2000
DOI: 10.1139/f00-060
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Erratum: An investigation into iron-stimulated phytoplankton productivity in epipelagic Lake Erie during thermal stratification using trace metal clean techniques

Abstract: Fig. 3. Periodogram of wave heights obtained at hourly intervals from Weather Buoy 45142 (42.7°N, 79.3°W) over the 30-day (n = 720) precruise period in 1996, 1997, and 1998. The inset shows the differential heat gain determined from thermal profiles at Station 23 over the same period (1 cal = 4.1868 J).

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Cited by 7 publications
(6 citation statements)
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“…[30][31][32][33] Since the introduction of clean techniques data for lakes are still limited, [34] recent studies highlighted that Fe concentrations are much lower than previously perceived. [20,35] For the lakes studied (Laurentian Great Lakes, Lake Geneva and Lake Kinneret) dFe is reported to be present in concentrations ranging from 0.5 to 312 nM (Table 1). [20,[35][36][37][38][39] The vertical and spatial distributions of dFe have similar patterns in large lakes and in the ocean.…”
Section: Iron Distribution In Aquatic Systemsmentioning
confidence: 99%
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“…[30][31][32][33] Since the introduction of clean techniques data for lakes are still limited, [34] recent studies highlighted that Fe concentrations are much lower than previously perceived. [20,35] For the lakes studied (Laurentian Great Lakes, Lake Geneva and Lake Kinneret) dFe is reported to be present in concentrations ranging from 0.5 to 312 nM (Table 1). [20,[35][36][37][38][39] The vertical and spatial distributions of dFe have similar patterns in large lakes and in the ocean.…”
Section: Iron Distribution In Aquatic Systemsmentioning
confidence: 99%
“…A spatial gradient of dFe in the epilimnion of lakes has been observed, from nearshore (dFe mean: 31.7 nM) to isolated areas (dFe mean: 1.5 nM), showing a strong increase of dFe concentration along the coastline as a result of lake-edge sources. [20,35,41] Elevated Fe concentrations are indeed generally found in near-shore waters, [64] often in the range of 100-1000 times higher than that found in the open ocean. [6] Despite a relatively high concentration of Fe in rivers, [64] very little riverine Fe reaches the open ocean as most of it is removed by precipitation, coagulation, and sedimentary processes favoured by the increase of salinity in estuaries.…”
Section: The Importance Of Iron In Aquatic Systemsmentioning
confidence: 99%
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