Effects of diurnal vertical mixing and stratification on phytoplankton productivity in geothermal Lake Rotowhero, New Zealand

Brookes, Justin D., O'Brien, Katherine R., Burford, Michele A., Bruesewitz, Denise A., Hodges, Ben R., McBride, Chris and Hamilton, David P. (2013) Effects of diurnal vertical mixing and stratification on phytoplankton productivity in geothermal Lake Rotowhero, New Zealand. Inland Waters, 3 3: 369-376. doi:10.5268/IW-3.3.625

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Author Brookes, Justin D.
O'Brien, Katherine R.
Burford, Michele A.
Bruesewitz, Denise A.
Hodges, Ben R.
McBride, Chris
Hamilton, David P.
Title Effects of diurnal vertical mixing and stratification on phytoplankton productivity in geothermal Lake Rotowhero, New Zealand
Journal name Inland Waters
ISSN 2044-2041
2044-205X
Publication date 2013
Sub-type Article (original research)
DOI 10.5268/IW-3.3.625
Volume 3
Issue 3
Start page 369
End page 376
Total pages 8
Place of publication Ambleside, Cumbria United Kingdom
Publisher Freshwater Biological Association
Collection year 2014
Language eng
Formatted abstract
Mixing processes in lakes are key factors controlling light availability for phytoplankton growth, but understanding the contribution of mixing is often confounded by other factors such as nutrient availability and species dynamics. Our study examined this problem in a low pH, geothermally heated lake dominated by one phytoplankton genus and lacking the complexity of nutrient limitation, phytoplankton species interactions, or grazing pressure. We hypothesized that the continuous strong convectively driven circulation resulting from atmospheric instability and sediment heating would negate any tendency of thermal stratification, entraining phytoplankton and transporting them away from high surface irradiance that could induce photoinhibition. During our study, water temperatures were considerably warmer than air temperatures, with a diurnal maximum surface temperature of 37.5 °C and minimum of 35.5 °C. Surface heating induced stratification, with a temperature difference of 1–2 °C evident during the day, but there was sufficient heat loss and mixing during the night to erode the stratification and create isothermal conditions. The vertical entrainment velocity driven by convective circulation was on the order of 0.1 mm s−1, but when there was strong solar heating, phytoplankton within the top 0.5 m of the water column still showed depressed photosynthetic quantum efficiencies, as determined with a Pulse Amplitude Modulated fluorometer (PHYTOPAM); however, this depression was less than for phytoplankton cells maintained throughout the day in surface waters with bottle incubations. At other times mixing generated by continuous heating and atmospheric instability meant that phytoplankton did not show photoinhibition; therefore, despite the geothermally driven mixing in Rotowhero, the intensity of solar radiation is still the key mechanism determining the stratification response and resultant photoinhibition of the phytoplankton.

Lake Rotowhero provides an excellent natural laboratory to examine the relative time scales of mixing and phytoplankton photoinhibition responses because small changes in solar radiation have such marked impacts on the diurnal stratification and radiation experienced by cells located above the diurnal thermocline.
Keyword Entrainment
Geothermal
Photoinhibition
Pulse amplitude modulated fluorometry
Chlorophyll-a fluorescence
Thermal lake
Temperature
Limnology
Rotoiti
Photosynthesis
Reservoir
Shallow
Q-Index Code C1
Q-Index Status Confirmed Code
Institutional Status UQ

Document type: Journal Article
Sub-type: Article (original research)
Collections: School of Civil Engineering Publications
Official 2014 Collection
 
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