Cited by 69Aquatic Ecosystems and Phytoplankton DynamicsWater Quality and Resources StudiesWater Quality and Pollution Assessment

Paleolimnology of Onondaga Lake: the History of Anthropogenic Impacts on Water Quality

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Rowell, H. Chandler·1996·Lake and Reservoir Management

Abstract

New York State's Onondaga Lake is a polluted, hypereutrophic, saline lake with a remarkable paleolimnological record. The chemical and diatom stratigraphy of two sediment cores was used to document past anthropogenic impacts on the lake's water quality. Onondaga Lake's pre-historic and pre-industrial water quality conditions are clarified and subsequent major pollution events identified. Pre-1800s Onondaga Lake was mesotrophic and considerably less saline (around 230 mgL−1 Cl−) than at present (around 450 mgL−1 Cl−). Factors that most affected lake water quality were: 1) increasing settlement in the watershed which increased lake sedimentation and nutrient levels, 2) development of the salt industry during the 1800s which contributed to a rise in lake salinity, 3) the soda-ash industry in die late 1800s through 1900s which added major amounts of CaCO3 and salt to the lake, and 4) post-World War II urban and industrial development which contributed to very high nutrient, Hg, and other heavy metal loadings.

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  • Historically a mesotrophic system, high nutrient concentrations (total phosphorus concentrations >100 ug/L) due to wastewater discharge and nonpoint-source loadings led to frequent algal blooms, high turbidity, and hypolimnetic anoxia, resulting in Onondaga Lake being classified as hypereutrophic.

    “Historically a mesotrophic system (Rowell 1996), high nutrient concentrations (total phosphorus [TP] concentrations in the lake >100 ug/L) due to wastewater discharge and nonpoint-source loadings led to frequent algal blooms, high turbidity, and hypolimnetic anoxia, resulting in the lake being classified as hypereutrophic (Effler 1996).”
  • Onondaga Lake was oligo-mesotrophic prior to European settlement in the late 1700s.

    “Diatom stratigraphy indicates that Onondaga Lake was oligo-mesotrophic prior to European settlement in the late 1700s (Rowell 1996).”

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Cites

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Research works printed but not linked: 26

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Authors
Rowell, H. C.
Affiliations
New York State Department of Environmental Conservation (US)
Corresponding author
Rowell, H. Chandler
Venue
Lake and Reservoir Management
Published
1996-03
Volume
12
Issue
1
Pages
35-45
ISSN
  • 0743-8141 (ISSN-L)
  • 1040-2381
  • 2151-5530
OpenAlex
W2136299400
Cited by
69
References
2
Citations by year
2024: 2 · 2021: 1 · 2020: 1 · 2018: 1 · 2017: 1 · 2016: 1 · 2015: 7 · 2014: 2 · 2013: 2 · 2012: 7
FWCI
3.73
Type
journal article
Language
en
Open access
Locations
Lake and Reservoir Management (publishedVersion)
Topics
  • Physical Sciences › Environmental Science › Environmental Chemistry › Aquatic Ecosystems and Phytoplankton Dynamics
  • Physical Sciences › Environmental Science › Water Science and Technology › Water Quality and Resources Studies
  • Physical Sciences › Environmental Science › Water Science and Technology › Water Quality and Pollution Assessment
Keywords
Onondaga Lake, paleolimnology, anthropogenic impacts, lake salinity, hypereutrophic lakes, diatom biostratigraphy, sediment core, salt industry, soda ash industry, nutrient loading, heavy metals, mercury, lake sedimentation

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