as
glass so diatoms can be preserved for thousands of years in the
sediments. Diatoms are particularly useful because most of them
live under well-known environmental conditions. This makes them
ideal to characterize what past environmental conditions were
like when they were living, such as phosphorus concentrations.
Diatoms have been used to estimate trends in phosphorus,
acidification, color, salinity and plant communities. Studies
have allowed us to determine that some lakes are naturally
acidic while others have become acidic as a result of human
activities. Other algal groups such as certain blue-green and
green algae are also preserved in the sediments.
Other fossils that are deposited and are useful
for re-creating past environments are aquatic insect larvae and
zooplankton. Insect larvae can be used to track changes in a
lake’s oxygen content over time. Zooplankton are often eaten by
fish and invertebrates, so changes in their numbers allow us to
infer past fish populations. For example, a decline in large
zooplankton is an indication of an increase in plankton-eating
fish such as perch or bluegills.
Paleolimnology is a
powerful tool to discover where a lake has been and maybe
predict where it is going. This buried treasure of information
is stored in lake sediments and we can read the sedimentary
records like the pages of an ancient book. Look for more
information on paleolimnology in future
Lake Tides.
by Paul Garrison, Wisconsin Department of
Natural Resources
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Lake District Q&A
We often get phone calls and
emails from Lake Tides readers
with a variety of questions about lake districts. Do you have a
question about lake districts that you would like to see answered
in Lake Tides? Send it to
uwexlakes@uwsp.edu so we can include it in a future issue.
Q: What are the requirements for annual meeting
notices?
A: The written notice
for an annual meeting must be mailed out at least 14 days in
advance to all lake district property owners whose names are
listed in the tax roll. Written notice must also be mailed out
to all electors (resident voters) whose addresses are known (or
can be reasonably determined) or the lake district may publish
notice of the meeting in two successive issues of the local
newspaper.* The lake district is also required to mail notice of
the annual meeting to the Wisconsin Department of Natural
Resources (Lakes Management Section, 101 S. Webster Street, PO
Box 7921, Madison, WI 53707-7921). Wis. Stat. �� 33.30(2)(a)
To comply with Wisconsin’s open meetings law
requirements, a lake district should also:
-
post the meeting notice at least 24 hours in
advance in three locations likely to be seen by the general
public. As an alternative, a lake district may give notice
by paid publication in the local newspaper (this covers #2).
-
provide the local newspaper with a meeting
notice.
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give a meeting notice to any additional
media source that has requested to be notified.
For more information on Wisconsin open meetings
law requirements, see the Attorney General’s Open Meetings Law
Compliance Guide found at www.doj.state.wi.us.
For more information on lake districts, see
People of the Lakes: A Guide for Wisconsin Lake Organizations,
www.uwsp.edu/cnr/uwexlakes/districts.
*Tax rolls are available to help lake districts
generate accurate mailing lists for property owners. Mailing
lists for electors (resident voters) are not always readily
available, therefore, lake districts have the option of
publishing the notice to get the word out to electors.
back to top
EPA Launches National Lake Survey
Our nation’s lakes will be undergoing a check-up
in 2007 as the Environmental Protection Agency (EPA) initiates a
statistical survey. The goal of the survey is to discover what
percentages of the nation’s lakes are in good, fair or poor
condition. A "stress test" will also be performed to examine the
relative importance of nutrients, non-native species, lakeshore
development, pathogens and other stressors on lake conditions.
The EPA’s approach is multi-faceted, and
designed to strengthen state, tribal and interstate monitoring
programs. This will encourage more efficient use of resources,
expanded accessibility and better use of data, and partnerships
among agencies and others. The survey should also set a sound
baseline of data by providing documented information on the
extent of water quality problems and key stressors on our
nation’s lakes.
A total of 909 lakes, representing five size
classes and distributed relatively evenly across the lower 48
states, are included in the survey. The lakes were selected
randomly (excluding the Great Lakes) from a sample that includes
freshwater lakes (natural and man-made) and ponds and reservoirs
that are at least one meter deep (3.28 feet) and over 10 acres
(4 hectares). A second set of samples will be conducted from 91
of the lakes. These lakes are a subset of lakes from the EPA’s
National Eutrophication Survey (NES) that was conducted in 1972.
Surveying these 91 lakes will allow other potential trends in
water quality to be examined.
Wisconsin has 29 lakes included in the survey,
ranging in size from 11-acre (4.6 hectares) Buckskin Lake in
Florence County to 133,404-acre (53,989 hectares) Lake
Winnebago. Two of the lakes, Blueberry Lake in Sawyer County and
Haskell Lake in Vilas County, are located within tribal
jurisdictions. Several of the lakes already have ongoing
monitoring through citizen monitoring or other efforts, and that
information will be used to supplement the national lakes survey
data and provide background data for interpretation.
The EPA is providing funding and in-kind
services to support the field and laboratory work needed to
complete the survey. A team of Wisconsin Department of Natural
Resources (WDNR) and U.S. Geological Survey staff will be
sampling the selected lakes during a mid-summer sampling window.
Samples to be collected include standard water quality
constituents (nutrients, pH, color, chlorophyll a, etc.), water
clarity, physical profiles, phytoplankton and zooplankton, a
sediment core, algal toxins, pathogens, and benthos (lake-bottom
organisms). In addition, a comprehensive shoreline assessment
will be performed at 10 sites around each lake. These core
indicators will be examined to diagnose the lake’s water
quality, ecological integrity, and recreational value.
The WDNR staff has been actively involved in
refining the sampling design, selecting metrics, reviewing field
and laboratory protocols, conducting site reconnaissance, and
communicating with other states on plans for the survey. The
WDNR is planning to use the national lake survey effort to
complement and enhance its own lake monitoring and assessment
efforts in Wisconsin. For example, WDNR may add more lakes to
better report on lake conditions representative of the full
range of Wisconsin lake types. The WDNR may also collect
additional data, such as detailed aquatic plant information or
enhanced littoral and shoreland habitat parameters.
Results of the national survey of lakes will be
analyzed and compiled during 2008, with a final report issued in
2009. For more information on the survey of the nation’s lakes,
visit
www.epa.gov/owow/lakes/lakessurvey.
by Tim Asplund and Marilyn Larsen, Wisconsin
Department of Natural Resources
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Calendar
February 21, 2007 –
Conservation Lobby Day. Talk with your state Assembly
Representative and your state Senator about why lake stewardship
is important to you. For more information:
www.conservationvoters.org/Public/index.php
February 24, 2007 –
Regional conference "From Plan into Practice: Solutions for our
Changing Lakes." Richard T. Anderson Education Center,
Waukesha County Technical College, Pewaukee. For more
information:
www.wisconsinlakes.org/Events/07planintopractice.htm
Mar 1-2, 2007 –
American Water Resources Association (AWRA) 2007 Meeting,
Wisconsin Dells. "The Future of Wisconsin’s Water Resources:
Science and Policy."
For more information:
www.awra.org/state/wisconsin
March 3-5, 2007 –
Midwest Aquatic Plant Management Society Annual Conference.
Wyndham Hotel in Downtown Milwaukee.
For more information:
www.mapms.org/MAPMSConf2007.html
March 26, 2007 –
Early bird deadline for the 2007 Wisconsin Lakes Convention.
For more information:
www.uwsp.edu/cnr/uwexlakes/conventions
Apr 21-22, 2007 –
Lake Home and Cabin Show, Milwaukee. For more information:
www.lakehomeandcabinshow.com/wisc
May 1, 2007 –
Grants Deadlines.
Lake Protection and Lake Classification Grants
www.dnr.state.wi.us/org/water/fhp/lakes/lakeprot.htm
River Protection Planning Grants
www.dnr.state.wi.us/org/caer/cfa/Grants/Rivers/riverplanning.html
River Protection Management Grants
www.dnr.state.wi.us/org/caer/cfa/Grants/Rivers/riverprotection.html
back to top
Reflections
If we had no winter, the spring would not be so
pleasant; if we did not sometimes taste of adversity, prosperity
would not be so welcome.
- Anne Bradstreet, Meditations Divine and
Moral, 1655, American poet (1612 - 1672)
back to top
Editor: Mary Pardee
Design Editor: Amy Kowalski
Contributing Editors: Robert Korth and
Tiffany Lyden, UWEX; Carroll Schaal, DNR
Photos by: Robert Korth
(unless
otherwise noted)
Illustrations by: Carol Watkins, Chris Whalen
The contents of Lake Tides
do not necessarily reflect the views and policies of UW-Extension,
UWSP-CNR, the Wisconsin DNR or the Wisconsin Association of Lakes.
Mention of trade names, commercial products, private businesses or
publicly financed programs does not constitute endorsement.
Lake Tides welcomes articles, letters or other news items for
publication. Articles in Lake Tides may be reprinted or
reproduced for further distribution with acknowledgment to the
Wisconsin Lakes Partnership. If you need this material in an
alternative format, please contact our office. No state tax
revenue supported the printing of this document.
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