Elsevier

Ecological Modelling

Volume 134, Issue 1, 30 September 2000, Pages 59-72
Ecological Modelling

A dinoflagellate adaptive behavior model: response to internal biochemical cues

https://doi.org/10.1016/S0304-3800(00)00336-7Get rights and content

Abstract

In this study we built two models to simulate vertical movements of an individual dinoflagellate. In the models, we laid out the flows of the chemical substances inside the cell and their changes in response to such environmental changes as nitrate concentration and light intensity. One of the models is called the Clock-Driven Model, in which the cell moves only according to the clock time and exhibits a regular vertical diel movement. The other model, which we call the Decision-Making Model, contains a network to make decisions for the next move, based on the interactions among biochemicals inside the phytoplankter and its environment. In this model, the decision emerges from the results of a cell's internal biochemical fluxes controlled by the threshold setting. The simulation results of both models with different nutrient conditions were compared in terms of the cell's behavioral patterns and the amount of protein produced by the cell. The results indicated that balances among the biochemicals and their fluxes can play a significant role in the directional decisions made by dinoflagellates under some environmental nitrate conditions, and that irregularity in a cell's movements may be affected by nitrate availability. Also, the simulation results suggest that irregular migration produced to meet the predefined criteria for biochemical fluxes inside the cell can benefit the cell in terms of protein accumulation. We propose that the essence of a cell's adaptivity to the environment resides in the internal cellular condition represented here by threshold values associated with biochemical fluxes and their balances, and that it is important to consider an organism's internal condition when constructing an adaptive behavior model.

Introduction

Observational studies on single-cell phytoplankton demonstrate adaptive behaviors according to changes in the physical environment (Kamykowski, 1981a, Cullen and Horrigan, 1981, MacIntyre et al., 1997). Many phytoplankton are not mere passive particles carried by the turbulence or currents in the ocean, but move autonomously from the surface to the deeper section of the ocean to accommodate themselves to various environmental conditions (Jennings, 1976). Although phytoplankton do not have neurons, they function as though they have sense organs for light and gravity (Levandowsky and Kaneta, 1987). Their adaptivity, however, may come not only from a sensitivity to external cues but also from mechanical or perceived changes in their internal state by mechanisms that are poorly defined at present (Jones, 1993, Kamykowski, 1995). Since marine phytoplankton live by depending on photosynthesis and the nutrients in the ocean, their decision to swim up or sink/swim down should be associated with the relation between plankton’s internal condition and the outside physical state.

In this study we have focused on the behavior of planktonic algae called dinoflagellates, which typically are single-cell organisms that autonomously migrate in the ocean. They gain energy and carbon/hydrogen/oxygen through photosynthesis and absorb other necessary nutrients from the surrounding seawater. We built models for an individual dinoflagellate’s vertical swimming behavior and formulated these models to identify the key elements in its adaptation to the environment. Most individual-based models for plankton describe relationships between changes in the external environment and an organisms' behavior, but not the organism's internal state (Murdoch, 1992). We, however, here considered the fluxes and changes of its internal biochemicals which are influenced by changes in the external environment. To construct models, we translated the external environmental changes into a plankter’s internal changes, viewing its behavior as an emergent result of interacting processes inside the organism.

Section snippets

Dinoflagellates and their environment

Dinoflagellates can migrate between the ocean surface and deeper water of more than 12 m, using their flagella. Many dinoflagellate species obtain energy and carbon/hydrogen/oxygen from photosynthesis and absorb other necessary nutrients like nitrogen from the seawater (Levandowsky and Kaneta, 1987). These elements are eventually combined to produce organic material including significant amounts of protein for cell growth. Many observations have noted that dinoflagellates migrate with a 24 h

Model description

Two models were constructed to examine if it is advantageous for a cell to determine its movement according to its biochemical fluxes. The first model, which we call Clock-Driven Model, represents the idea that the internal clock of the cell related to the diel light cycle governs its vertical movements. The other model, which we call Decision-Making Model, was developed based on our assumption that the cell is monitoring its internal biochemical changes to determine its next move. In both

Simulation representation, external conditions and results

We have implemented the models to simulate different external conditions, and made graphs to represent the simulation results. The vertical movement of the dinoflagellate cell is plotted along with the light intensity at the surface in a graphical window, while another window shows the amounts of internal nitrate, photosynthate and protein relative to their predefined maximum values. The value of accumulated protein is reset to half when the amount reaches its predefined maximum value, so that

Discussion

Although the control of dinoflagellate DVM is attributed mainly to the light intensity or to its internal clock, the simulation results suggested that the migration pattern also can profitably vary according to internal changes in photosynthate and nitrate. These results indicate that the periodicity of dinoflagellate diel movement may be regulated by its response to environmental cycles or to its internal clock but that its irregularity may be affected by nitrate availability. The migration

Acknowledgements

We would like to thank Dr Hiroyuki Matsuda at Ocean Research Institute of Tokyo University for his useful advice on the adaptive aspects of our models and Dr Hidekatsu Yamazaki at Tokyo University of Fisheries for providing advice in the development of our models. This work was supported by NSF OCE-9503253.

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