scholarly journals Aliphatic hydrocarbons in sediment cores from the southern basin of Lake Michigan

1991 ◽  
Author(s):  
P.V. Doskey ◽  
A.W. Andren
1988 ◽  
Vol 45 (6) ◽  
pp. 1030-1035 ◽  
Author(s):  
Daniel J. Conley ◽  
Michael A. Quigley ◽  
Claire L. Schelske

Estimated lake-wide sediment fluxes of silica and phosphorus (P) were determined and then compared with other components in the biogeochemical cycle to investigate the importance of sediment regeneration in Lake Michigan. Dissolved silica (Si) and soluble reactive phosphorus (SRP) fluxes from sediments were measured by the incubation of intact sediment cores. Estimated Si flux from sediments can supply 21% of the total mass of silica in the water annually and 26% of the Si used during annual diatom production. By contrast, estimated SRP flux from lake sediments can supply only 4.1% of the mass of total P in the water annually and <1% of the P utilized for annual primary production. Because the internal regeneration of P occurs rapidly in the water column, compared with the much slower regeneration of Si (0.8∙yr−1), P can be used many times during an annual cycle whereas Si is used only once. Thus, differences in the supply rates and in the biogeochemical recycling rates of Si and P can lead to seasonal Si depletion in the water mass and influence the outcome of seasonal phytoplankton species succession by limiting Si availability necessary for diatom production.


2020 ◽  
Vol 57 (2) ◽  
pp. 292-305
Author(s):  
Catherine H. Yansa ◽  
Albert E. Fulton ◽  
Randall J. Schaetzl ◽  
Jennifer M. Kettle ◽  
Alan F. Arbogast

We report on pollen, plant macrofossils, and associated lithostratigraphy of a sediment core extracted from the base of Silver Lake, a kettle lake in northern Lower Michigan, USA, which reveal a complex deglacial scenario for ice block melting and lake formation, and subsequent plant colonization. Complementary multivariate statistical and squared chord distance analyses of the pollen data support these interpretations. The basal radiocarbon age from the core (17 540 cal years BP) is rejected as being anomalously old, based on biostratigraphic anomalies in the core and the date’s incongruity with respect to the accepted regional deglaciation chronology. We reason that this erroneous age estimate resulted from the redeposition of middle-Wisconsin-age fossils by the ice sheet, mixed with the remains of plants that existed as the kettle lake formed at ca. 10 940 cal years BP by ice block ablation. Thereafter, the kettle lake became a reliable repository of Holocene-age fossils, documenting a mature boreal forest that existed until 10 640 cal years BP, followed by a pine-dominated mixed forest, an early variant of the mixed conifer–hardwood forest that persists to the present day. Our study demonstrates that researchers investigating kettle lakes, a common depositional archive for plant fossils in deglaciated landscapes, should exercise caution in interpreting the basal (Late Pleistocene/early Holocene-age) part of lake sediment cores.


1991 ◽  
Vol 17 (1) ◽  
pp. 94-108 ◽  
Author(s):  
Mark H. Hermanson ◽  
Erik R. Christensen ◽  
Dale J. Buser ◽  
Li-Mei Chen

2006 ◽  
Vol 63 (4) ◽  
pp. 872-890 ◽  
Author(s):  
Thomas F Nalepa ◽  
David L Fanslow ◽  
Andrew J Foley III ◽  
Gregory A Lang ◽  
Brian J Eadie ◽  
...  

Benthic surveys were conducted in the southern basin of Lake Michigan and throughout the lake to assess trends in benthic populations, emphasizing recent changes in densities of the benthic amphipod Diporeia spp. and dreissenid mussels. In the southern basin, Diporeia populations declined 89%, 91%, and 45% between 1993 and 2002 at sites <30, 31–50, and 51–90 m, respectively. Lakewide, the population declined 65% between 1994–1995 and 2000. Over the same time period, dreissenid densities, particularly Dreissena bugensis, increased. Intensive studies at 45 m sites in the southeastern region examined changes in lipid content, age structure, and benthic food inputs relative to the hypothesis that food limitation was a factor in Diporeia's disappearance. As Diporeia densities declined to zero, length–weight remained unchanged, and lipid content generally increased. Recruitment still occurred, but the young did not survive to become adults. Based on organic carbon, biogenic silica, and chlorophyll collected in sediment traps and found in the upper sediments, pelagic inputs to the benthic region still occurred. Our field observations and laboratory experiments did not disprove the hypothesis that food limitation from dreissenid filtering activities was the cause of the decline, but direct relationships between the loss of Diporeia and indicators of food availability were difficult to establish.


1981 ◽  
Vol 15 (1) ◽  
Author(s):  
J. Muhlbaier ◽  
G.T. Tisue
Keyword(s):  

1984 ◽  
Vol 10 (3) ◽  
pp. 307-321 ◽  
Author(s):  
Brian J. Eadie ◽  
Richard L. Chambers ◽  
Wayne S. Gardner ◽  
Gerald L. Bell

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