Assessing the Influence of Environmental pH on Algal Physiology Using a Novel Culture System

Since the Industrial Revolution, surface ocean pH has declined due to the input of anthropogenically derived carbon dioxide, termed ocean acidification. Examinations of phytoplankton physiology in the face of changing pH are becoming more important as anthropogenically-driven pH decreases in the sur...

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Bibliographic Details
Main Author: Golda, Rachel
Other Authors: Oregon State University. Sea Grant College Program
Format: Doctoral or Postdoctoral Thesis
Language:English
unknown
Published: Oregon Health and Science University
Subjects:
Online Access:https://ir.library.oregonstate.edu/concern/defaults/ng451p78x
Description
Summary:Since the Industrial Revolution, surface ocean pH has declined due to the input of anthropogenically derived carbon dioxide, termed ocean acidification. Examinations of phytoplankton physiology in the face of changing pH are becoming more important as anthropogenically-driven pH decreases in the surface ocean progress (termed ocean acidification). Previous research has shown that phytoplankton response to acidification are highly variable, with some taxa showing improvement and some showing marked deterioration. The ability to maintain homeostasis of intracellular pH is an important adaptation for phytoplankton to continue to thrive under changing conditions; increased energy production has been shown to mitigate the negative effects of acidification. This dissertation examines the effect of steady state and changing pH environments on the internal pH, esterase activity, and photosynthetic efficiency (the latter two parameters are involved with energy production or utilization) of the marine phytoplankton species, Isochrysis galbana. To accomplish this, a novel pHstat system was developed for the culture of marine phytoplankton, capable of maintaining both steady state and dynamic pH environments autonomously over extended periods. The pHstat system was used to grow phytoplankton at three steady state pH levels (pH 7.5, 8.0, and 8.5), as well under two separate dynamic conditions. The dynamic conditions were differentiated by coupling or decoupling light cycles from their natural relationship with pH (i.e., pH increases during the day due to photosynthetic uptake of inorganic carbon and decreases at night due to carbon addition through cellular respiration) in an effort to determine if intracellular pH changes were driven by changes in external pH or by changes in internal pools of dissolved inorganic carbon (DIC) availability due to carbon fixation and cellular respiration. To determine intracellular pH using a rapid, reliable method, I explored the efficacy of the fluorescent intracellular pH indicator for ...