China’s water footprint by province,and inter-provincial transfer of virtual water

Water shortages and the uneven distribution of water resources restrict China’s sustainable development. The concepts of virtual water and water footprints provide a new approach to alleviate regional shortages of Chinese water resources by the inter-provincial allocation of commercial water resources. In this study, an interregional input-output model was applied to quantitatively estimate the water footprint of each province in China and to quantify the inter-provincial transfer of virtual water. The results indicated that there was considerable diversity in the water footprints of the various provinces. Provinces with larger populations and greater GDP had larger water footprints, and developed regions had higher proportions of external water footprints. From the perspective of final demand, local consumption was the main factor driving the water footprints of these provinces. From the perspective of sectoral structure, the agricultural water footprint had a larger proportion in these provinces. The transfer of virtual water in China did not occur from regions with abundant water resources to those suffering from water shortages, but it generally occurred from west to east, from inland to coastal areas, and from underdeveloped to developed regions. Many water-deficient regions also had large net virtual water exports. Water shortages in China will be alleviated by the enhancement of industrial water-use efficiency in water-deficient regions, the transfer of water-intensive industries to regions with abundant water resources, and the development of tertiary industries with low water consumption.     

So,why is water biologically important?

Some brief impressionistic and necessarily subjectively based comments on the content of the Discussion Meeting are made. It is pointed out that the principal thrust of most of the presentations was directed towards structural aspects of proteins in various media. Comments are also made on the necessary interplay between the medium in which biomolecules occur and the interatomic forces between the atoms comprising the biomolecules. Some speculation is made on the possibility of life-forms existing in extreme environments.     

Effect of uniconazole and limited water on growth,water relations,and mineral nutrition of “Lalandei” Pyracantha

Pyracantha (Pyracantha coccinea M. J. Roem. Lalandei) plants were treated with uniconazole at 0.5 mg ai container^–1 as a medium drench, 150 mg ai L^–1 as a foliar spray, or left untreated. Plants from all treatments were placed under three water regimes: drought acclimated, nonacclimated and later exposed to drought, or nonstressed. Acclimated plants were conditioned by seven 4-day stress cycles (water withheld), while nonacclimated were well watered prior to a single 4-day stress cycle at the same time as the seventh drought cycle of acclimated plants. Nonstressed plants were well watered throughout the study. Nonstressed plants had higher leaf water potentials and leaf conductances than acclimated and nonacclimated plants, and transpiration rates were higher in nonacclimated than acclimated plants. Uniconazole did not affect leaf water potential, leaf conductance, or transpiration rate. Acclimated plants had smaller leaf areas and leaf, stem, and root dry weights than nonacclimated or nonstressed plants. Plants drenched with uniconazole had the lowest stem and root dry weights. Acclimated plants also contained higher N concentrations than nonacclimated or nonstressed plants, and higher P concentrations than nonacclimated plants. Uniconazole medium drench treatments increased levels of Mn and P. Calcium concentration was increased in plants receiving either medium drench or foliar applications.     

How do salinity and water stress affect transport of water,assimilates and ions to tomato fruits?

The study was conducted in order to determine whether water stress affects the accumulation of dry matter in tomato fruits similarly to salinity, and whether the increase in fruit dry matter content is solely a result of the decrease in water content. Although the rate of water transport to tomato fruits decreased throughout the entire season in saline water irrigated plants, accumulation rates of dry matter increased significantly. Phloem water transport contributed 80–85% of the total water transport in the control and water-stressed plants, and over 90% under salinity. The concentration of organic compounds in the phloem sap was increased by 40% by salinity. The rate of ions transported via the xylem was also significantly increased by salinity, but their contribution to fruit osmotic adjustment was less. The rate of fruit transpiration was also markedly reduced by salinity. Water stress also decreased the rate of water transport to the tomato fruit and increased the rate of dry matter accumulation, but much less than salinity. The similar changes, 10–15%, indicate that the rise in dry matter accumulation was a result of the decrease in water transport. Other parameters such as fruit transpiration rates, phloem and xylem sap concentration, relative transport via phloem and xylem, solutes contributing to osmotic adjustment of fruits and leaves, were only slightly affected by water stress. The smaller response of these parameters to water stress as compared to salinity could not be attributed to milder stress intensity, as leaf water potential was found to be more negative. Measuring fruit growth of girdled trusses, in which phloem flow was inactive, and comparing it with ungirdled trusses validated the mechanistic model. The relative transport of girdled as compared to ungirdled fruits resembled the calculated values of xylem transport.     

How amyloplasts,water deficit and root tropisms interact?

Hydrotropism, the differential growth of plant roots directed by a moisture gradient, is a long recognized, but not well-understood plant behavior. Hydrotropism has been characterized in the model plant Arabidopsis. Previously, it was postulated that roots subjected to water stress are capable of undergo water-directed tropic growth independent of the gravity vector because of the loss of the starch granules in root cap columella cells and hence the loss of the early steps in gravitropic signaling. We have recently proposed that starch degradation in these cells during hydrostimulation sustain osmotic stress and root growth for carrying out hydrotropism instead of reducing gravity responsiveness. In addition, we also proposed that abscisic acid (ABA) and water deficit are critical regulators of root gravitropism and hydrotropism, and thus mediate the interacting mechanism between these two tropisms. Our conclusions are based upon experiments performed with the no hydrotropic response (nhr1) mutant of Arabidopsis, which lacks a hydrotropic response and shows a stronger gravitropic response than that of wild type (WT) in a medium with an osmotic gradient.Key words: starch, water deficit, auxin, abscisic acid, gravitropism, hydrotropismRoots of land plants sense and respond to different stimuli, some of which are fixed in direction and intensity (i.e., gravity) while other vary in time, space, direction and intensity (i.e., obstacles and moisture gradients). Directed growth of roots in relation to a gradient in moisture is called hydrotropism and begins in the root cap with the sensing of the moisture gradient. However, since gravity is an omnipresent accompaniment of Earthly life and many living process have evolved with it as a background constant, it is not surprising that root hydrotropism interacts with gravitropism.¹ The hydrotropic response in Arabidopsis, compare with other plants such as pea and cucumber^2,3 is readily observed even in the presence of gravity.^4,5 When Arabidopsis roots are subjected to a water gradient, such that the source of water is placed 180° opposed to the gravity vector, the roots will grow upwards, displaying positive hydrotropism. Therefore, it has been feasible to isolate so far two Arabidopsis mutants affected in their hydrotropic response.^5,6 Analysis of these mutants reveals new insights of the mechanism of hydrotropism. For one hand, the no hydrotropic response (nhr1) mutant lacks a hydrotropic response, and shows a stronger gravitropic response than that of wt and a modified wavy growth response in a medium with an osmotic gradient.^5,7 On the other hand, the mizu-kussei1 (miz1) mutant did not exhibit hydrotropism and showed regular gravitropism.⁶ Hence, the root hydrotropic response is both linked and unlinked from the gravitropic one. Nonetheless, miz1 roots also showed a reduced phototropism and a modified wavy growth response. This indicates that both MIZ1 and NHR1 are not exclusive components of the mechanism for hydrotropism and supports the notion that the root cap has assessment mechanisms that integrate many different environmental influences to produce a final integrated response.⁸ Thus, the physiological phenomena distinctively displayed by roots in order to forage resources from the environment are the result of integrated responses that resulted from many environmental influences sensed in the root cap.In the course of studying how gravity and water availability affected the perception and assessment of each other in root cap cells that generated the final root tropic response, we found that ABA is a critical regulator of the signal transduction mechanism that integrated these two-root tropisms.⁷ For this, we analyzed the long-term hydrotropic response of Arabidopsis roots in an osmotic gradient system. ABA, locally applied to seeds or root tips of nhr1, significantly increased root downward growth in a medium with an osmotic gradient (root length of nhr1 seedlings grown in this medium were on average 12.5 mm and plus 10 µM ABA were 25.1 mm). On the other hand, WT roots germinated and treated locally with ABA in this system were strongly gravitropic, albeit they had almost no starch in amyloplasts of root cap columella cells. Hydrotropically stimulated nhr1 roots, with or without ABA, maintained starch in amyloplastas, as opposed to those of WT. Therefore, the near-absence (WT) or abundant presence (nhr1) of starch granules does not affect the extent of downward gravitropism of roots in an osmotic gradient medium. Starch degradation in the wt might participate in osmoregulation by which root cells maintain turgor and consequently carry out hydrotropism, instead of reducing gravity responsiveness. In fact, it was just recently published that salt-induced rapid degradation of starch in amyloplasts is not likely the main reason for a negative gravitropic response seen under salt stress, because sos mutant roots of Arabidopsis showed negative gravitropic growth without any apparent rapid digestion of starch granules.⁹ Additionally, the stems of overwintering tubers of Potamogeton pectinatus are capable of elongating much faster in the absence than in the presence of oxygen for up to 14 days and its stems has an enhanced capacity for gravitropic movements in completely anoxic conditions.¹⁰ These authors hypothesized that ABA and starch degradation in the starchy tuber sustained stem cell elongation and cell division as well as differential growth required for the gravitropic response in these aquatic plants. These data taken together suggest that in conditions of anoxia, or water stress, ABA and degradation of starch play a critical role in the ability to survive relatively prolonged periods of unfavorable growth conditions. These players are critical when water or minerals are scarce since they regulate the enhancement of root downward growth. However, since roots can trail humidity gradients in soil, they can modulate their branching patterns (architecture) and thus respond to hydrotropism once a water-rich patch is found. Then the response of plants to gravity is principally one of nutrition (shoots to light, roots to mineral and water) and consequently must be regulated according to the long- and short-term environmental variables that occur during the development of the plant.Differential growth that occurs during the gravitropic and phototropic response has been explained according to the Cholodny-Went hypothesis, which states that the lateral transport of auxin across stimulated plant tissues is responsible for the curvature response.¹¹ Analysis of hydrotropism in some Arabidopsis agravitropic auxin transport mutants has demonstrated that these mutations do not influence their hydrotropic response.⁴ Furthermore, current pharmacological studies using inhibitors also indicated that both auxin influx and efflux are not required for hydrotropic response whereas auxin response is necessary for it.¹² These authors suggested a novel mechanism for auxin in root hydrotropism. Here, we analyzed whether asymmetric auxin distribution takes place across hydrotropically-stimulated roots using transgenic plants carrying a responsive auxin promoter (DR5) driving the expression of β-glucuronidase (GUS) or green fluorescent protein (GFP)^13,14 in wt and nhr1 backgrounds. Wt and nhr1 roots hydrotropically stimulated in a system with air moisture gradient⁵ showed no asymmetric expression of the DR5:: GUS or DR5::GFP (Fig. 1A and B). Nonetheless, nhr1 roots showed a substantial decrease in the signal driven by the DR5::GUS and GFP reporters in humidity saturated conditions (Fig. 1A, part b and B, part b), which might indicate that auxin-induced gene expression in the root cap was inhibited. It remains to be determined the significance of this inhibition in the no hydrotropic response phenotype displayed by nhr1 roots. Determination of the DR5::GUS expression in wt and nhr1 roots growing in an osmotic gradient medium for testing long-term hydrotropism revealed that the GUS signal was to some extent diminished in both wt or in nhr1 roots (Fig. 2C and D) compared to those roots growing in normal medium (Fig. 2A and B). An inhibitor of auxin response reduced hydrotropism,¹² and also inhibited auxin-dependent DR5::GUS expression.¹⁵ However, a decrease of DR5::GUS in wt root tips was not an impediment for developing an hydrotropic response. On the other hand, nhr1 roots also showed a decrease of DR5::GUS expression (Fig. 2B and D) and a complete absence of DR5::GFP (data not shown), which did not influence the extent of downward root gravitropism in water deficit conditions. Therefore, it is difficult to assign a role of auxin-induce gene expression in hydrotropism and further studies are required in order to unravel this issue. Furthermore, it needs to be resolved whether these expression studies oppose the idea that gradients in auxin precede differential growth in response to humidity gradients.Open in a separate windowFigure 1DR5:: GUS (A) and DR5::GFP (B) activity in the wild type NHR1 and nhr1 backgrounds. (A) Root tips hydrostimulated in a system with air moisture gradient (C and D) or grown in a saturated water conditions (A and B) stained with 1 mM 5-bromo-4-chloro-3-indolyl-β-d-glucuronic (X-Gluc) acid buffer under the same conditions for 80 min. (B) Root tips hydrostimulated as in (A) (C and D) or grown in a saturated water conditions (A and B) whose green fluorescent signal was visualized by confocal microscopy. Shown are images selected from at least 45 representative root tips. Bar = 29 µm.Open in a separate windowFigure 2Expression of DR5::GUS in wild type NHR1 and nhr1 backgrounds. Roots were hydrotropically stimulated for 8 days in a medium with an osmotic gradient (C and D) or grown in normal medium (A and B) and stained with X-Gluc acid buffer under the same conditions for 80 min. Shown are images selected from at least 50 representative root tips. Bar = 25 µm.Our studies⁷ revealed that ABA is a critical regulator of both root gravitropism and hydrotropism in water deficit conditions, and that the role of auxin under these conditions seems to differ from those observed in several studies thus far published on gravitropism made under well-water conditions. The molecular characterization of NHR1 and from other nhr-like mutants already isolated in our lab will clarify the mechanisms involved in this fascinating tropism.¹⁶     

Biofouling in water systems – cases,causes and countermeasures

Biofouling is referred to as the unwanted deposition and growth of biofilms. This phenomenon can occur in an extremely wide range of situations, from the colonisation of medical devices to the production of ultra-pure, drinking and process water and the fouling of ship hulls, pipelines and reservoirs. Although biofouling occurs in such different areas, it has a common cause, which is the biofilm. Biofilms are the most successful form of life on Earth and tolerate high amounts of biocides. For a sustainable anti-fouling strategy, an integrated approach is suggested which includes the analysis of the fouling situation, a selection of suitable components from the anti-fouling menu and an effective and representative monitoring of biofilm development.     

Wachstumsbeeinflussung durch Acetylcholin,Histamin, Alloxan,Nadisan, Aristamid,Nicotin-säureamid und p-Aminobenzoesäure beim Hühnerembryo

Ohne ZusammenfassungXVII. Mitteilung zu Steuerung von Wachstum und Formbildung durch Wirkstoffe der Arbeitsgemeinschaft Prof. Dr. H.Wurmbach und Mitarbeiter, Reihe C: Morphologische Untersuchungen an Vögeln.Mit Unterstützung der Deutschen Forschungsgemeinschaft, des Herrn Ministers für Wirtschaft und Verkehr des Landes Nordrhein-Westfalen und der Indonesischen Regierung.     

Phase Behavior, Stability, and Mesomorphism of Monostearin–oil–water Gels

This paper is the characterization of a new material comprised of oil, water, monostearin and stearic acid, which can be used as a heart-friendly, low-saturate, trans fatty acid-free spreadable fat and shortening. Oil–water–monstearin mixtures formed a gel above 2% monostearin and 30% water and were stable over a month’s time. An increase in the storage modulus (G′), and peak melting temperature (T _m) was observed over time, which suggests a slow change in structure to a more solid form. Powder x-ray diffraction measurements at temperatures above the Krafft temperature of the monglyceride (57°C) indicated the existence of a lamellar liquid crystalline phase $ {\left( {L_{\alpha } } \right)} This paper is the characterization of a new material comprised of oil, water, monostearin and stearic acid, which can be used as a heart-friendly, low-saturate, trans fatty acid-free spreadable fat and shortening. Oil–water–monstearin mixtures formed a gel above 2% monostearin and 30% water and were stable over a month’s time. An increase in the storage modulus (G′), and peak melting temperature (T _m) was observed over time, which suggests a slow change in structure to a more solid form. Powder x-ray diffraction measurements at temperatures above the Krafft temperature of the monglyceride (57°C) indicated the existence of a lamellar liquid crystalline phase with a (001) reflection occurring at 50 ?. In addition to the 50 ? reflection at small angles, a wide angle reflection at 4.2 ? was observed upon cooling below 60°C, indicating a transition from the to the phase, which upon storage at 22°C for one day converted to the coagel, or β-gel phase.     

Excited-state proton-transfer reactions of 7-azaindole with water,ammonia and mixed water–ammonia: microsolvated dynamics simulation

Dynamics simulations of excited-state multiple proton transfer (ESMPT) reactions in 7-azaindole (7AI) with ammonia, mixed water–ammonia, and water molecules were investigated by quantum dynamics simulations in the first-excited state using RI-ADC(2)/SVP-SV(P) in the gas phase. 7AI(WW), 7AI(WA), 7AI(AW) and 7AI(AA) clusters (W, water and A, ammonia) show very high probability of the excited-state triple proton transfer (ESTPT) occurrence in ranges from 20% for 7AI(WA) to 60% for 7AI(AW), respectively. Furthermore, 7AI(AW) clusters with ammonia placed near N–H of 7AI has the highest probability among other isomers. In 7AI with three molecules of bridged-planar of water, ammonia and mixed water–ammonia clusters, the excited-state quadruple proton transfer reactions occur ineffectively and rearrangement of hydrogen-bonded network on solvents also takes place prior to either ESTPT or excited-state double proton transfer. The role played by mixed-solvent is revealed with replacing H₂O with NH₃ in which the ESMPT is found to be more efficient corresponding to lower barrier in the excited state. The preferential number of solvent surrounding 7AI that facilitates the proton transfer process is two for methanol and water but this preferential number for ammonia is one.

Highlights: (i) replacing H₂O with NH₃ assists ESPT corresponding to lower barrier in the excited state; (ii) the ESMPT time of 7AI with mixed water–ammonia is in the sub-picosecond timescale; (iii) the PT tends to be concerted process with at least one ammonia, but synchronous without ammonia.     

Biogeochemical processes at the sediment–water interface, Bombah Broadwater, Myall Lakes

Myall Lakes has experienced algal blooms in recent years which threaten water quality. Biomarkers, benthic fluxes measured with chambers, and pore water metabolites were used to identify the nature and reactivity of organic matter (OM) in the sediments of Bombah Broadwater (BB), and the processes controlling sediment-nutrient release into the overlying waters. The OM in the sediments was principally from algal sources although terrestrial OM was found near the Myall River. Terrestrial faecal matter was identified in muddy sediments and was probably sourced via runoff from farm lands. The reactive OM which released nutrients into the overlying waters was from diatoms, dinoflagellates and probably cyanobacteria. Microcystis filaments were observed in surface sediments. OM degradation rates varied between 5.3 and 47.1 mmol m^?2 day^?1 (64–565 mg m^?2 day^?1), were highest in the muddy sediments and sulphate reduction rates accounted for 20–40% of the OM degraded. Diatoms, being heavy sink rapidly, and are an important vector to transport catchment N and P to sites of denitrification and P-trapping in the sediments. Denitrification rates (mean ～4 mmol N m^?2 day^?1), up to 7 mmol N m^?2 day^?1 (105 mg N m^?2 day^?1) were measured, and denitrification efficiencies were highest (mean = 86 ± 4%) in the sandy sediments (～20% of the area of BB), but lower in the muddy sediments (mean = 63 ± 15%). These differences probably result from higher OM loads and anaerobic respiration in muddy sediments. Most DIP (>70%) from OM degradation was not released into overlying waters but remained trapped in surface sediments. Biophysical (advective) processes were responsible for the measured metabolite (O₂, CO₂, DSi, DIN and DIP) fluxes across the sediment–water interface.     

Elektronenmikroskopische Darstellung,Längenverteilung und Konfiguration einsträngiger Desoxyribonucleinsäure im Cytochrom-c-Film

Zusammenfassung Durch Alkali nachFreifelder undDavison einsträngig gemachte DNA aus Forellengonaden wird mittels Spreitung einer DNA/Protein-Lösung elektronenmikroskopisch dargestellt. Ihre Konfiguration, gemessen durch das mittlere Quadrat der Abstände der Molekülenden als Funktion der Konturenlänge, ist flexibler als bei zweisträngiger DNA unter gleichen Bedingungen, weicht aber wie diese infolge ihres Polyelektrolytcharakters vom statistischen Knäuel merklich ab. Die exponentielle Verteilung der Konturenlängen wird als statistische Verteilung der Bruchstellen gedeutet.

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Summary Single-stranded DNA is visualized by electron microscopy after the denaturation procedure by alkali (Freifelder andDavison) and by spreading to a mixed DNA-protein film. The configuration is measured by the mean squares of end-to-end distances as a function of contour lengths. Single-stranded DNA is more flexible than double-stranded DNA under the same conditions but like native DNA differs markedly from the random coil, probably because of electrostatic interactions along the polyelectrolyte molecule. The exponential distribution of the contour lengths is explained as a random distribution of breaks in single strands similar to these of native DNA.

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Wir danken Herrn Prof. Dr. K.Herzberg für die Unterstützung dieser Arbeit, Frau C.Plescher sowie Frl. I.Hortenbach für technische Mitarbeit und der Deutschen Forschungsgemeinschaft für Beihilfen.     

Taphonomy of modern deep,cold‐temperate water coral reefs

Deep‐water corals are widely distributed along the cold‐temperate northeastern Atlantic continental margin. Despite the widespread occurrence of these aphotic coral constructions in deep shelf settings, the processes of framework formation and postmortem alterations which result in different preservational styles are still poorly known. Detailed mapping surveys on probably one of the largest Lophelia reef structures were carried out on the Sula Ridge, Mid‐Norwegian Shelf in 270 to 300 m depth. Side scan sonar records and camera surveys yield information at various scales of resolution on the reef complex which is more than 9 km long and up to 45 m high. Living Lophelia colonies effectively prevent colonization by other organisms and are successful in the rejection of passing detrital material from the soft tissue. In a healthy condition the coral is able to encrust repetitively attached organisms by selectively secreted sclerenchyme layers, thus, this defensive reaction results in the thickening of the skeleton. Early postmortem alteration in Lophelia colonies is introduced by the formation of a biofilm and Dodgella (fungi) infestation. The biofilm is associated with selective Fe‐Mn precipitation on the coral skeleton. This is the zone of intense attachment of sessile invertebrates such as serpulids, brachiopods, foraminifers and encrusting bryozoans. More advanced taphonomic stages show an increasing dominance in sponges which reduce the interskeletal framework porosity significantly. In addition, boring sponges excavate the thickly calcified Lophelia skeletons, thus leading to in situ collapsing structures on the sea floor. It is the intensity of sediment trapping biofilms and sponge colonization and the amount of imported detrital particles predominantly from the pelagial zone that control the generation of a pure coral rubble facies or the preservation of collapsed but mud‐rich detrital mounds.     

Serum-Cholesterin,ABO-Blutgruppen und Hämoglobintyp

Zusammenfassung Serum-Cholesterin, ABO-Blutgruppen (N=715), Glucose-6-PhosphatDehydrogenase (G-6-PD, Farbstoff-Reduktionstest, N=611) und der Hämoglobintyp (osmotische Resistenz und Cellulose-Acetat-Elektrophorese, N=469) wurden bei anscheinend gesunden, 20 Jahre alten Männern aus 12 Distrikten der Provinz Chiang Mai in Nordthailand bestimmt. Das Körpergewicht hatte keinen Einfluß auf die Cholesterinkonzentration. Probanden der Blutgruppe A hatten signifikant höhere Cholesterinwerte als die der Gruppen 0 und B. Gruppe B hatte höhere Werte als Gruppe 0, aber die Differenz war nur schwach signifikant. Der mittlere Cholesterinwert der Probanden mit -Thalassaemia minor war signifikant niedriger als der der Gruppen mit normalem Hämoglobin und mit -Thalassaemie oder abnormalem Hämoglobin. Zwischen den drei letzteren Gruppen bestand kein signifikanter Unterschied. Diese Befunde bestätigen für eine tropische Bevölkerung mit an Fetten armer Ernährung die Beziehung zwischen -Thalassämie (Fessas et al., 1963; Mayo et al., 1969, Griechenland) und ABO-Blutgruppen (Mayo et al., 1969; Oliver et al., 1969; Langman et al., 1969; Beckman u. Olivecrona, 1970) einerseits und der Serum-Cholesterin-Konzentration.

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Serum-cholesterol, AB0 blood-groups and haemoglobin typeGenetic influences on the serum-cholesterol level

Summary Serum-cholesterol, ABO blood-groups (N=715), glucose-6-phosphate dehydrogenase (G-6-PD, dye decolorization test, N=611) and haemoglobin type (osmotic fragility, cellulose acetate electrophoresis, N=469) were determined in apparently health, 20 years old males from 12 districts of the province of Chiang Mai in northern Thailand. Body weight and G-6-PD deficiency did not seem to influence the serum-cholesterol level. Probands with blood-group A had significantly higher cholesterol concentrations than groups 0 and B. The difference between groups 0 and B, the latter having somewhat higher levels, was only weakly significant. Cholesterol levels were significantly lower in probands with -thalassaemia minor when compared with a normal control group. The difference between the control group and the probands with -thalassaemia and abnormal haemoglobins (mainly HbE trait) was not significant. These findings confirm for a tropical rural population with a diet low in fat the association between -thalassaemia and low cholesterol concentrations previously reported from Greece (Fessas et al., 1963; Mayo et al., 1969) and the association between blood-group A and high cholesterol levels found in several European populations (Mayo et al., 1969; Oliver et al., 1969; Langman et al., 1969; Beckman and Olivecrona, 1970).

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Beurlaubt von der Universitäts-Kinderklinik Bonn.

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Eingerichtet und unterstützt von der Stiftung Volkswagenwerk.     

Beiträge zur Kronblattmorphologie. IV. Unifaziale Vorläuferspitzen an den Kronblättern einiger Crassulaceen,Passifloraceen, Balsaminaceen,Convolvulaceen und Cucurbitaceen

Zusammenfassung Unifazial ausgebildete Blattspitzen an den Kronblättern vonSedum, Echeveria, Pachyphytum, Passiflora undImpatiens und an den Zipfeln der Sympetalen Korollen vonQuamoclit, Ipomoea, Cucurbita undEcballium werden beschrieben und ihre Bedeutung für den Kronblattbau besprochen. Diese Spitzen weichen in ihrer Gestaltung nicht von der der Kelchblätter und im weiteren von der der Laubblätter ab. Da aber das Kronblatt im wesentlichen aus dem Oberblatt allein hervorgeht, kann hier kein Zweifel darüber bestehen, daß diese Kronblattspitzen nur die morphologischen Oberblattspitzen und nicht das ganze Oberblatt darstellen, was bei manchen eine unifaziale Spitze tragenden Kelchblättern der Fall ist.     

Wassersättigungsdefizit,Spaltenbewegung und Photosynthese

Zusammenfassung Wenn die Pflanze mehr Wasser verliert, als sie gleichzeitig ersetzen kann, und dadurch in Unterbilanz (Wassersättigungsdefizit) gerät, so leidet erfahrungsgemäß die Photosynthese. Der Wasserverlust kann diese unmittelbar etwa durch Entquellung des Protoplasmas beeinträchtigen oder mittelbar, indem hydroaktive Schließbewegungen der Stomata den Gaswechsel hemmen. Es fragt sich, welcher der beiden Einflüsse ausschlaggebend ist. Zur Klärung der Frage wurden von einigen mesophytischen Kraut- und Baumtypen Blatt- (Zweig-) Proben entnommen und an diesen, nachdem man sie im Dunkeln sich mit Wasser hatte sättigen lassen, bei 22° C und 10.000 bzw. 2000 Lux die Abläufe der Assimilation und Respiration (URAS), der Spaltenbewegungen (Auflichtmikroskop) und die Zunahme des Defizits (Wägung) soweit irgend möglich synchron ermittelt und verglichen. Es ergab sich, daß die Photosynthese zunächst mit der Spaltweite zunimmt und immer erst dann mehr oder weniger rasch zurückgeht, wenn die Spalten infolge des wachsenden Defizits sich mehr und mehr verengen. Mit oder kurz nach völligem hydroaktivem Schluß der Stomata (im Mikroskop erscheint er manchmal verfrüht, weil das wirkliche Schließen nicht sichtbar ist) ist der Gaswechsel so weit unterbunden, daß mur mehr die Respirations-CO₂ reassimiliert wird. Positive Nettoassimilation war dann nie mehr feststellbar. Die Photosynthese wird bei wechselnder Wasserbilanz durch das Spiel der Spalten entscheidend beherrscht, wogegen dieses die Respiration, wenn überhaupt, so jedenfalls viel weniger beeinflußt. Alles in allem reagieren demnach die Spaltapparate mindestens bei Mesophyten unter den gegebenen Bedingungen empfindlicher auf Wasserverlust als der Assimilationsapparat des Mesophylls, so daß unmittelbare Beeinträchtigung der Photosynthese durch Wasserverlust im allgemeinen wohl erst nach Spaltenschluß wirksam wird, was bei der Geringfügigkeit der kutikularen CO₂-Auf-nahme wenig Bedeutung hat. Die Möglichkeit von Ausnahmen wird er-örtert.Herrn Prof. Dr. F. Weber zum 70. Geburtstag.