Danielle Creek
University of Sydney
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Featured researches published by Danielle Creek.
Proceedings of the National Academy of Sciences of the United States of America | 2016
Mary A. Heskel; Odhran S. O'Sullivan; Peter B. Reich; Mark G. Tjoelker; Lasantha K. Weerasinghe; Aurore Penillard; John J. G. Egerton; Danielle Creek; Keith J. Bloomfield; Jen Xiang; Felipe Sinca; Zsofia R. Stangl; Alberto Martinez-de la Torre; Kevin L. Griffin; Chris Huntingford; Vaughan Hurry; Patrick Meir; Matthew H. Turnbull; Owen K. Atkin
Significance A major concern for terrestrial biosphere models is accounting for the temperature response of leaf respiration at regional/global scales. Most biosphere models incorrectly assume that respiration increases exponentially with rising temperature, with profound effects for predicted ecosystem carbon exchange. Based on a study of 231 species in 7 biomes, we find that the rise in respiration with temperature can be generalized across biomes and plant types, with temperature sensitivity declining as leaves warm. This finding indicates universally conserved controls on the temperature sensitivity of leaf metabolism. Accounting for the temperature function markedly lowers simulated respiration rates in cold biomes, which has important consequences for estimates of carbon storage in vegetation, predicted concentrations of atmospheric carbon dioxide, and future surface temperatures. Plant respiration constitutes a massive carbon flux to the atmosphere, and a major control on the evolution of the global carbon cycle. It therefore has the potential to modulate levels of climate change due to the human burning of fossil fuels. Neither current physiological nor terrestrial biosphere models adequately describe its short-term temperature response, and even minor differences in the shape of the response curve can significantly impact estimates of ecosystem carbon release and/or storage. Given this, it is critical to establish whether there are predictable patterns in the shape of the respiration–temperature response curve, and thus in the intrinsic temperature sensitivity of respiration across the globe. Analyzing measurements in a comprehensive database for 231 species spanning 7 biomes, we demonstrate that temperature-dependent increases in leaf respiration do not follow a commonly used exponential function. Instead, we find a decelerating function as leaves warm, reflecting a declining sensitivity to higher temperatures that is remarkably uniform across all biomes and plant functional types. Such convergence in the temperature sensitivity of leaf respiration suggests that there are universally applicable controls on the temperature response of plant energy metabolism, such that a single new function can predict the temperature dependence of leaf respiration for global vegetation. This simple function enables straightforward description of plant respiration in the land-surface components of coupled earth system models. Our cross-biome analyses shows significant implications for such fluxes in cold climates, generally projecting lower values compared with previous estimates.
Plant Cell and Environment | 2015
Markus Nolf; Danielle Creek; Remko A. Duursma; Joseph A. M. Holtum; Stefan Mayr; Brendan Choat
Coordination of stem and leaf hydraulic traits allows terrestrial plants to maintain safe water status under limited water supply. Tropical rain forests, one of the worlds most productive biomes, are vulnerable to drought and potentially threatened by increased aridity due to global climate change. However, the relationship of stem and leaf traits within the plant hydraulic continuum remains understudied, particularly in tropical species. We studied within-plant hydraulic coordination between stems and leaves in three tropical lowland rain forest tree species by analyses of hydraulic vulnerability [hydraulic methods and ultrasonic emission (UE) analysis], pressure-volume relations and in situ pre-dawn and midday water potentials (Ψ). We found finely coordinated stem and leaf hydraulic features, with a strategy of sacrificing leaves in favour of stems. Fifty percent of hydraulic conductivity (P50 ) was lost at -2.1 to -3.1 MPa in stems and at -1.7 to -2.2 MPa in leaves. UE analysis corresponded to hydraulic measurements. Safety margins (leaf P50 - stem P50 ) were very narrow at -0.4 to -1.4 MPa. Pressure-volume analysis and in situ Ψ indicated safe water status in stems but risk of hydraulic failure in leaves. Our study shows that stem and leaf hydraulics were finely tuned to avoid embolism formation in the xylem.
Tree Physiology | 2014
Lasantha K. Weerasinghe; Danielle Creek; Kristine Y. Crous; Shuang Xiang; Michael J. Liddell; Matthew H. Turnbull; Owen K. Atkin
We explored the impact of canopy position on leaf respiration (R) and associated traits in tree and shrub species growing in a lowland tropical rainforest in Far North Queensland, Australia. The range of traits quantified included: leaf R in darkness (RD) and in the light (RL; estimated using the Kok method); the temperature (T)-sensitivity of RD; light-saturated photosynthesis (Asat); leaf dry mass per unit area (LMA); and concentrations of leaf nitrogen (N), phosphorus (P), soluble sugars and starch. We found that LMA, and area-based N, P, sugars and starch concentrations were all higher in sun-exposed/upper canopy leaves, compared with their shaded/lower canopy and deep-shade/understory counterparts; similarly, area-based rates of RD, RL and Asat (at 28 °C) were all higher in the upper canopy leaves, indicating higher metabolic capacity in the upper canopy. The extent to which light inhibited R did not differ significantly between upper and lower canopy leaves, with the overall average inhibition being 32% across both canopy levels. Log-log RD-Asat relationships differed between upper and lower canopy leaves, with upper canopy leaves exhibiting higher rates of RD for a given Asat (both on an area and mass basis), as well as higher mass-based rates of RD for a given [N] and [P]. Over the 25-45 °C range, the T-sensitivity of RD was similar in upper and lower canopy leaves, with both canopy positions exhibiting Q10 values near 2.0 (i.e., doubling for every 10 °C rise in T) and Tmax values near 60 °C (i.e., T where RD reached maximal values). Thus, while rates of RD at 28 °C decreased with increasing depth in the canopy, the T-dependence of RD remained constant; these findings have important implications for vegetation-climate models that seek to predict carbon fluxes between tropical lowland rainforests and the atmosphere.
Proceedings of the National Academy of Sciences of the United States of America | 2016
Mary A. Heskel; Owen K. Atkin; Odhran S. O'Sullivan; Peter B. Reich; Mark G. Tjoelker; Lasantha K. Weerasinghe; Aurore Penillard; John J. G. Egerton; Danielle Creek; Keith J. Bloomfield; Jen Xiang; Felipe Sinca; Zsofia R. Stangl; Alberto Martinez-de la Torre; Kevin L. Griffin; Chris Huntingford; Vaughan Hurry; Patrick Meir; Matthew H. Turnbull
Reply to Adams et al. : Empirical versus process-based approaches to modeling temperature responses of leaf respiration
Tree Physiology | 2018
Brendan Choat; Markus Nolf; Rosana López; Jennifer M. R. Peters; Madeline R Carins-Murphy; Danielle Creek; Timothy J. Brodribb
Drought stress can result in significant impairment of the plant hydraulic system via blockage of xylem conduits by gas emboli. Recovery after drought stress is an essential component of plant survival but is still a poorly understood process. In this study, we examined the capacity of woody species from two genera (Eucalyptus and Quercus) to refill embolized xylem vessels during a cycle of drought and recovery. Observations were made on intact plants of Eucalyptus calmudulensis, E. grandis, E. saligna and Quercus palustris using X-ray microtomography. We found no evidence of an effective xylem refilling mechanism in any of the plant species. Despite rehydration and recovery of plant water potential to near pre-drought levels, embolized vessels were not refilled up to 72 h after rewatering. In E. saligna, water droplets accumulated in previously air-filled vessels for a very small percentage of vessels. However, no instances of complete refilling that would restore embolized vessels to hydraulic function were observed. Our observations suggest that rapid refilling of embolized vessels after drought may not be a wide spread mechanism in woody plants and that embolism formed during drought represents long term cost to the plant hydraulic system.
New Phytologist | 2015
Owen K. Atkin; Keith J. Bloomfield; Peter B. Reich; Mark G. Tjoelker; Gregory P. Asner; Damien Bonal; Gerhard Bönisch; Matt G. Bradford; Lucas A. Cernusak; Eric G. Cosio; Danielle Creek; Kristine Y. Crous; Tomas F. Domingues; Jeffrey S. Dukes; John J. G. Egerton; John R. Evans; Graham D. Farquhar; Nikolaos M. Fyllas; Paul P. G. Gauthier; Emanuel Gloor; Teresa E. Gimeno; Kevin L. Griffin; Rossella Guerrieri; Mary A. Heskel; Chris Huntingford; Françoise Yoko Ishida; Jens Kattge; Hans Lambers; Michael J. Liddell; Jon Lloyd
Global Change Biology | 2017
Odhran S. O'Sullivan; Mary A. Heskel; Peter B. Reich; Mark G. Tjoelker; K.W. Lasantha K. Weerasinghe; Aurore Penillard; Lingling Zhu; John J. G. Egerton; Keith J. Bloomfield; Danielle Creek; Nur H. A. Bahar; Kevin L. Griffin; Vaughan Hurry; Patrick Meir; Matthew H. Turnbull; Owen K. Atkin
Global Change Biology | 2017
Andrew P. Scafaro; Shuang Xiang; Benedict M. Long; Nur H. A. Bahar; Lasantha K. Weerasinghe; Danielle Creek; John R. Evans; Peter B. Reich; Owen K. Atkin
Global Change Biology | 2017
Varsha S. Pathare; Kristine Y. Crous; Julia Cooke; Danielle Creek; David S. Ellsworth
Annals of Botany | 2017
Aimee E. Bourne; Danielle Creek; Jennifer M. R. Peters; David S. Ellsworth; Brendan Choat