Last November at Faville Grove Sanctuary we filled in a series of drainage ditches stretching three-quarters of a mile in the Ledge Lowlands along Prairie Lane. With nowhere to go, groundwater and precipitation began to collect, pooling up and re-saturating the peaty soil of the former wetland. Within only a few days, a tiny bubbling spring began to emerge from the earth, sending a trickle of water into the seeded bare soil. Weeks later, all laid dormant under a blanket of deep white snow with the exception of the tiny spring as the ground continued to release a gentle rivulet of earth-warmed water. For most of the winter, the spring remained visible as the seeping waters exposed the naked black soil against the white backdrop of the landscape.
Now, the snow has soaked into the earth while spring rains and the steady influx of groundwater puddle in our recovering wetland, where last year and for decades prior, water was quickly shunted off to a series of ditches and dumped into the Crawfish River. Just in time to take advantage of the brimming wetlands and waterlogged fields, the Wilson’s snipe has arrived in small flocks from their wintering grounds to descend upon the newly created wetland, where they probe the peaty soil for small invertebrates. By April, the haunting winnow of the snipe, produced not by song but by the open fan of the tail feathers, can be heard in the twilight hours as the first arriving males spar for prime mating territory throughout the floodplain.
Naturalists will often track the progression of natural phenomena as spring events unfold: the date of first open water on a local lake, the arrival of bluebirds to freshly cleaned nest boxes, and the emergence of the first pasque flower through cold, rocky soils. For a cabin-bound naturalist, recording these events is valuable not only to boost the spirits after a long winter, but also holds scientific and practical significance. Nature is also a dutiful record keeper, with a library of notes that span to the end of the Pleistocene, when life returned to colonize the raw landscape—a clean slate following the retreat of the last glaciers. In less disturbed locations, if you follow the bill of the snipe deep into the peat you may find layer upon microscopic layer of pollen deposits, preserved in an oxygen-free environment. Under careful examination, scientists can identify the type of pollen in the various layers and begin to understand changes in the local vegetation since the end of the last ice age. In southern Wisconsin, the deepest, and therefore oldest, layers of pollen are largely from spruce and fir when the climate was still cool and conducive to the growth of conifers. As you rise higher in the peat to more recent deposits, pollen composition shifts to oaks and hardwoods, indicating a major vegetation change in response to the powerful forces of a warming climate.
While walking under a canopy of oaks on a cool April morning it’s easy to appreciate these stately giants with their flowers (called catkins) dangling in the breeze, budding twigs beginning to shield the last clear view of their massive outstretched arms, perhaps the very same limbs that supported roosting flocks of passenger pigeons, fattened on abundant acorns, over a century ago. The oak can live to be well over 300 years old, and during that time it leaves it’s signature in every patch of peaty soil when rains of pollen are carried by spring winds and deposited in the archives of our landscape.
Oaks leave their mark on us as well. Memories of this magnificent tree have warmed our hearts and bodies for generations. Despite our fondness for this signature tree of the southern Wisconsin landscape, the future of oak ecosystems throughout the state remains uncertain. With the cessation of cleansing fire and the encroachment of exotic brush, dense shade prevents the next generation of oak seedlings from taking root. Look for young oaks in any local woodlot and the you might find only a few gaunt individuals on the edge of the woods, desperately reaching for light, with few remaining leaves and lower branches already lost to the shade. The outstretched limbs on the lower branches of mature oaks face a similar fate as they are overtaken by invading, shade-tolerant trees. The future of the oak in southern Wisconsin, like so many other features of our natural landscape, depends on our active management. Thinning trees and brush (including some native species) and reintroducing the healing quality of prescribed fire will go a long way to insure that the oak remains the flagship tree of southern Wisconsin. When the last pre-European settlement trees have fallen to the earth, the record of our stewardship will remain for the scientist and the snipe.
in a series of drainage ditches stretching three-quarters
of a mile in the Ledge Lowlands along Prairie Lane.
With nowhere to go, groundwater and precipitation
began to collect, pooling up and re-saturating the
peaty soil of the former wetland. Within only a few
days, a tiny bubbling spring began to emerge from the
earth, sending a trickle of water into the seeded bare
soil. Weeks later, all laid dormant under a blanket of
deep white snow with the exception of the tiny spring
as the ground continued to release a gentle rivulet of
earth-warmed water. For most of the winter, the spring
remained visible as the seeping waters exposed the naked
black soil against the white
backdrop of the landscape.
Now the snow has soaked
into the earth and spring rains
and a steady influx of groundwater
puddle in our recovering
wetland, where last year
and for decades prior, water
was quickly shunted off to a
series of drainage ditches and
dumped into the Crawfish
River. Taking advantage of the
waterlogged fields, the Wilson’s
snipe has arrived in small
flocks from their wintering
grounds and descended upon
the newly created wetland,
where they probe the peaty
soil for small invertebrates.
By April, the haunting winnow of the snipe, produced
not by song but by the open fan of the tail feathers,
could be heard in the twilight hours as the first arriving
males spar for prime mating territory throughout the
floodplain.
Naturalists will often track the progression of natural
phenomenon as spring events unfold: the date of
first open water on a local lake, the arrival of bluebirds
to freshly cleaned nest boxes, and the emergence of
the first pasque flower through warming, rocky soils.
For a winter-weary naturalist, recording these events
is valuable not only to boost the spirits, but also holds
scientific and practical significance. Nature is also a
dutiful record keeper, with a library of notes that span
to the end of the Pleistocene, when life returned to
colonize the raw landscape—a clean slate following






