Larix decidua and other larches in Europe: distribution, habitat, usage and threats

The European larch (Larix decidua Mill.) is a pioneer, very long-lived, fast-growing coniferous tree, which occurs in the central and eastern mountains of Europe, forming open forests or pasture woods at the upper tree limits. Larch is the only deciduous conifer in Europe as an adaptation to continental alpine climates. In fact, it is able to tolerate very cold temperatures during winter and, by losing its needles, avoids foliage desiccation. It is a transitional species, colonising open terrain after natural disturbances. It forms pure stands but more often it is found with other alpine tree species, which tend to replace it if no other disturbances occur. Thanks to its adaptability and the durability of its wood, the European larch represents an important silvicultural tree species in the alpine regions, planted even outside its natural ranges. Its wood is largely used for carpentry, furniture and pulp for paper. In lower altitudes or with high precipitation rates, larch is more susceptible to fungal diseases. Outbreaks of insect defoliators, principally caused by the larch bud moth (Zeiraphera diniana), can limit tree development, with economic losses in plantations, but they rarely lead to the death of the trees.

A first chironomid-based summer temperature reconstruction (13–5 ka BP) around 49°N in inland Europe compared with local lake development

Temperature reconstructions for the end of the Pleistocene and the first half of the Holocene based on biotic proxies are rare for inland Europe around 49°N. We analysed a 7 m long sequence of lake deposits in the Vihorlat Mts in eastern Slovakia (820 m a.s.l.). Chironomid head capsules were used to reconstruct mean July temperature (TJuly), other proxies (diatoms, green algae, pollen, geochemistry) were used to reconstruct local environmental changes that might have affected the climate reconstruction, such as epilimnetic total phosphorus concentrations (TP), lake level changes and development of surrounding vegetation. During the Younger Dryas (YD), temperature fluctuated between 7 and 11 °C, with distinct, decadal to centennial scale variations, that agree with other palaeoclimate records in Europe such as δ18O content in stalagmites or Greenland ice cores. The results indicate that the site was somewhat colder than expected from the general south-to-north YD temperature gradient within Europe, possibly because of north-facing exposition. The warmer phases of the YD were characterised by low water level or even complete desiccation of the lake (12,200-12,400 cal yr BP). At the Late-Glacial/Holocene transition TJuly steeply increased from from 11 to 15.5 °C (11,700-11,400 cal yr BP) - the highest TJuly for entire sequence. This rapid climate change was reflected by all proxies as a compositional change and increasing species diversity. The open woodlands of Pinus, Betula, Larix and Picea were replaced by broad-leaved temperate forests dominated by Betula, later by Ulmus and finally by Corylus (ca 9700 cal yr BP). At the same time, input of eroded coarse-grained material into the lake decreased and organic matter (LOI) and biogenic silica increased. The Early-Holocene climate was rather stable till 8700 cal yr BP, with temporary decrease in TJuly around 11,200 cal yr BP. The lake was productive with a well-developed littoral, as indicated by both diatoms and chironomids. A distinct decline of TJuly to 10 °C between 8700 and 8000 cal yr BP was associated with decreasing chironomid diversity and increasing climate moistening indicated by pollen. Tychoplanktonic and phosphorus-demanding diatoms increased which might be explained by hydrological and land-cover changes. Later, a gradual warming started after 7000 cal yr BP and representation of macrophytes, periphytic diatoms and littoral chironomids increased. Our results suggest that the Holocene thermal maximum was taking place unusually early in the Holocene at our study site, but its timing might be affected by topography and mesoclimate. We further demonstrated that temperature changes had coincided with variations in local hydrology

Physiological Responses to Environmental Variation in Intertidal Red Algae: Does Thallus Morphology Matter?

Morphological variation within and among many species of algae show correlated life history traits. The trade-offs of Life history traits among different morphs are presumed to be determined by morphology. Form-function hypotheses also predict that algae of different morphological groups exhibit different tolerances to physiological stress, whereas algae within a morphological group respond similarly to stress. We tested this hypothesis by comparing photosynthetic and respiratory responses to variation in season, light, temperature, desiccation and freezing among the morphologically similar fronds of Chondrus crispus and Mastocarpus stellatus and the alternate stage crust of M. stellatus. Physiological differences between fronds of the 2 species and crusts and fronds were consistent with their patterns of distribution and abundance in the intertidal zone. However, there was no clear relationship between algal morphology and physiological response to environmental variation. These results suggest that among macroalgae the correlation between Life history traits and morphology is not always causal. Rather, the link between life history traits and morphology is constrained by the extent to which physiological characteristics codetermine these features.

(Table 1) Characteristics of Klebsormidium (filamentous green algae) strains from the Antarctic, Arctic and Slovakia

The freezing and desiccation tolerance of 12 Klebsormidium strains, isolated from various habitats (aero-terrestrial, terrestrial, and hydro-terrestrial) from distinct geographical regions (Antarctic - South Shetlands, King George Island, Arctic - Ellesmere Island, Svalbard, Central Europe - Slovakia) were studied. Each strain was exposed to several freezing (-4°C, -40°C, -196°C) and desiccation (+4°C and +20°C) regimes, simulating both natural and semi-natural freeze-thaw and desiccation cycles. The level of resistance (or the survival capacity) was evaluated by chlorophyll a content, viability, and chlorophyll fluorescence evaluations. No statistical differences (Kruskal-Wallis tests) between strains originating from different regions were observed. All strains tested were highly resistant to both freezing and desiccation injuries. Freezing down to -196°C was the most harmful regime for all studied strains. Freezing at -4°C did not influence the survival of studied strains. Further, freezing down to -40°C (at a speed of 4°C/min) was not fatal for most of the strains. RDA analysis showed that certain Antarctic and Arctic strains did not survive desiccation at +4°C; however, freezing at -40°C, as well as desiccation at +20 °C was not fatal to them. On the other hand, other strains from the Antarctic, the Arctic, and Central Europe (Slovakia) survived desiccation at temperatures of +4°C, and freezing down to -40°C. It appears that species of Klebsormidium which occupy an environment where both seasonal and diurnal variations of water availability prevail, are well adapted to freezing and desiccation injuries. Freezing and desiccation tolerance is not species-specific nor is the resilience only found in polar strains as it is also a feature of temperate strains.

Macroinvertebrate abundance and proportion of trait categories in river biotopes across England and Wales

There is a long tradition of river monitoring using macroinvertebrate communities to assess environmental quality in Europe. A promising alternative is the use of species life-history traits. Both methods, however, have relied on the time-consuming identification of taxa. River biotopes, 1-100 m**2 'habitats' with associated species assemblages, have long been seen as a useful and meaningful way of linking the ecology of macroinvertebrates and river hydro-morphology and can be used to assess hydro-morphological degradation in rivers. Taxonomic differences, however, between different rivers had prevented a general test of this concept until now. The species trait approach may overcome this obstacle across broad geographical areas, using biotopes as the hydro-morphological units which have characteristic species trait assemblages. We collected macroinvertebrate data from 512 discrete patches, comprising 13 river biotopes, from seven rivers in England and Wales. The aim was to test whether river biotopes were better predictors of macroinvertebrate trait profiles than taxonomic composition (genera, families, orders) in rivers, independently of the phylogenetic effects and catchment scale characteristics (i.e. hydrology, geography and land cover). We also tested whether species richness and diversity were better related to biotopes than to rivers. River biotopes explained 40% of the variance in macroinvertebrate trait profiles across the rivers, largely independently of catchment characteristics. There was a strong phylogenetic signature, however. River biotopes were about 50% better at predicting macroinvertebrate trait profiles than taxonomic composition across rivers, no matter which taxonomic resolution was used. River biotopes were better than river identity at explaining the variability in taxonomic richness and diversity (40% and <=10%, respectively). Detailed trait-biotope associations agreed with independent a priori predictions relating trait categories to near river bed flows. Hence, species traits provided a much needed mechanistic understanding and predictive ability across a broad geographical area. We show that integration of the multiple biological trait approach with river biotopes at the interface between ecology and hydro-morphology provides a wealth of new information and potential applications for river science and management.

(Table 2) Stratigraphic position of midpoints of reddish and beige layers of lithologic cycles in the Loulja-A Section and their astronomical ages after tuning to the ETP and Summer Insolation Curves of the La2004 solution

An integrated high-resolution stratigraphy and orbital tuning is presented for the Loulja sections located in the Bou Regreg area on the Atlantic side of Morocco. The sections constitute the upward continuation of the upper Messinian Ain el Beida section and contain a well-exposed, continuous record of the interval straddling the Miocene-Pliocene (M-P) boundary. The older Loulja-A section, which covers the interval from ~5.59 to 5.12 Ma, reveals a dominantly precession-controlled color cyclicity that allows for a straightforward orbital tuning of the boundary interval and for detailed cyclostratigraphic correlations to the Mediterranean; the high-resolution and high-quality benthic isotope record allows us to trace the dominantly obliquity-controlled glacial history. Our results reveal that the M-P boundary coincides with a minor, partly precession-related shift to lighter "interglacial" values in d18O. This shift and hence the M-P boundary may not correlate with isotope stage TG5, as previously thought, but with an extra (weak) obliquity-controlled cycle between TG7 and TG5. Consequently, the M-P boundary and basal Pliocene flooding of the Mediterranean following the Messinian salinity crisis are not associated with a major deglaciation and glacio-eustatic sea level rise, indicating that other factors, such as tectonics, must have played a fundamental role. On the other hand, the onset of the Upper Evaporites in the Mediterranean marked by hyposaline conditions coincides with the major deglaciation step between marine isotope stage TG12 and TG11, suggesting that the associated sea level rise is at least partly responsible for the apparent onset of intermittently restricted marine conditions following the main desiccation phase. Finally, the Loulja-A section would represent an excellent auxiliary boundary stratotype for the M-P boundary as formally defined at the base of the Trubi marls in the Eraclea Minoa section on Sicily.

Age-depth relation, radiocarbon ages and tephra geochemistry of core 5022-2CP from Laguna Potrok Aike, southern Patagonia

The 106 m long composite profile from site 2 of ICDP expedition 5022 (PASADO) at Laguna Potrok Aike documents a distinct change in sedimentation patterns from pelagic sediments at the top to dominating mass movement deposits at its base. The main lithological units correspond to the Holocene, to the Lateglacial and to the last glacial period and can be interpreted as the result of distinct environmental variations. Overflow conditions might have been achieved during the last glacial period, while signs of desiccation are absent in the studied sediment record. Altogether, 58 radiocarbon dates were used to establish a consistent age-depth model by applying the mixed-effect regression procedure which results in a basal age of 51.2 cal. ka BP. Radiocarbon dates show a considerable increase in scatter with depth which is related to the high amount of reworking. Validation of the obtained chronology was achieved with geomagnetic relative paleointensity data and tephra correlation.

Age model of ODP Hole 107-654A

It has long been speculated that glacio-eustatic sea level drop may have caused or contributed to the isolation and consequent desiccation of the Mediterranean in the late Miocene (the 'Messinian salinity crisis'). Ocean Drilling Program site 654 on the Sardinia margin of the Tyrrhenian Sea is the first deep-sea drill site to penetrate through upper Messinian evaporites into lower Messinian/upper Tortonian open marine sediments, and thus offers a unique opportunity to date the onset of the salinity crisis. A reexamination of the magnetostratigraphic, biostratigraphic, and stable isotope-stratigraphic constraints on the preevaporite sediments of site 654 has yielded two possible ages for the contact between salinity crisis sediments and the underlying normal marine sediments. One magnetostratigraphic interpretation plus the biostratigraphically determined position of the Tortonian/Messinian boundary imply a date of about 6.2 Ma for the youngest presalinity crisis sediments. An alternative magnetostratigraphic interpretation plus the carbon isotope stratigraphy imply a date of about 5.2 Ma. The younger of these dates coincides with a delta18O spike in open ocean sediments [Keigwin, 1987 doi:10.1029/PA002i006p00639], which is attributed to increased ice volume.

Pliocene stable oxygen and carbon isotope record of benthic foraminifera from ODP Site 138-846 in the eastern equatorial Pacific

Oxygen and carbon isotope ratios were measured in benthic foraminifers from the entire Pliocene and latest Miocene sections of Site 846, a 180-m section, at a sampling interval of 10 cm. This provides a temporal resolution of about 2500 yr. The documented continuity of the record is excellent. Using the time scale that was developed on the basis of orbital tuning of GRAPE density records, we observed a fairly constant phase relationship between delta18O and variations in the obliquity of Earth's rotational axis. A new numbering scheme for Pliocene isotope stages is proposed. This high-resolution delta18O record clarifies several interesting aspects of late Neogene climatic evolution, including a "glacial" event that may have caused the final Messinian desiccation of the Mediterranean Sea; one or more "interglacial" events that might have caused refilling of the Mediterranean; a well-resolved couplet of glacial events at about the age of the Sidujfall Subchron; interglacial extremes in the early part of the Gauss that could have resulted from either significant deglaciation on Antarctica or from warming of deep water; and a gradual ramp of increasingly extreme "glacial" events, starting at about the Kaena Subchron and culminating with delta18O stage 100 in the earliest Matuyama.

Composition of Messinian sediments from the Tyrrhenian Sea

The data base for this study is represented by essentially nonevaporitic Messinian sediments recovered at ODP Sites 654, 653, 652, and 656 along the eastern Sardinian margin, and of the overlying early Pliocene oozes. Grain-size distribution, carbonate content, and microscopic observation of the sand size fractions were investigated. Messinian paleoenvironments, documented in the western Tyrrhenian Sea (ODP Sites 654 and 653), provide additional evidence supporting the deep basin desiccation model. A sharp lithologic contrast between early Pliocene pelagic oozes and latest Messinian conformable gypsiferous silts supports this model. The "lago-mare" biofacies was only occasionally observed in the shallowest site and is limited to the topmost part of the Messinian. Sites 652 and 656, lying in the deeper part of the Tyrrhenian and located on the downthrown side of an important eastward dipping fault system known as "Faglia centrale" are characterized by terrigenous sedimentation, with partly recycled minor evaporites. Of special interest is Site 652, where the thickness of the (probable) Messinian is 530 m. Sedimentary characters indicate a permanently subaqueous but nonmarine environment, with turbidites accumulating in a rapidly subsiding basin. According to the model proposed, this basin was fed by continental waters during times of maximum evaporitic draw-down, with temporary marine incursions from the west or southwest when the water level was higher. A basement ridge separated the evaporating pond from this endoreic lake located on the opposite (eastern) margin of the Tyrrhenian Basin, which was then limited to its western part. Post-Messinian reactivation of the "Faglia centrale" is necessary to account for the inversion of the relief.

Boron contents and boron, carbon, and oxygen isotope data for ODP Sites 160-970 and 160-971

Products of two mud volcanoes from the distal part of the Mediterranean Ridge accretionary complex have been investigated regarding their B, C, and O stable isotope signatures. The mud breccias have been divided into mud matrix, lithified clasts, biogenic deposits, and authigenic cements and crusts related to fluid flow and cementation. Isotope geochemistry is used to evaluate the depth of mobilization of each phase in the subduction zone. B contents and isotope ratios of the mud and mud clasts show a general trend of B enrichment and decreasing d11B values with increasing consolidation (i.e., depth). However, the majority of the clast and matrix samples relate to moderate depths of mobilization within the wedge (1-2 km below seafloor). The carbonate cements of most of these clasts as well as the authigenic crusts, however, provide evidence for a deep fluid influence, probably associated with the décollement at 5-6 km depth. This interpretation is supported by d13C ratios of the crust, which indicate precipitation of C from thermogenic methane, and by the d11B ratios of pore-water samples of mud-breccia drill cores. Clams (Vesicomya sp.) living adjacent to fluid vents have d11B and d18O values corresponding to brines known in the area, which acted as the parent solution for shell precipitation. Such brines are most likely Miocene pore waters trapped at deep levels within the backstop to the accretionary prism, probably prior to desiccation of the Mediterranean in the Messinian (6-5 Ma). Combining all results, deep fluid circulation and expulsion are identified as the main processes triggering mud liquefaction and extrusion, whereas brines contribute only locally. Given the high B contents, mud extrusion has to be considered a major backflux mechanism of B into the hydrosphere.

(Table 1) Chemical composition of Mediterranean halite from DSDP Hole 13-134

Bromine content of a 15 cm halite core from Deep Sea Drilling Project Leg XIII Hole 134 was analyzed at 1.5 cm intervals. The Br varies from 140 to 254 ppm, and three maxima were found to coincide with three postulated horizons of desiccation. The Br profile confirms the interpretation from sedimentologic evidence that Mediterranean salts were deposited in a desiccating basin.

Leftovers in seed dispersal: ecological implications of partial seed consumption for oak regeneration

1. Successful seed dispersal by animals is assumed to occur when undamaged seeds arrive at a favourable microsite. Most seed removal and dispersal studies consider only two possible seed fates, predation or escape intact. Whether partial consumption of seeds has ecological implications for natural regeneration is unclear. We studied partial consumption of seeds in a rodent-dispersed oak species. 2. Fifteen percent of dispersed acorns were found partially eaten in a field experiment. Most damage affected only the basal portion of the seeds, resulting in no embryo damage. Partially eaten acorns had no differences in dispersal distance compared to intact acorns but were recovered at farther distances than completely consumed acorns. 3. Partially eaten acorns were found under shrub cover unlike intact acorns that were mostly dispersed to open microhabitats. 4. Partially eaten acorns were not found buried proportionally more often than intact acorns, leading to desiccation and exposure to biotic agents (predators, bacteria and fungi). However, partial consumption caused more rapid germination, which enables the acorns to tolerate the negative effects of exposure. 5. Re-caching and shrub cover as microhabitat of destination promote partial seed consumption. Larger acorns escaped predation more often and had higher uneaten cotyledon mass. Satiation at seed level is the most plausible explanation for partial consumption. 6. Partial consumption caused no differences in root biomass when acorns experienced only small cotyledon loss. However, root biomass was lower when acorns experienced heavy loss of tissue but, surprisingly, they produced longer roots, which allow the seeds to gain access sooner to deeper resources. 7.Synthesis. Partial consumption of acorns is an important event in the oak regeneration process, both quantitatively and qualitatively. Most acorns were damaged non-lethally, without decreasing both dispersal distances and the probability of successful establishment. Faster germination and production of longer roots allow partially eaten seeds to tolerate better the exposure disadvantages caused by the removal of the pericarp and the non-buried deposition. Consequently, partially consumed seeds can contribute significantly to natural regeneration and must be considered in future seed dispersal studies.

Caracterización molecular del mutante riso 1508 de cebada : modificaciones transcripcionales y posttranscripcionales en el desarrollo de la semilla

La semilla es el principal órgano reproductivo de las plantas espermatofitas, permitiendo la dispersión de las poblaciones y asegurando su supervivencia gracias a su tolerancia a la desecación y a su capacidad para germinar bajo condiciones ambientales óptimas. El rendimiento y valor económico de los cereales, que constituyen la primera cosecha mundial, depende, en buena medida, de la eficacia con que se acumulan en la semilla sustancias de reserva: proteínas, carbohidratos y lípidos. El principal carbohidrato acumulado en la semilla de cebada es el almidón y la fracción mayoritaria de proteínas es la de las prolaminas (solubles en etanol al 70%); estas proteínas tienen muy bajo contenido en lisina, un aminoácido esencial en la dieta de animales monogástricos. Con el fin de mejorar el valor nutricional de la semilla de cebada, se han obtenido diferentes mutantes con un mayor contenido en este aminoácido. Riso 1508 es un mutante de cebada rico en lisina cuya mutación lys3a, de efectos pleiotrópicos, segrega como un único gen mendeliano. Entre otros, presenta una reducción drástica de la expresión de algunos genes que codifican proteínas de reserva de tipo prolamina, en concreto, presenta reducida la expresión de los genes que codifican B-, C- y ϒ-Hordeínas y del inhibidor de tripsina CMe, pero no tiene alterada la expresión del gen que codifica las D-Hordeínas. Este último gen carece en su promotor del motivo GLM (5’‐(G/A)TGA(G/C)TCA(T/C)‐3’), que es reconocido por factores transcripcionales bZIP. En este trabajo, el mutante de cebada Riso 1508 se ha utilizado como herramienta para profundizar en el conocimiento de la regulación génica en semillas durante las fases de la maduración y la germinación. Para ello, en una primera aproximación, se llevó a cabo un análisis transcriptómico comparando el genotipo mutante con el silvestre durante la maduración de la semilla. Además de confirmar variaciones en los genes que codifican proteínas de reserva, este análisis indicó que también estaban afectados los genes relacionados con metabolismo de carbohidratos. Por ello se decidió caracterizar la familia multigénica de sacarosas sintasa (SUSy) en cebada. Se anotaron dos nuevos genes, HvSs3 y HvSs4, cuya expresión se comparó con la de los genes HvSs1 y HvSs2, previamente descritos en el laboratorio. La expresión de los cuatro genes en tejidos diferentes y su respuesta a estreses abióticos se analizó mediante RT-qPCR. HvSs1 y HvSs2 se expresaron preferencialmente durante el desarrollo del endospermo, y HvSs1 también fue un tránscrito abundante durante la germinación. HvSs1 se indujo en hojas en condiciones de anoxia y HvSs3 por estrés hídrico, y ambos genes se indujeron por tratamientos de frío. La localización subcelular de las cuatro isoformas no fue sólo citoplásmica, sino que también se localizaron en zonas próximas a retículo endoplásmico y en la cara interna de la membrana plasmática; además, se observó una co-localización de HvSS1 con el marcador de mitocondrias. Estos datos sugieren un papel distinto aunque parcialmente solapante de las cuatro Sacarosa Sintasas de cebada, descritas hasta la fecha. Las cinéticas de expresión de los genes que codifican los TFs más importantes implicados en la regulación génica durante el desarrollo del endospermo de cebada, se analizaron por RT-qPCR en ambos genotipos, demostrando que los TFs de la clase DOF aparecieron desregulados durante todo el proceso en Riso 1508 comparado con el cv. Bomi, aunque también se observaron diferencias significativas en algunos de los que codifican bZIPs. Estudios previos indicaban que el ortólogo de BLZ2 en maíz, O2, se regula post-traduccionalmente mediante un mecanismo de fosforilación/defosforilación reversible, y que la forma defosforilada es la fisiológicamente activa. En este trabajo se demostró que BLZ2 está sujeto a este tipo de regulación y que la proteín-fosfatasa HvPP2C2 está implicada en el proceso. La interacción de HvPP2C2 y BLZ2 tiene lugar en el núcleo celular únicamente en presencia de 100 μM ABA. En el mutante Riso 1508, BLZ2 se encuentra en un estado hiperfosforilado tanto durante la maduración como durante la germinación de la semilla, lo que dificultaría la unión de BLZ2 a las secuencias GLM en los promotores de los genes que codifican B-, C-,y ϒ- Hordeínas y CMe. Summary The seed is the main reproductive organ of spermatophyte plants allowing the spread of populations and ensuring their survival through its desiccation tolerance and because of their ability to germinate under optimum environmental conditions. Yield and economic value of cereal crops, that constitute the first world crop, depend largely on the efficiency with which they accumulate in the seed reserve substances: proteins, carbohydrates and lipids. The main carbohydrate accumulated in the barley seed is starch and the major protein fraction is that of prolamins (soluble in 70% ethanol); these proteins have a very low lysine content, an essential amino-acid for the diet of monogastric animals. In order to improve the nutritional value of the barley seed, different mutants have been obtained with a higher content of this amino-acid. Riso 1508 is one lysine-rich mutant whose mutation (lys3a) segregates as a single Mendelian gene with pleiotropic effects, such as a drastic reduction of genes encoding the trypsin inhibitor CMe and the B-, C-and ϒ-hordeins, but has not altered the expression of the gene encoding the D-hordeins. This latter gene lacks in its promotor the GLM motif (5’‐(G/A)TGA(G/C)TCA(T/C)‐3’), that is recognised by bZIP transcription factors In this work we have used the barley mutant Riso 1508 as a tool for better understanding gene regulation in seeds during the maturation and germination phases. To this aim, a transcriptomic analysis was performed comparing wild and mutant genotypes during seed maturation. Besides confirming variations in the expression of genes encoding reserve proteins, this analysis indicated that some genes related with carbohydrate metabolism were also affected. It was therefore decided to characterize the multigene family of sucrose synthases (SUSy) in barley. Two new genes were annotated, HvSs3 and HvSs4, and its expression was compared with that of genes HvSs1 and HvSs2, previously described in our laboratory. The expression of the four genes in different tissues and in response to abiotic stresses was analyzed by RTqPCR. HvSs1 and HvSs2 were preferentially expressed during the development of the endosperm, and the HvSs1 transcript was also abundant upon germination. HvSs1 was induced in leaves by anoxic conditions, HvSs3 by water stress, and both genes were induced by cold treatments. The subcellular localization of all four isoforms was not only cytoplasmic, but they could be found along the endoplasmic reticulum and at the inner side of the cell membrane; HvSS1, was also associated with the mitochondrial marker. These data suggest a distinct but partially overlapping roles for the barley sucrose synthases, described so far. The expression kinetics of the genes encoding the most important TFs involved in gene regulation during barley endosperm development was analyzed by RT-qPCR in both genotypes. These data show that the genes encoding DOF TFs were mis-regulated throughout the process in Riso 1508, although significant differences were also found among some of those encoding bZIPs. Previous studies indicated that the BLZ2 orthologue in maize, O2, was post-translationally regulated by reversible phosphorylation/dephosphorylation and that the dephosphorylated protein is the physiologically active form. In this work we demostrate that BLZ2 is under a similar regulation and that the proteinphosphatase HvPP2C2 is implicated in the process. The interaction between HvPP2C2 and BLZ2 takes place in the cell nucleus only in the presence of 100 μM ABA. In the Riso 1508 mutant, BLZ2 is found in a hyperphosphorylated state in the maturation phase and upon seed germination; because of this, the BLZ2 binding to the GLM promoter sequences of genes encoding B-, C- y ϒ- Hordeins and CMe would be decreased in the mutant.

Estudio de la estabilidad genética asociada a los procesos de crioconservación de ápices de menta

La crioconservación se ha descrito como una técnica de conservación ex situ a largo plazo que ha sido aplicada con éxito a numerosas especies, y resulta especialmente importante en aquellas con propagación vegetativa, infértiles o amenazadas, en las que sistemas de conservación ex situ más sencillos, como los bancos de semillas, no son posibles. También presenta ventajas frente a la conservación in vitro, ya que logra disminuir o eliminar problemas como la excesiva manipulación del material, evitando los subcultivos periódicos y disminuyendo así el riesgo de contaminaciones y de aparición de variación somaclonal. Sin embargo, someter al material vegetal a los procedimientos que implica la crioconservación provoca distintos estreses. Entre ellos, el estrés oxidativo puede potencialmente producir daños en membranas, proteínas, carbohidratos y en el ADN. En este trabajo se han evaluado diversos sistemas de crioconservación en ápices de Mentha × piperita L., híbrido estéril entre Mentha aquatica L. y Mentha spicata L. Se han utilizado ápices de dos genotipos (‘MEN 186’y ‘MEN 198’) en los cuales se compararon dos técnicas de crioconservación, encapsulación-deshidratación y vitrificación-droplet. El análisis de la supervivencia y capacidad de regeneración del material sometido a los tratamientos de crioconservación, junto con el análisis de la estabilidad genética de dicho material mediante marcadores moleculares (RAPD y AFLP) han permitido comparar los distintos protocolos y tratamientos establecidos. El estudio sobre el tipo de protocolo empleado reveló una mayor variabilidad genética en la técnica de encapsulación-deshidratación, especialmente en el genotipo ‘MEN 186’, ya que ‘MEN 198’ resultó ser más estable en todos los análisis. La inestabilidad encontrada en esta técnica no fue exclusiva de aquellos explantos crioconservados, sino que los pasos previos a la inmersión en nitrógeno líquido (NL) también provocaron variaciones en el ADN. Según el tipo de muestra analizada se encontraron diferencias en la estabilidad: muestras provenientes de callos presentaron una mayor inestabilidad que aquellas de hojas (brotes). Se utilizaron tres medios para la recuperación de los ápices tras la crioconservación con el uso de diferentes combinaciones de reguladores de crecimiento: “Reed” (0,5 mgL-1 6-bencilaminopurina, BAP), “Senula” (0,5 mgL-1 6-dimetilalilamino-purina, 2-iP + 0,1 mgL-1 ácido α-naftalen-acético, ANA) y “Nudos” (0,5 mgL-1 BAP + 0,1 mgL-1ANA). El medio “Reed” produjo un aumento en la supervivencia y recuperación de los ápices en ambos genotipos y técnicas, y disminuyó la formación de callo. Sin embargo, no tuvo un efecto significativo en la estabilidad genética. El medio “Senula” provocó una mayor estabilidad genética en el genotipo más inestable, ‘MEN 186’. Para reducir el daño oxidativo producido durante la encapsulación-deshidratación, e incrementar la recuperación de los ápices manteniendo su estabilidad genética, se comparó el efecto de añadir sustancias antioxidantes en el precultivo de los ápices (ácido ascórbico, vitamina E y glutatión). No se obtuvo la respuesta esperada y estos tratamientos no presentaron efectos significativos tanto en la estabilidad como en la recuperación. Para entender mejor qué sucede durante todo el proceso de encapsulación-deshidratación, se evaluó cada paso del protocolo por separado y su efecto en la estabilidad y la recuperación. Además, se determinó el estado de oxidación en cada etapa mediante la cuantificación de malondialdehído y la detección de la formación de radicales libres (mediante el ensayo del ácido tiobarbitúrico, y sondas fluorescentes específicas, respectivamente). Se determinó que a partir de los primeros pasos se genera estrés oxidativo, el cual aumenta a medida que se avanza por el protocolo hasta la inmersión en nitrógeno líquido. Esto se ve reflejado en la disminución progresiva tanto de la recuperación como de la estabilidad genética. Con el uso de antioxidantes en el precultivo (ácido ascórbico y vitamina E) no se obtuvo un efecto positivo en el mantenimiento de la estabilidad genética, y tan sólo con el uso de vitamina E se observó una recuperación mayor en uno de los pasos estudiados (después de la desecación). Sin embargo, cuando se utilizó ácido ascórbico durante el precultivo o la deshidratación osmótica se consiguió disminuir de forma significativa la formación de MDA y la acumulación del radical superóxido (O2•-) en la mayoría los pasos analizados, aunque esta reducción no parece tener un efecto directo en la estabilidad genética del material recuperado. ABSTRACT Cryopreservation has been described as an effective technique for the long term of ex situ conservation that has been successfully applied to numerous species, and is of especial relevance for those with vegetative propagation, infertile or endangered, in which simpler systems of ex situ conservation, such as seed banking, are not feasible. It also has advantages over in vitro conservation, as it reduces or eliminates excessive material handling, avoids periodic subcultures and thus limits the risk of contamination and the appearance of somaclonal variation. However, plant material is subjected to different treatments involved in the cryopreservation procedures, which impose several stresses. Among them, oxidative stress can potentially cause damage to membranes, proteins, carbohydrates and DNA. In this work, two cryopreservation techniques have been evaluated in Mentha × piperita L. shoot tips, sterile hybrid between Mentha aquatica L. and Mentha spicata L. Two genotypes ('MEN 186' and 'MEN 198') were used to compare two techniques: encapsulation-dehydration and droplet-vitrification. The analysis of survival and recovery capacity of the material after the cryopreservation treatments, and the analysis of the genetic stability by molecular markers (RAPD and AFLP) have enabled the comparison between protocols and treatments. The study of the two cryopreservation procedures revealed a higher genetic variability in the encapsulation-dehydration technique, especially in genotype 'MEN 186', as 'MEN 198' was more stable in all analyses. The instability generated in this technique was not exclusive of cryopreserved explants, pretreatments prior to immersion in NL also caused DNA variations. The type of sampled plant material revealed also differences in the stability: callus samples showed greater instability than shoots. Three different culture media were used for the recovery of shoot tips after cryopreservation, using different combinations of growth regulators: "Reed" (0.5 mgL-1 6-benzylaminopurine, BAP), "Senula" (0.5 mgL-1 6-dimetilalilamino-purine, 2-iP + 0.1 mgL-1 α-naphthalene acetic acid, ANA) and "Nodes" (0.5 mgL-1 BAP + 0.1 mgL-1 ANA). "Reed" medium increased survival and recovery of shoot tips in both genotypes and techniques and decreased callus formation. However, it didn`t have a significant effect on genetic stability. "Senula" medium caused a higher genetic stability in the most unstable genotype, 'MEN 186'. To reduce oxidative damage during encapsulation-dehydration, and increase shoot tip recovery and maintain genetic stability, the effect of added antioxidants (ascorbic acid, vitamin E and glutathione) in the shoot tip preculture medium was studied. These treatments had no significant effect on both stability and recovery. To better understand the events during the encapsulation-dehydration process, the effect of each step of the protocol on stability and recovery was evaluated separately. Moreover, the oxidation level was determined by quantifying malondialdehyde (MDA) formation and detecting free radical accumulation (using the thiobarbituric acid assay, and specific fluorescent probes, respectively). The oxidative stress was detected from the first steps and increased throughout the protocol until the immersion in liquid nitrogen. This was also reflected in the gradual decline of recovery and genetic stability. The use of antioxidants (ascorbic acid and vitamin E) in the shoot tip preculture medium had no effect in maintaining genetic stability; only vitamin E increased recovery in one of the steps studied (after desiccation). However, when ascorbic acid was used during the preculture or during the osmotic dehydration, a significantly decrease was observed in MDA formation and superoxide radical accumulation in most of the steps analyzed, although this reduction did not seem to have a direct effect on the genetic stability of recovered material.