Cited by 70Aquatic Ecosystems and Phytoplankton DynamicsMarine and coastal ecosystemsWater Quality and Resources Studies

Long‐term changes in the areal hypolimnetic oxygen deficit (AHOD) of Onondaga Lake: Evidence of sediment feedback

Matthews, David A., Effler, Steven W.·2006·Limnology and Oceanography

Abstract

Long‐term trends in the rate of depletion of hypolimnetic dissolved oxygen (DO) are documented for ionically enriched hypereutrophic Onondaga Lake, New York, for the 1978–2002 interval. Depletion rates, represented as areal hypolimnetic oxygen deficits (AHOD, g m−2 d−1), are calculated on the basis of weekly DO profiles of 1‐m resolution and estimates of coincident inputs of DO from overlying layers driven by vertical mixing. Vertical mixing inputs of DO are important in this system, representing from 15% to 37% (mean 25%) of AHOD. Interannual variations in hypolimnetic temperatures have comparatively minor (±6%) effects on AHOD. AHOD decreased 49%, from an average of 2.12 g m−2 d−1 for the 1978–1986 interval, to an average of 1.08 g m−2 d−1 for the 1997–2002 interval. This decrease was driven by an abrupt decrease in the deposition of particulate organic carbon into the hypolimnion starting in 1987. The magnitude of the decrease in AHOD closes reasonably well with decreases in both primary production in the trophogenic zone and organic carbon deposition to the tropholytic zone. The time course of the decrease in AHOD is consistent with localization of oxygen‐demanding processes within the lake sediments, reflecting the progression of sediment diagenesis.

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Crossref · 10.4319/lo.2006.51.1_part_2.0702

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48 of 48 references verified0 citation errors · 0 not checkable

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  • Hypolimnetic anoxia eliminated the year-round availability of coldwater habitats in Onondaga Lake; however, dissolved oxygen conditions were sufficient to support seasonal use for coldwater species using the lake as part of their regional, annual home range.

    “Hypolimnetic anoxia eliminated the year-round availability of coldwater habitats; however, dissolved oxygen conditions were sufficient to support seasonal use for coldwater species using the lake as part of their regional, annual home range.”
  • Oxygen is depleted rapidly from the hypolimnion of Onondaga Lake after the onset of thermal stratification.

    “Oxygen is depleted rapidly from the hypolimnion after the onset of thermal stratification (Matthews and Effler 2006).”
  • In lakes with a long history of eutrophy (i.e., a large pool of unmineralized organics in the sediments), the time to reach a new steady-state hypolimnetic dissolved oxygen depletion rate may be on the order of years to decades.

    “In lakes with a long history of eutrophy (i.e., a large pool of unmineralized organics in the sediments), the time to reach a new steady-state, hypolimnetic DO depletion rate may be on the order of years to decades.”

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Authors
Matthews, D. A., & Effler, S. W.
Affiliations
Upstate Freshwater Institute (US)
Corresponding author
Matthews, David A.
Venue
Limnology and Oceanography
Publisher
Wiley
Published
2006-01
Volume
51
Issue
1part2
Pages
702-714
ISSN
  • 0024-3590 (ISSN-L)
  • 1939-5590
OpenAlex
W2106975190
Cited by
70
References
48
Citations by year
2026: 1 · 2025: 2 · 2024: 2 · 2023: 4 · 2021: 1 · 2020: 2 · 2019: 3 · 2018: 5 · 2017: 1 · 2016: 2 · 2015: 7 · 2014: 2 · 2013: 3 · 2012: 7
FWCI
4.38
Type
journal article
Language
en
Open access
closed
Locations
Limnology and Oceanography (publishedVersion)
Topics
  • Physical Sciences › Environmental Science › Environmental Chemistry › Aquatic Ecosystems and Phytoplankton Dynamics
  • Physical Sciences › Earth and Planetary Sciences › Oceanography › Marine and coastal ecosystems
  • Physical Sciences › Environmental Science › Water Science and Technology › Water Quality and Resources Studies
Keywords
Onondaga Lake, hypereutrophic lakes, sediment diagenesis, dissolved oxygen depletion, vertical mixing, primary production, long-term trends, lake sediments

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