The Response of Banksia Roots to Change in Water Table Level in a Mediterranean-Type Environment
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Edith Cowan University Research Online Theses: Doctorates and Masters Theses 2011 The response of Banksia roots to change in water table level in a Mediterranean-type environment Caroline Canham Edith Cowan University Follow this and additional works at: https://ro.ecu.edu.au/theses Part of the Ecology and Evolutionary Biology Commons, and the Plant Sciences Commons Recommended Citation Canham, C. (2011). The response of Banksia roots to change in water table level in a Mediterranean-type environment. https://ro.ecu.edu.au/theses/389 This Thesis is posted at Research Online. https://ro.ecu.edu.au/theses/389 Edith Cowan University Copyright Warning You may print or download ONE copy of this document for the purpose of your own research or study. The University does not authorize you to copy, communicate or otherwise make available electronically to any other person any copyright material contained on this site. You are reminded of the following: Copyright owners are entitled to take legal action against persons who infringe their copyright. A reproduction of material that is protected by copyright may be a copyright infringement. Where the reproduction of such material is done without attribution of authorship, with false attribution of authorship or the authorship is treated in a derogatory manner, this may be a breach of the author’s moral rights contained in Part IX of the Copyright Act 1968 (Cth). Courts have the power to impose a wide range of civil and criminal sanctions for infringement of copyright, infringement of moral rights and other offences under the Copyright Act 1968 (Cth). Higher penalties may apply, and higher damages may be awarded, for offences and infringements involving the conversion of material into digital or electronic form. THE RESPONSE OF BANKSIA ROOTS TO CHANGE IN WATER TABLE LEVEL IN A MEDITERRANEAN-TYPE ENVIRONMENT Caroline Canham B. Sc. (Hons.) This thesis is presented in fulfilment of the requirements for the degree of Doctor of Philosophy Faculty of Computing, Health and Science Edith Cowan University May, 2011 USE OF THESIS The Use of Thesis statement is not included in this version of the thesis. Abstract For phreatophytic plants to persist in a given habitat they need to maintain a functional connection to the water table, and the capacity for roots to respond to changes in the water table is a key aspect of this. If root growth is limited by season, plants may not be able to grow roots to adjust to changes in the water table at a particular time of the year. The redistribution of roots, particularly the capacity for roots to follow the water table down in summer and autumn months, is vital for phreatophytic plants to maintain a functional connection with the water table. Root activity by phreatophytic Banksia in south-west Western Australia was assessed using root in-growth bags, with above- ground plant phenological processes observed simultaneously. The root in-growth bag technique that was used showed that Banksia roots are able to grow, provided soil conditions are conducive and there are no endogenous limitations to root growth at different times of the year, such as a dormancy period. The ability to grow at any time in response to soil conditions might be an essential prerequisite for phreatophytes if they are to survive fluctuating water table conditions in seasonally water-limited environments. Assuming that roots follow a seasonally dynamic watertable, a further study using chemical tracers assessed water uptake from the capillary fringe at contrasting times of the year. Lithium chloride was used in spring and 15N in autumn, to avoid contamination between the two sampling periods. There was some indication that the phreatophytic Banksia study species were utilising groundwater. This was evident from observation of tracer uptake from the capillary fringe during spring, when the water table was at its highest level. However, water uptake from the capillary fringe by Banksia was not evident during the autumn sampling period. This is likely to be due to methodological constraints, as plants did not demonstrate any signs of water stress despite the low water content in the vadose zone. These physiological indicators suggest that plants were still accessing groundwater at this time of the year. iii Quantifying the rate of root elongation for a particular species may give some indication of the rate of water table decline that they are able to survive. Root elongation rates and response to rapid water table decline were observed in rhizopods, allowing for the maintenance and manipulation of a water table under glasshouse conditions. The maximum rates of root elongation were found to be 36.7 mm day-1 and 18.2 mm day-1 for Banksia attenuata and Banksia littoralis respectively. These rates of root elongation may be regarded as rapid in comparison to the rates of water table decline that the species are likely to experience over summer and autumn water table decline. Such rapid rates of root elongation indicate that plants can potentially maintain contact with a water table decline at far greater rates than those that occur during a normal seasonal cycle of water table fluctuations. Based on the rates of root elongation by phreatophytic Banksia, it was expected that plants would maintain a functional connection with a rapidly decreasing water table. However, despite plant-available water being present in the soil profile, there was very limited root extension following rapid water table drawdown. In addition to little root elongation response, seedlings demonstrated a rapid drought response to water table decline, quickly reducing stomatal conductance, transpiration and photosynthesis. It is likely that the lack of root elongation response to a declining water table by the phreatophytic Banksia study species was due to plants being unable to meet their water requirements once the water table fell below the rooting depth of the plants. It was found that the response of phreatophytic Banksia to rapid water table decline depends on the availability of other water sources, and the rate of water table decline. iv Copyright and access declaration I certify that this thesis does not, to the best of my knowledge and belief: (i) incorporate without acknowledgment any material previously submitted for a degree or diploma in any institution of higher education; (ii) contain any material previously published or written by another person except where due reference is made in the text of this thesis; or (iii) contain any defamatory material. Signed Date 23 May 2011 v Acknowledgements I first would like to thank my two supervisors, A. Prof. Ray Froend and Prof. Will Stock. I can unreservedly say that without their patient support, guidance and encouragement I would not have made it this far. I wish to acknowledge the Water Corporation and Australian Research Council, who provided the financial support to make this project possible. The study site was located at Whiteman Park, and I would like to thank their Land & Environment Manager Chris Rafferty for her assistance with access and information. I am indebted to a large number of research assistants and other students who have assisted me in the field, laboratory and glasshouse. In particular, I wish to acknowledge Muriel Davies who has assisted me in many different aspects throughout the preparation of this thesis, including many long hours of field work. I am grateful for the assistance of Coral Newman for proofreading this thesis at short notice and for providing helpful and encouraging feedback. Thank you to my friends and family for their support throughout. Finally, thank you to Andrew Rafty for your never-ending help, encouragement and support over the years. vi TABLE OF CONTENTS USE OF THESIS ii ABSTRACT iii DECLARATION v ACKNOWLEDGEMENTS vi TABLE OF CONTENTS vii CHAPTER 1 General Introduction 1 CHAPTER 2 Study area and species descriptions 8 Dynamics of Banksia root growth relative to a seasonally CHAPTER 3 19 fluctuating water table. Introduction 19 Materials and Methods 24 Results 31 Discussion 43 Seasonal groundwater uptake by dominant canopy CHAPTER 4 50 species in a Banksia woodland. Introduction 50 Materials and Methods 53 Results 57 Discussion 62 Seedling root elongation rates for two phreatophytic CHAPTER 5 66 Banksia species with contrasting water requirements Introduction 66 Materials and Methods 69 Results 77 Discussion 83 Root response of phreatophytic Banksia exposed to rapid CHAPTER 6 86 rates of water table decline. Introduction 86 Materials and Methods 90 Results 95 Discussion 103 CHAPTER 7 General Discussion 109 REFERENCES 114 Chapter One General Introduction Groundwater accounts for more than 30% of the earth’s fresh water (Shiklomanov 1998), and a variety of ecosystems have developed in the presence of groundwater (Eamus et al. 2006). Groundwater may be defined as part of the soil profile that has reached maximum water holding capacity, with all soil pores filled with water, also referred to as the zone of saturation (Freeze & Cherry 1979; Eamus et al. 2006; Fig. 1.1). Plants which use groundwater are referred to as phreatophytic, from the Greek ‘phreatos’ – a well, and ‘phyte’, denoting a plant having a particular characteristic (Meinzer 1923). Phreatophytes can access groundwater either directly from the water table (the upper surface of groundwater) or from the capillary fringe, which sits above the water table and contains groundwater held by capillary action (Freeze & Cherry 1979; Eamus et al. 2006). Phreatophytes are prevalent in water-limited environments, where annual evapotranspiration exceeds annual rainfall, resulting in a net deficit in water availability (Abrahams & Parsons 1994; Cui & Shao 2005). This water deficit is exacerbated in habitats with soils that have low water-holding capacity, such as coarse sands (Sperry et al. 2002). In such environments, water availability in the unsaturated (vadose) zone is often unreliable, and, as a result, many species develop deep root systems to access deeper water sources, such as groundwater (Stone & Kalisz 1991; Canadell et al.