Articulo 15. Practicas higiénicas y medidas de protección
3.5.2 Decreto 3075 capítulo VIII Restaurantes y establecimientos de consumo de alimentos
Reponses of the grey mangrove Avicennia marina (Forssk.) Vierh. to growth salinity were studied at scales ranging from the growth of whole plants to the function of individual leaves. The results revealed insights on water transport, storage, and use along a salinity gradient. The key findings and their implications for future research are discussed below:
Physiological and anatomical analyses were combined in Chapter 2 to identify processes underlying growth responses of the mangrove Avicennia marina to salinities ranging from fresh to seawater conditions. The seedlings failed to grow in 0 to 5% seawater, whereas maximal growth occurred in 50 to 75% seawater, which, in physiological terms, indicated that A. marina is an obligate halophyte. Anatomical data revealed variation in rates of development and composition of hydraulic tissues that were consistent with salinity-‐dependent patterns in water use and growth, including a structural explanation for low stomatal conductance and growth in low salinity. These results invite questions about the generality of the growth response.
Other mangrove species, such as Ceriops tagal (Smith, 1988), Bruguiera parviflora, Ceriops australis, C. decandra (Ball, 2002), Rhizophora mangle (Werner & Stelzer, 1990), and Sonneratia alba (Ball & Pidsley, 1995) , have also been reported to grow either very poorly or not at all in fresh water. However, Krauss and Ball (2013) pointed out that these apparent responses to freshwater conditions were confounded by low nutrient concentrations. This issue was eliminated in the present study, and the results provided strong evidence that Avicennia marina is an obligate halophyte (Chapter 2). It would be useful to revisit the growth of other mangrove species under freshwater conditions.
In Chapter 2, the absence of seawater prevented proper development of xylem conduits of A. marina, thus, constraining water uptake and limiting leaf gas exchange and plant growth. Many possibilities could be explored. One hypothesis is that A. marina may have evolved a requirement for Na+, in which Na+ partially replaces the
seawater, K+ concentrations on a bulk leaf water basis fell from 300 to 60 mM while Na+ increased from 20 to 947 mM. Under sodium deficiency, if potassium were to substitute imperfectly for sodium, then signals for, say, xylem differentiation or generation of turgor required for cell expansion could be impaired.
In Chapter 3, the pressure-‐volume relationships in field grown leaves of the mangrove, Avicennia marina, exhibited three domains dominated successively by 1) the presence and consumption of extracellular water, 2) variable turgor and loss of intracellular water, and 3) osmotic behavior of flaccid cells and plasmolysis. Visualization of leaf lamina with reference to the three-‐domain PV curve revealed a cascade of water storage compartments that operated over different ranges of hydration. When leaves were fully hydrated, extracellular water storage occurred in multiple sites, including hollow trichomes and novel structures named “cisternae”. This extracellular water in the leaf could enable transient water use without substantive turgor loss when other factors, such as high soil salinity, constrain rates of water transport.
Is extracellular water storage a common feature in mangroves? Leaf morphology is diverse among mangroves. Species differ in leaf size, tissue composition, the presence of trichomes and glands, etc. It would be useful to extend the study to other species of mangroves that differ in leaf structure and complexity. PV curve analyses can be used to identify and quantify extracellular water storage in different species. Further anatomical analyses could examine the diversity in the sites and structures involved in extracellular water storage among mangrove species. Finally, there is much to be learnt about how water is absorbed by leaves, distributed to storage systems, and accessed during leaf dehydration.
In Chapter 4, leaf turgor loss points were shown to correlate with soil water salinity. Cellular osmotic adjustment was likely to maintain water supply from roots under the most severe conditions. Leaves, however, could not be fully hydrated or fully turgid with only water supplied from deep roots. These results indicated that different water sources, for example, surface water of lower salinity, or dew and rainfall, play an important role in plant function and growth, potentially enabling greater duration of higher stomatal conductance and hence also assimilation rates when water supply from the roots is constrained by high soil salinities. It would be exciting to expand the
study to test the generality of these findings among other mangrove species that differ in leaf anatomy, salt tolerance and distribution along salinity gradients.
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