scholarly journals FAYETTEVILLE GREEN LAKE, NEW YORK. II. PRECIPITATION AND SEDIMENTATION OF CALCITE IN A MEROMICTIC LAKE WITH LAMINATED SEDIMENTS1

1969 ◽  
Vol 14 (6) ◽  
pp. 830-847 ◽  
Author(s):  
G. J. Brunskill
Keyword(s):  
New York ◽  
Meromictic Lake ◽  
Green Lake

MAPPING MICROBIAL COMMUNITY COMPOSITION AND GEOCHEMICAL GRADIENTS AT HIGH SPATIAL RESOLUTION IN A MEROMICTIC LAKE (GREEN LAKE, FAYETTEVILLE, NEW YORK)

2017 ◽  
Author(s):  
Jonah Boucher ◽  
◽  
Jeff Havig ◽  
Trinity L. Hamilton ◽  
Dionysios A. Antonopoulos ◽  
...  
Keyword(s):  
New York ◽  
Microbial Community ◽  
Community Composition ◽  
Spatial Resolution ◽  
High Spatial Resolution ◽  
Microbial Community Composition ◽  
Meromictic Lake ◽  
Green Lake

Chapter 8.7 Freshwater Stromatolitic Bioherms in Green Lake, New York

1976 ◽  
pp. 479-488 ◽  
Author(s):  
Jane R. Eggleston ◽  
Walter E. Dean
Keyword(s):  
New York ◽  
Green Lake

scholarly journals FAYETTEVILLE GREEN LAKE, NEW YORK. IV. INTERSTITIAL WATER CHEMISTRY OF THE SEDIMENTS1

1969 ◽  
Vol 14 (6) ◽  
pp. 858-861 ◽  
Author(s):  
Gregg J. Brunskill ◽  
Robert C. Harriss
Keyword(s):  
New York ◽  
Water Chemistry ◽  
Interstitial Water ◽  
Green Lake

Post-Younger Dryas climate interval linked to circumpolar vortex variability: isotopic evidence from Fayetteville Green Lake, New York

2002 ◽  
Vol 19 (3-4) ◽  
pp. 321-330 ◽  
Author(s):  
Kirby M. ◽  
Patterson W. ◽  
Mullins H. ◽  
Burnett A.
Keyword(s):  
New York ◽  
Younger Dryas ◽  
Isotopic Evidence ◽  
Circumpolar Vortex ◽  
Green Lake

The variation of annual 210Pb flux to varved sediments of Fayetteville Green Lake, New York from 1885 to 1965

1988 ◽  
Vol 23 (2) ◽  
pp. 848-854
Author(s):  
Gregg J. Brunskill ◽  
Stuart D. Ludlam
Keyword(s):  
New York ◽  
Varved Sediments ◽  
Green Lake

The behavior of biologically important trace elements across the oxic/euxinic transition of meromictic Fayetteville Green Lake, New York, USA

2015 ◽  
Vol 165 ◽  
pp. 389-406 ◽  
Author(s):  
Jeff R. Havig ◽  
Michael L. McCormick ◽  
Trinity L. Hamilton ◽  
Lee R. Kump
Keyword(s):  
New York ◽  
Trace Elements ◽  
Green Lake

scholarly journals A re-examination of the mechanism of whiting events: A new role for diatoms in Fayetteville Green Lake (New York, USA)

2021 ◽  
Author(s):  
Chloe Stanton ◽  
Julie Cosmidis ◽  
Lee Kump
Keyword(s):  
New York ◽  
Green Lake

Anoxic depositional overprinting of 238U/235U in calcite: When do carbonates tell black shale tales?

Geology ◽  
2021 ◽  
Author(s):  
Xinming Chen ◽  
Stephen J. Romaniello ◽  
Michael McCormick ◽  
Alyssa Sherry ◽  
Jeff R. Havig ◽  
...  
Keyword(s):  
New York ◽  
Water Column ◽  
Isotope Geochemistry ◽  
Sediment Traps ◽  
Depositional Environments ◽  
Uranium Isotopes ◽  
Carbonate Sediments ◽  
Anoxic Water ◽  
Green Lake ◽  
Bottom Waters

The fidelity of uranium isotopes (δ238U) in marine carbonates as a paleoredox proxy relies on whether carbonates can record and preserve seawater δ238U. Although modern carbonate sediments deposited under oxic conditions have been shown to track seawater δ238U, it remains unknown whether this is true for carbonates deposited under anoxic conditions. This is a crucial question because many ancient carbonates were likely deposited or reworked under anoxic bottom waters. To better understand the behavior of uranium isotopes under this scenario, we investigated U isotope geochemistry in the meromictic Fayetteville Green Lake (FGL; New York, USA), where primary calcite is precipitated from oxic surface waters, sinks past the chemocline, and is deposited under anoxic bottom waters. We observed significant depletions of dissolved U concentration (from 2.7 to 0.9 ppb) and δ238U (from –0.55‰ to –0.96‰) below the chemocline in FGL. Parallel with these depletions, δ238U of sediment traps increased progressively from –0.51‰ to –0.16‰, suggesting that U(VI) reduction was occurring in the anoxic water column. Carbonate sediments deposited under anoxic bottom waters were enriched in U by 6–18× compared to primary calcite. Our data suggest that such significant authigenic U enrichments resulted from U(VI) reduction in the anoxic water column and below the sediment-water interface. The δ238U value in the top 0.25 cm of sediments was –0.29‰ ± 0.10‰, overprinting original δ238U in primary calcite (–0.51‰ ± 0.02‰). Future applications of carbonate δ238U as a paleoredox proxy should consider depositional environments (oxic vs. anoxic) of carbonates.

Sedimentation rates in Fayetteville Green Lake, New York, U.S.A.

Sedimentology ◽  
1981 ◽  
Vol 28 (1) ◽  
pp. 85-96 ◽  
Author(s):  
STUART D. LUDLAM
Keyword(s):  
New York ◽  
Sedimentation Rates ◽  
Green Lake

scholarly journals Fayetteville, Green Lake, New York: 3 H-3 He water mass ages and secondary chemical structure1,2

1981 ◽  
Vol 26 (1) ◽  
pp. 110-122 ◽  
Author(s):  
T. Torgersen ◽  
D. E. Hammond ◽  
W. B. Clarke ◽  
T.-H. Peng
Keyword(s):  
New York ◽  
Water Mass ◽  
Green Lake ◽  
Secondary Chemical
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