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First published online February 25, 2005; 10.1104/pp.104.058156 Plant Physiology 137:1139-1146 (2005) © 2005 American Society of Plant Biologists
Water Stress Deforms Tracheids Peripheral to the Leaf Vein of a Tropical Conifer1Department of Plant Science, University of Tasmania, Hobart, Tasmania 7001, Australia (T.J.B.); and Department of Organismic and Evolutionary Biology, Harvard University, Cambridge, Massachusetts 02183 (T.J.B., N.M.H.)
Just as a soggy paper straw is prone to yielding under the applied suction of a thirsty drinker, the xylem tracheids in leaves seem prone to collapse as water potential declines, impeding their function. Here we describe the collapse, under tension, of lignified cells peripheral to the leaf vein of a broad-leaved rainforest conifer, Podocarpus grayi de Laub. Leaves of Podocarpus are characterized by an array of cylindrical tracheids aligned perpendicular to the leaf vein, apparently involved in the distribution of water radially through the mesophyll. During leaf desiccation the majority of these tracheids collapsed from circular to flat over the water potential range 1.5 to 2.8 MPa. An increase in the percentage of tracheids collapsed during imposed water stress was mirrored by declining leaf hydraulic conductivity (Kleaf), implying a direct effect on water transport efficiency. Stomata responded to water stress by closing at 2.0 MPa when 45% of cells were collapsed and Kleaf had declined by 25%. This was still substantially before the initial indications of cavitation-induced loss of hydraulic conductance in the leaf vein, at 3 MPa. Plants droughted until 49% of tracheids had collapsed were found to fully recover tracheid shape and leaf function 1 week after rewatering. A simple mechanical model of tracheid collapse, derived from the theoretical buckling pressure for pipes, accurately predicted the collapse dynamics observed in P. grayi, substantiating estimates of cell wall elasticity and measured leaf water potential. The possible adaptive advantages of collapsible vascular tissue are discussed.
Leaves employ the strong cohesive properties of water to do the work of pulling water from the soil to prevent leaf desiccation during gas exchange (Dixon and Joly, 1895
To resist megapascals of crushing pressure across the cell wall, xylem conduits have evolved thick secondary walls incorporating lignin as a means of fortifying their tangential elastic modulus against collapse (Raven, 1977
To date, physiological work on xylem dysfunction has focused almost exclusively on cavitation as the process responsible for reduced hydraulic efficiency in plants under water stress. The assumption is that increasing water tension in plants exposed to drying soil or elevated transpiration leads to cavitation of the water in xylem conduits before water potential falls sufficiently low to collapse cells. Indeed, several papers have specifically addressed this issue and concluded that xylem conduits of soft and hardwoods are twice as resistant to collapse as they are to cavitation (Hacke et al., 2001
Leaves are the obvious place to look for evidence of xylem dysfunction by collapse under hydrostatic tension. Leaves experience the lowest water potentials in the plant while containing a large proportion of air, thus creating conditions for maximum pressure differentials across xylem cell walls. Also it is commonly the case that leaf veins terminate in large collapse-prone tracheids with thin, highly pitted walls (Esau, 1977
In attempting to quantify the extent of tracheid cell collapse in living leaves we focus here on the leaves of a member of the genus Podocarpus, the most common conifer genus south of the equator. Podocarpus is an unusual genus that produces the largest of all conifer leaves (up to 45 x 300 mm) while relying on a single vein per leaf for hydraulic supply. Podocarpus leaves depend on a network of extravenous tracheids (Bucholtz and Gray, 1948
Here we examine the response of cell geometry and leaf hydraulic conductance to water potential to determine whether cell collapse is likely to interfere with water conduction under field conditions in this species. A structural mechanical model is used to predict theoretical collapse pressures for conduits, assuming they behave as cylindrical pipes. The model, based on Timshenko's equation relating pipe size and wall properties to buckling pressure, is applied to the measured dimensions of ATT tracheids in the leaves of Podocarpus specimens.
Tracheid Collapse
Declining leaf water potential had a marked effect on the geometry of ATT tracheids as quantified by the circularity index (C). At water potentials above 1.5 MPa very little conduit deformation was observed, with 75% to 92% of tracheids exhibiting a round geometry (C > 0.8), while no cells appeared flattened (Figs. 2 and 3). At water potentials below 1.5 MPa, however, a sharp increase in the proportion of collapsed cells led to a drop in the mean C (Fig. 3) of ATT tracheids in the leaf. A strongly bimodal distribution of cell geometries existed in leaves at between 1.5 and 2.8 MPa (Fig. 2) with >75% of cells either circular (C > 0.8) or flattened (C < 0.4). This led to a high SD in mean cell circularity for leaves dehydrated below 1.5 MPa. A better index of the impact of cell collapse on water transport capacity of the ATT is the percentage of collapsed (and presumably dysfunctional) tracheids (C < 0.4). The percentage of collapsed cells was found to increase steeply as
Leaves frozen in situ while attached to trees exhibited identical behavior to those detached prior to desiccation. One sample tree was subjected to drought by withholding water, and after 3 weeks of drought, leaves were found to be at 2.25 to 2.3 MPa and stomata remained closed during the day. Tracheid collapse was observed at 49% ± 8%, which recovered to 0% 1 week after rewatering (Fig. 3). Occasional sectioning of tracheids in the midvein of leaves suggested that this xylem tissue was not prone to collapse (T.J. Brodribb, unpublished data).
Leaf hydraulic conductance declined rapidly from a mean maximum of 6.7 mmol m2 s1 MPa1 in leaves above 1.8 MPa to less than 1 mmol m2 s1 MPa1 in leaves at water potentials more negative than 3.0 MPa (Fig. 4). The leaf vein was found to be substantially more resistant to dysfunction under simulated xylem tension than the leaf lamina, illustrating a transition from 24% to 80% loss of hydraulic conductance over the range 3 to 4 MPa (Fig. 4A). Tracheid collapse on the other hand was much better correlated with the loss of whole-leaf hydraulic conductance. Declining Kleaf was closely mirrored by the increase in the percentage of collapsed tracheids in the ATT (Fig. 4B).
Stomatal conductance responded to a range of water potentials depending on the humidity to which leaves were exposed during desiccation. Despite this, the water potential resulting in 90% stomatal closure was consistent among all replicates, occurring at a mean water potential of 2.0 ± 0.25 MPa. This number was also independent of the rate of desiccation and the time after cutting from the tree (T.J. Brodribb, unpublished data). The timing of stomatal closure corresponded with the early stages of tracheid collapse (45%) and the initial decline of Kleaf (25% depression). The water potential of 90% stomatal closure did not appear related to the vulnerability of the vein xylem (Fig. 4A).
Tracheid wall thickness and cell radius were highly correlated in the ATT (r2 = 0.61; P < 0.001). Tracheid cell sizes ranged from a minimum diameter of 12 µm to a maximum slightly over 30 µm (Fig. 5). A similar range of tracheid diameters was observed in the midvein xylem where the largest cells were 24 µm (data not shown). Pitting in ATT tracheids was found to be frequent in cells bordering spongy mesophyll, while among the bulk of tracheids only endwalls were densely pitted. Lateral walls exhibited single rows of pits in regions of contact between tracheids.
By treating tracheids as pipes (ignoring areas of structural weakening such as pitted regions of the wall) it was possible to estimate the collapse behavior of a representative sample of 80 tracheids using the theoretical buckling pressure given in Equation 2. The predicted distribution of collapse pressures (assuming no cavitation in tracheids) was very close to the observed pattern when an elastic modulus of M = 800 MPa was used for the tracheid wall (Fig. 6). The lower value of 500 MPa for M underestimated the wall strength, predicting cells to collapse at less negative water potentials.
The collapse of tracheids under water tension is shown here to be an important feature of the physiology of the conifer Podocarpus grayi. The tracheids prone to collapse (ATT) were those occurring outside the leaf vein and were involved in the delivery of water radially from the vein toward the leaf margin. It is significant to note that a great many gymnosperms, particularly those in the southern hemisphere, possess similar accessory xylem either in the form of ATT (Podocarpaceae and Cycas) or as elongate idiosclerieds oriented radially (Papuacedrus) or parallel (Agathis) to the leaf vein. Given that xylem in the needles of several Pinus species has also recently been shown to collapse under tension (Cochard et al., 2004 The data presented strongly suggest that the collapse of ATT tracheids in P. grayi is likely to have directly caused the decline in Kleaf in this species. The pattern of decreasing Kleaf in P. grayi under water stress closely matched the percentage of tracheids observed to be collapsed in the ATT (Fig. 4B). Hydraulic flow through tracheids crushed to the collapsed category (geometrically defined by a value of C < 0.4) would be <6% of the conductance of uncollapsed conduits (assuming that tracheids collapse into an ellipse shape), effectively deactivating them as water-conducting tissues. Deactivation of the ATT by cell collapse must greatly impede the flow of water through the leaf as a whole, given that water would be forced to travel many thousands of microns through nonspecialized cells before reaching the sites of evaporation. For this reason it is not surprising that stomatal closure in P. grayi was correlated with the process of cell collapse rather than the subsequent process of xylem cavitation in the midrib (Fig. 4A).
Interestingly, we found stomatal closure in response to leaf desiccation to occur midway through the loss of Kleaf and tracheid collapse (Fig. 4, A and B). Closure of stomata after the onset of xylem dysfunction has been shown to occur in some tropical angiosperms but appears to require some sort of refiling process to repair embolized xylem (Bucci et al., 2003
In fact it may be the case that the collapse of ATT tracheids is an adaptive means of regulating leaf water potential without risking embolism. Being a mechanical process, the collapse of tracheids is likely to release the bulk of the lumen water over a small range of water potentials (i.e. at the point of buckling of the cell wall). Given that most tracheids buckled under a tension of 1.5 to 2.5 MPa, this would provide a specific capacitance to the leaf over the water potential range of stomatal closure. From cross sectional area measurements we calculated that an average of 2,300 mmol m2 of water was present in nondeformed ATT tracheids. This is a significant volume when it is considered that only 1,450 mmol m2 is required to hydrate an average P. grayi leaf from 2 MPa to 0 MPa (T.J. Brodribb, unpublished data). Under conditions of rapidly declining vapor-pressure difference, the release of ATT water during collapse of cells would significantly delay water potential decline in the leaf, given that maximum rates of E in P. grayi were close to 1 mmol m2 s1 (T.J. Brodribb, unpublished data). This might provide a water potential buffer, enabling complete stomatal closure before leaf water potential is allowed to fall to a point where vein (or stem) embolism is initiated. Such a process would be energetically preferable to a system of diurnal embolism and refiling because, unlike conduit embolism, tracheid collapse appears to be readily reversed once water supply is reestablished (Fig. 3) making for a cost-free recovery of Kleaf post stress. A system of collapse-dependent capacitance may be important in a great many leaves of both conifers and angiosperms, given that many species from both groups possess nonliving lignified tissues outside the leaf vascular bundle (Esau, 1977
Collapse of tracheid cells in the leaf attests to the existence of large negative pressures in the xylem. Although the application of Equation 2 should accurately predict collapse pressures in tubes, there is some uncertainty in the magnitude of the elastic modulus for the tracheid wall and the weakening effect of pitting. Although the presence of (unbordered) pits in the walls of ATT tracheids reduces its resistance to crushing, SEM examination revealed that only a small percentage of the tracheids measured were sectioned through the pit aperture. Hence most of the cells observed were of uniform wall thickness and, as such, should adhere to the buckling equation (2) used here (Timoshenko, 1930 In many plant groups including conifers, cycads, and many angiosperm families, the final delivery of water from xylem cells to mesophyll tissue takes place through lignified cells with large lumens and highly developed pitting. It is these cells, rather than the xylem in vascular bundles that seems most prone to dysfunction by collapse. Their irregular geometry, proximity to air spaces, and exposure to the highest tensions in the plant make their cell walls prone to buckling, but by the same token, their geometry will also make collapse difficult to observe under tension. On the other hand these cells may also be prone to cavitation, alleviating hoop stress on the cells prior to collapse. Whatever the story, we believe more attention should be focused upon tracheids within the leaf if we are to achieve a better understanding of the delivery of water to leaves under tension.
Plant Material All measurements were carried out on two 8-year-old specimens of Podocarpus grayi grown from seed under ambient glasshouse conditions (temperature range 5°C to 36°C, maximum light intensity 950 µmol m2 s1) at the University of Tasmania, Hobart. Although the genus Podocarpus is found throughout the southern hemisphere in moist forest and subalpine scrub, P. grayi is restricted to the far northeast of Australia where it grows as a small subcanopy tree in rainforest from sea level to approximately 600-m altitude. Leaves of P. grayi are linear, typically 80 to 150 mm in length and 10 to 15 mm in diameter with only a single midrib for venation.
Leaf hydraulic conductance (Kleaf) was measured using a leaf rehydration technique (Brodribb and Holbrook, 2003
leaf was > 0.05 MPa, after which leaves were detached for determination of PV relations on the leaf tissue. Leaf weight and water potential were measured periodically during slow desiccation of sample leaves in the laboratory. The initial (linear) slopes of the relative water content (RWC) versus leaf curves yielded the leaf capacitance function in terms of RWC. Calculation of Kleaf (mmol m2 s1 MPa1) requires that leaf capacitance be calculated in absolute terms and normalized by leaf area. To do this, the capacitance calculated from the PV relationship was multiplied by the saturated mass of water in the leaf and then divided by leaf area (Koide et al., 1991
Five leaves were excised under water and two longitudinal cuts made parallel to the midrib (5 mm either side) along the length of the leaf. These cuts were designed to minimize resistance to radial leakage of water out of the midrib during flow measurements. Leaves were attached to a steady-state flow meter (Zwieniecki et al., 2000
Twenty-five leaves from each of the two P. grayi individuals were cut from trees during the morning while plants were hydrated and allowed to dry for different periods to yield a range of leaf water potentials from 0.35 MPa to 4MPa. For each leaf specimen, leaf water potential was determined by cutting off the lower third of the leaf for pressure bomb measurement while the upper two-thirds of the leaf were sealed in plastic bags to prevent further water loss and used for microscope examination. The proportion of collapsed cells was determined on leaves snap frozen in liquid nitrogen to preserve the tissue conformation under tension. Leaves were placed into a small aluminum specimen holder and submerged in liquid nitrogen. Each leaf was then trimmed to about 20 mm in length and placed in a shallow polystyrene well such that the leaf remained submerged in liquid nitrogen. The ATT runs perpendicular to the midrib, so leaves were cut 5 mm from the margin, parallel to the midrib to expose the ATT tracheids in cross section. Sectioned leaves were examined at 20x magnification under a fluorescence microscope (Axioscop, Carl Zeiss, Oberkochen, Germany) while still partially submerged in liquid nitrogen, and photographed using a digital camera (Axiocam, Carl Zeiss) attached to a photographic tube. Ten images per leaf were taken at approximately 2-mm intervals along the 20-mm leaf section, each containing approximately 15 tracheids. Tracheid outlines were later traced in Adobe Photoshop (Adobe Systems, Mountain View, CA) and transferred to ImageJ for analysis. Degree of cell collapse was expressed as a C described by Equation 1.
(1) C = 4 Circularity data were first analyzed as a mean value per leaf (±SD, n = 150); however, geometries were found to exhibit a strongly bimodal distribution of highly collapsed or uncollapsed cells. For this reason the percentage of collapsed cells (C < 0.4) and uncollapsed cells (C > 0.8) was also calculated for each leaf sample. To test whether collapse occurred while leaves were attached to the tree, a single tree was left unwatered for 3 weeks to simulate drought. Once leaf water potential had dropped sufficiently to prevent stomatal opening during the day (2.3 MPa), three leaves were dipped into liquid nitrogen while attached to the tree and harvested for shape analysis as above. The tree was then rewatered and, once photosynthesis had recovered to 90% of predrought levels, another three leaves were frozen on the plant and harvested for tracheid shape determination.
Leaf water potential at stomatal closure was determined on detached leaves under a range of evaporative gradients to test the consistency of the stomatal response to leaf water potential (Brodribb and Holbrook, 2004a
A sample of five leaves were hydrated and sectioned 3 mm from the margin to expose the ATT in cross section as above. These sections were then serially dehydrated in alcohol and placed in an automated critical point drier where they were dried and gold coated. Samples were then examined under an ESEM (Quanta 200, Philips, Eindhoven, The Netherlands) and 30 images of ATT tracheids were photographed at 1,500x magnification along the length of the five sample sections. Images were then analyzed using graphics software to measure cell diameter and cell wall thickness of 80 ATT tracheids.
In hydrated leaves the ATT tracheids were very close to circular in cross section with only small regions of contact between cells. Hence in this case tracheid geometry approximates a cylindrical tube (rather than a deflecting plate as is the case with neighboring vessels; Hacke et al., 2001
For each of the 80 cells surveyed, a critical collapse pressure (Pcr) was predicted from Equation 2. This range of pressures was taken to represent the mean behavior of tracheids in the leaf and used to model the progress of cell collapse in response to decreasing leaf water potential. This modeled response was then compared with direct observations of frozen leaves described above.
When present, curves were fitted to the data to show pattern rather than mechanism, and hence best fit models were adopted. For Kleaf vulnerability a cumulative normal distribution was fitted as described previously (Brodribb and Hill, 1999
The authors are grateful to Prof. Gustaaf Halegraeff for the use of the fluorescence microscope. Dr. Greg Jordan provided useful discussion and lab space. Prof. Holbrook was hosted by the University of Tasmania during her sabbatical. Received December 12, 2004; returned for revision January 10, 2005; accepted January 10, 2005.
1 This work was supported by the National Science Foundation (grant no. IBN 0212792) and by a grant from the National Geographic Society (grant no. 747503). Article, publication date, and citation information can be found at www.plantphysiol.org/cgi/doi/10.1104/pp.104.058156. * Corresponding author; e-mail brodribb{at}fas.harvard.edu; fax 61362262698.
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