CEAZA
Induced twining in Ipomoea purpurea (L.) Roth.: response threshold and induction by volatiles and snail damage.
Atala, C., Quilodrán, M., & Molina-montenegro, M.
Twining in some Convolvulaceae can be induced by leaf damage and jasmonic acid application. This induced response is believed to reduce the likelihood of future leaf damage and it is limited by drought. This response has been detected in the Convolvulaceae family using artificial damage. The mechanisms and ecological implications of this response are still unknown. In this study was tested if the induced twining requires a threshold level and if it is induced by volatiles and/or by snail damage. Three separated greenhouse experiments were conducted in order to test the induced twining in Ipomoea purpurea (Convolvulaceae) by applying different levels of artificial damage (0, 1, 5, 10 perforations to the leaves), volatiles (ground leaves) and natural damage by snails. Plants receiving the two higher damage levels twined faster than the individuals exposed to the two lower damage levels. Plants exposed to grounded leaves (volatiles) twined faster than control plants. Finally, twining was induced by snail damage more than in undamaged plants. Most growth traits did not change in any treatment. Twining in I. pupurea can be induced by artificial or natural damage, and also by volatiles emitted by damaged leaves of neighbor plants, making the induced twining an ecologically relevant response.
Año: 2014
Palabras claves: Induced twining, Ipomoea purpurea, Convolvulaceae, induced responses, herbivory.
Referencia APA: Atala, C., Quilodrán, M., & Molina-montenegro, M. (2014). Induced twining in Ipomoea purpurea (L.) Roth.: response threshold and induction by volatiles and snail damage. Gayana Bot., 71(2), 181-187.
Hydrologic landscape classification assesses streamflow vulnerability to climate change in Oregon, USA.
Leibowitz, S., Comeleo, R., Wigington, P., Weaver, C., Morefield, P., Sproles, E., & Ebersole, J.
Classification can allow for evaluations of the hydrologic functions of landscapes and their responses to stressors. Here we demonstrate the use of a hydrologic landscape (HL) approach to evaluate vulnerability to potential future climate change at statewide and basin scales in the state of Oregon. The HL classification has five components: climate, seasonality, aquifer permeability, terrain, and soil permeability. We evaluate changes when the 1971–2000 HL climate indices are recalculated using 2041–2070 simulation results from the ECHAM (European Centre HAMburg) and PCM (Parallel Climate Model) climate models with the A2, A1b, and B1 emission scenarios. Changes in climate class were modest (4–18%) statewide. However, there were major changes in seasonality class for five of the six realizations (excluding PCM_B1): Oregon shifts from being 13% snow-dominated to 4–6% snow-dominated under these five realizations, representing a 56–68% reduction in snowmelt-dominated area. At the basin scale, simulated changes for the Siletz Basin, in Oregon's Coast Range, include a small switch from very wet to wet climate, with no change in seasonality. However, there is a modest increase in fall and winter water due to increased precipitation. For the Sandy Basin, on the western slope of the Cascades, HL climate class does not change, but there are major changes in seasonality, especially for areas with low aquifer permeability, which experiences a 100% loss of spring seasonality. This would reduce summer baseflow, but effects could potentially be mitigated by streamflow buffering effects provided by groundwater in the high aquifer permeability portions of the upper Sandy. The Middle Fork John Day Basin (MFJD), in northeastern Oregon, is snowmelt-dominated. The basin experiences a net loss of wet and moist climate area, along with an increase in dry climate area. The MFJD also experiences major shifts from spring to winter seasonality, representing a 20–60% reduction in snowmelt-dominated area. Altered seasonality and/or magnitude of seasonal streamflows could potentially affect survival, growth and reproduction of salmonids in these watersheds, with the greatest effects projected for the MFJD. A major strength of the HL approach is that results can be applied to similarly classified, ungaged basins. Information resulting from such evaluations can help inform management responses to climate change at regional and basin scales without requiring detailed modeling efforts.
Año: 2014
Palabras claves:
Referencia APA: Leibowitz, S., Comeleo, R., Wigington, P., Weaver, C., Morefield, P., Sproles, E., & Ebersole, J. (2014). Hydrologic landscape classification evaluates streamflow vulnerability to climate change in Oregon, USA. Hydrology and Earth System Sciences, 18(9), 3367-3392.
Assessing the importance of human activities for the establishment of the invasive Poa annua in Antarctica.
Molina-Montenegro, M., Carrasco-Urra, F., Acuña-Rodríguez, I., Oses, R., Torres-Díaz, C., & Chwedorzewska, K.
Because of its harsh environmental conditions and remoteness, Antarctica is often considered to be at low risk of plant invasion. However, an increasing number of reports have shown the presence and spread of non-native plants in Antarctica; it is therefore important to study which factors control the invasion process in this ecosystem. Here, we assessed the role of different human activities on the presence and abundance of the invasive Poa annua. In addition, we performed a reciprocal transplant experiment in the field, and a manipulative experiment of germination with P. annua and the natives Colobanthus quitensis and Deschampsia antarctica, in order to unravel the effects of physical soil disturbance on the establishment and survival of P. annua. We found a positive correlation between abundance of P. annua and level of soil disturbance, and that survival of P. annua was 33% higher in sites with disturbed soil than non-disturbed. Finally, we found that disturbance conditions increased germination for P. annua, whereas for native species germination in experimentally disturbed soil was either unchanged or reduced compared to undisturbed soil. Our results indicate that human activities that modify abiotic soil characteristics could play an important role in the abundance of this invasive species. If the current patterns of human activities are maintained in Antarctica, the establishment success and spread of P. annua could increase, negatively affecting native flora.
Año: 2014
Palabras claves: Alien species; Colobanthus quitensis; Deschampsia antarctica; human disturbance; Poa annua; tourists.
Referencia APA: Molina-Montenegro, M., Carrasco-Urra, F., Acuña-Rodríguez, I., Oses, R., Torres-Díaz, C., & Chwedorzewska, K. (2014). Assessing the importance of human activities for the establishment of the invasive Poa annua in Antarctica. Polar Research, 33(0).
Differential susceptibility to the Withering Syndrome agent and renal coccidia in juvenile Haliotis rufescens, Haliotis discus hannai and the interspecific hybrid.
González, R., Lohrmann, K., Pizarro, J., & Brokordt, K.
Withering Syndrome (WS) is a pathogenic chronic disease caused by the intracellular rickettsial-like bacterium “Candidatus Xenohaliotis californiensis” (WS-RLOs), which affects many abalone species. The renal coccidium (Margolisiella haliotis) has often been observed concurrent with WS infection. The red abalone Haliotis rufescens is a very susceptible species to WS and is also infected by the coccidium M. haliotis. In contrast, the Japanese abalone Haliotis discus hannai is not infected by these parasites. Interspecific hybridization is a method for improving important traits in animal husbandry. The objective of this study was to determine susceptibility to WS-RLO and M. haliotis infection in the hybrid generated from a cross between red and Japanese abalones. Juveniles from both species and the interspecific hybrid were challenged by exposure to effluent from red abalone adults infected with both parasites. The animals were analyzed by histology at 130 days post-challenge. A 33% prevalence WS-RLOs was observed in the red abalone H. rufescens, whereas a 20% prevalence was observed in the hybrid. Infections were graded on a scale of 0–3. Of these red abalones infected, 53% presented grade 1 infection intensity, 10% had grade 2 infections, and 50% had grade 3 infections. However, the hybrids only presented intensities at the extremes of the scale; of those infected 33% showed grade 1 infections and 66% had grade 3 infections. The coccidium prevalence was 7% in red abalone individuals and 13% in the hybrid abalone. In contrast, the Japanese abalone did not present infections with either parasite. As with the prevalence, the infection intensities for the coccidium were higher in the hybrid abalone; of those infected 25% had grade 2 infections, and 75% had grade 3 infections, but the red abalone presented only grade 2 infection intensities. Therefore, the hybrid did not inherited non-susceptibility or resistance characteristics of the parental H. discus hannai and possessed biological conditions that could foster development of both parasites. Development of a culture based on this hybrid abalone should consider its susceptibility to infection by coccidian, WS-RLOs and the potential for developing the WS disease.
Año: 2014
Palabras claves: Withering Syndrome; Candidatus Xenohaliotis californiensis; Coccidium Margolisiella haliotis; Haliotis rufescens; Haliotis discus hannai; Abalone hybrid.
Referencia APA: González, R., Lohrmann, K., Pizarro, J., & Brokordt, K. (2014). Differential susceptibility to the Withering Syndrome agent and renal coccidia in juvenile Haliotis rufescens, Haliotis discus hannai and the interspecific hybrid. Journal Of Invertebrate Pathology, 116, 13-17
Albedo over rough snow and ice surfaces.
Lhermitte, S., Abermann, J., & Kinnard, C.
Both satellite and ground-based broadband albedo measurements over rough and complex terrain show several limitations concerning feasibility and representativeness. To assess these limitations and understand the effect of surface roughness on albedo, firstly, an intrasurface radiative transfer (ISRT) model is combined with albedo measurements over different penitente surfaces on Glaciar Tapado in the semi-arid Andes of northern Chile. Results of the ISRT model show effective albedo reductions over the penitentes up to 0.4 when comparing the rough surface albedo relative to the albedo of the flat surface. The magnitude of these reductions primarily depends on the opening angles of the penitentes, but the shape of the penitentes and spatial variability of the material albedo also play a major role.
Secondly, the ISRT model is used to reveal the effect of using albedo measurements at a specific location (i.e., apparent albedo) to infer the true albedo of a penitente field (i.e., effective albedo). This effect is especially strong for narrow penitentes, resulting in sampling biases of up to ±0.05. The sampling biases are more pronounced when the sensor is low above the surface, but remain relatively constant throughout the day. Consequently, it is important to use a large number of samples at various places and/or to locate the sensor sufficiently high in order to avoid this sampling bias of surface albedo over rough surfaces. Thirdly, the temporal evolution of broadband albedo over a penitente-covered surface is analyzed to place the experiments and their uncertainty into a longer temporal context. Time series of albedo measurements at an automated weather station over two ablation seasons reveal that albedo decreases early in the ablation season. These decreases stabilize from February onwards with variations being caused by fresh snowfall events. The 2009/2010 and 2011/2012 seasons differ notably, where the latter shows lower albedo values caused by larger penitentes. Finally, a comparison of the ground-based albedo observations with Landsat and MODIS (Moderate Resolution Imaging Spectroradiometer)-derived albedo showed that both satellite albedo products capture the albedo evolution with root mean square errors of 0.08 and 0.15, respectively, but also illustrate their shortcomings related to temporal resolution and spatial heterogeneity over small mountain glaciers.
Año: 2014
Palabras claves:
Referencia APA: Lhermitte, S., Abermann, J., & Kinnard, C. (2014). Albedo over rough snow and ice surfaces. The Cryosphere, 8(3), 1069-1086.
Condiciones paleovegetacionales y asentamientos humanos durante el formativo temprano: análisis de polen del sitio Tulán-85 (1.530/1.260-460/420 años cal. a.c.), cuenca del Salar de Atacama.
González-Silvestre, L., Maldonado, A., Núñez, L., Cartajena, I., Carrasco, C., & de Souza, P.
Se presenta el análisis polínico obtenido de una columna estratigráfica que cubre toda la secuencia ocupacional del asentamiento formativo temprano Tulán-85 localizado al sureste del salar de Atacama fechado entre los 1.530-1.260 a 460-420 cal. a.C. Se concluye que es posible diferenciar mediante el polen actual tres pisos altitudinales de vegetación, al tanto que la comparación de las muestras fósiles con aquellas actuales sugieren condiciones de mayor humedad en la base de la secuencia, al comienzo de la fase Tilocalar (1.530-1.260 cal. a.C.). En los niveles medios comienzan los eventos áridos, identificándose al final de la columna los mayores indicadores de aridez. Los antecedentes paleoclimáticos de la alta puna señalan que las ocupaciones pastoralistas de la fase Tilocalar son sincrónicas con el establecimiento de condiciones más húmedas, lo que es concordante con los resultados del análisis polínico. Estas habrían repercutido favorablemente en las ocupaciones pastoralistas en los pisos inferiores. Es importante destacar la identificación de eventos de aridez hacia el final de la ocupación, los que no habían sido descritos con anterioridad para el área de estudio.
Año: 2013
Palabras claves: Formativo Temprano, polen fósil, condiciones húmedas, eventos áridos, salar de Atacama.
Referencia APA: González-Silvestre, L., Maldonado, A., Núñez, L., Cartajena, I., Carrasco, C., & de Souza, P. (2013). Condiciones paleovegetacionales y asentamientos humanos durante el formativo temprano: análisis de polen del sitio Tulán-85 (1.530/1.260-460/420 años cal. a.c.), cuenca del Salar de Atacama. Chungará (Arica), 45(3), 387-410.
Parameterisation of incoming longwave radiation over glacier surfaces in the semiarid Andes of Chile.
MacDonell, S., Nicholson, L., & Kinnard, C.
A good understanding of radiation fluxes is important for calculating energy, and hence, mass exchange at glacier surfaces. This study evaluates incoming longwave radiation measured at two nearby glacier stations in the high Andes of the Norte Chico region of Chile. These data are the first published records of atmospheric longwave radiation measurements in this region. Nine previously published optimised parameterisations for clear sky emissivity all produced results with a root mean square error (RMSE) ~20 W m−2 and bias within ±5 W m−2, which is inline with findings from other regions. Six optimised parameterisations for incoming longwave in all sky conditions were trialled for application to this site, five of which performed comparably well with RMSE on daytime data <18 W m−2 and bias within ±6 W m−2 when applied to the optimisation site and RMSE <20 W m−2 and bias within ±10 W m−2 when applied to the validation site. The parameterisation proposed by Mölg et al. (J Glaciol 55:292-302, 2009) was selected for use in this region. Incorporating the proposed elevation modification into the equation reduced the bias in the modelled incoming longwave radiation for the validation site. It was found that applying the parameterisation optimised in the original work at Kilimanjaro produced good results at both the primary and validation site in this study, suggesting that this formulation may be robust for different high mountain regions.
Año: 2013
Palabras claves:
Referencia APA: MacDonell, S., Nicholson, L., & Kinnard, C. (2013). Parameterisation of incoming longwave radiation over glacier surfaces in the semiarid Andes of Chile. Theoretical And Applied Climatology, 111(3-4), 513-528.
Ecophysiological constraints on the larvae of Pleuroncodes monodon and the implications for its reproductive strategy in poorly oxygenated waters of the Chile-Peru undercurrent.
Yannicelli, B. & Castro, L.
Pleuroncodes monodon is a conspicuous component of the Humboldt Current ecosystem. Benthic adults south of ∼22°S are associated with low temperature (T) ∼11°C and low dissolved oxygen (DO) (<0.5 mL L−1) waters during the hatching period. Because P. mondon inhabits an oxygen minimum zone and larval release is assumed to match most favorable environmental conditions, larval performance under cold hypoxic conditions and its implications have not yet been assessed experimentally. We quantitatively assessed the effect of DO and T within environmental ranges, and initial starvation on survival, developmental time, and growth of P. monodon zoeae. Molting success from zoea I to zoea II was significantly and positively dependent on DO rearing levels. Age at molting was a negative power function of oxygen concentration. Initial exposure to low DO increased larval mortality by 3% per day of exposure. After ∼4 and ∼1.5 days of starvation after birth under normoxia and hypoxia, respectively, 50% of larvae failed to molt to zoea II. Rearing in 1 mL L−1 DO produced 50% lighter larvae after molting into zoea II. Mortality of larvae reared at 11°C was 40% higher than that at 15 and 20°C. Functions for development time and growth negative/positive dependence on temperature were also fitted. Pleuroncodes monodon zoea I are highly tolerant of low oxygen when compared with other crustacean. Nevertheless, DO and T conditions during hatching season are suboptimal for development. Early larval survival as an ultimate cause of reproductive/environmental coupling in this case should be critically revised.
Año: 2013
Palabras claves: Developmental time, growth, hypoxia, Pleuroncodes monodon, point-of-no-return, survival, temperature.
Referencia APA: Yannicelli, B. & Castro, L. (2013). Ecophysiological constraints on the larvae of Pleuroncodes monodon and the implications for its reproductive strategy in poorly oxygenated waters of the Chile-Peru undercurrent. Journal Of Plankton Research, 35(3), 566-581.
Linking human activity and ecosystem condition to inform marine ecosystem based management.
Menzel, S., Kappel, C., Broitman, B., Micheli, F., & Rosenberg, A.
There is growing consensus that integrated marine management is needed. However, implementation of ecosystem-based management (EBM) faces major operational challenges, including accurately delineating the links between ecosystem components and benefits to humans, and quantifying trade-offs associated with different management decisions.
It is suggested using human activity level as an indicator of the benefit provided by marine ecosystems at a certain location in comparison with other locations and establishing links between human activity levels and ecological conditions.
This approach allows for the determination of what ecological conditions may provide the greatest human benefits and thus may be targets for management action.
This approach is used to investigate the link between scuba diving in the Monterey Bay area, California, USA, and different ecological characteristics of kelp forests. Diving intensity levels correlate with kelp persistence, suggesting that kelp persistence may be used as an indicator of benefits from diving and for evaluating the impact of potentially competing activities through their effects on kelp.
Overall, an operational definition of marine ecosystem services is provided and it is suggested that this method could be extended to a suite of different activities and systems and thus may become useful in considering trade-offs among different activities that depend upon the same ecosystem.
Año: 2013
Palabras claves: Ecosystem services; natural resource management; ecological indicators; Monterey Bay; California; kelp forest ecosystem; scuba diving; ecological production function; human benefits from ecosystems.
Referencia APA: Menzel, S., Kappel, C., Broitman, B., Micheli, F., & Rosenberg, A. (2013). Linking human activity and ecosystem condition to inform marine ecosystem based management. Aquatic Conserv: Mar. Freshw. Ecosyst., 23(4), 506-514.
The response of leaf respiration to water stress in Nothofagus species.
Sanhueza, C., Bascunan-Godoy, L., Corcuera, L., & Turnbull, M.
Nothofagus solandri is regarded as more tolerant to drought than Nothofagus menziesii in the field. However, the physiology of responses to water limitation in these species is not well understood. In this study, the thermal sensitivity of leaf respiration and its underlying metabolism in response to drought were investigated in mature trees and saplings. Respiration (R d) and photosynthesis (A max) were measured during drying and re-wetting cycles. In addition, respiratory pathway changes were evaluated by oxygen isotope fractionation and protein analyses. Under drought treatment in the glasshouse, both species showed similar photosynthetic performance, but under mild water stress N. solandri was able to increase A max. Under moderate water deficit (around −2 MPa), N. solandri increased respiration at a base temperature of 10°C (R 10) but then decreased it to initial values after re-watering. In N. menziesii, R 10 did not respond significantly to water-stress treatment. The temperature sensitivity of R d (Q 10 and E o) was unchanged for both species during the gradual deficit water treatment in the glasshouse. Although respiratory electron flow was mainly via the cytochrome pathway under all conditions, an increase in alternative oxidase/cytochrome oxidase protein content suggests that the alternative pathway is involved in modulating respiratory metabolism during the recovery after drought.
Año: 2013
Palabras claves: Alternative oxidase, cytochrome oxidase, drought, metabolism, New Zealand, trees.
Referencia APA: Sanhueza, C., Bascunan-Godoy, L., Corcuera, L., & Turnbull, M. (2013). The response of leaf respiration to water stress in Nothofagus species. New Zealand Journal Of Botany, 51(2), 88-103.
Analysis of benthic macroinvertebrates and biotic indices to evaluate water quality in rivers impacted by mining activities in northern Chile.
Alvial, I., Tapia, D., Castro, M., Duran, B., & Verdugo, C.
Catchments in the semiarid regions are especially susceptible to environmental perturbation associated with water scarcity, hydrological variations and overuse by anthropogenic activities. Using multivariate analysis to relate environmental and biological data, and diversity and biotic indices (ChBMWP, ChIBF), we analyzed the macroinvertebrate composition of 12 rivers of the semiarid region of northern Chile. A non-metric multidimensional scaling for macroinvertebrate taxa and a principal component analysis for environmental variables strongly separated upstream sites (e.g. Vacas Heladas and Malo Rivers), which presented low pH and high dissolved metal concentrations, from other sites. Effectively, CCA showed that metals and low pH, associated with the altitudinal gradient, determined the distributional patterns of macroinvertebrates in the Elqui catchment. The causes of these particular conditions could be related to geological processes and human impact. The biotic indices applied to the sampling sites corroborated and reflected these characteristics, with La Laguna and Turbio Rivers showing a diverse macroinvertebrate community and moderate to good water quality, and the Claro River showing favorable conditions for the development of aquatic biota, indicating its better quality relative to other stations. To the middle and low part of the basin, a change in the composition of the community was observed, with species that suggest an impact by an increase in organic matter, due to agricultural activities and urban settlements concentrated in this area. Our results suggest that macroinvertebrate taxa in northern Chile may be exceptional species, adapted to unfavorable geochemical conditions, and emphasize the need for protection of the semiarid basins of the region.
Año: 2013
Palabras claves: macro-invertebrates / biotic indices / multivariate analysis / semiarid region
Referencia APA: Alvial, I., Tapia, D., Castro, M., Duran, B., & Verdugo, C. (2013). Analysis of benthic macroinvertebrates and biotic indices to evaluate water quality in rivers impacted by mining activities in northern Chile. Knowledge And Management Of Aquatic Ecosystems, (407), 01.
Meteorological observations on the northern Chilean coast during VOCALS-REx.
Rutllant, J., Muñoz, R., & Garreaud, R.
Surface coastal observations from two automatic weather stations at Paposo (~25° S) and radiosonde observations at Paposo and Iquique (~20° S) were carried out during VOCALS-REx (VAMOS Ocean-Cloud-Atmosphere-Land Study Regional Experiment). Within the coastal marine boundary layer (MBL), sea–land breezes are superimposed on the prevailing southerlies, resulting in light northeasterly winds from midnight to early morning and strong southwesterlies in the afternoon. The prevailing northerlies above the MBL and below the top of the Andes are modulated by the onshore-offshore (zonal) flow forced by the diurnal cycle of surface heating/cooling along the western slope of the Andes. The daytime phase of this diurnal cycle is consistent with an enhanced afternoon coastal subsidence manifested in afternoon warming near the top of the subsidence inversion (~1.8 K at 800 hPa), lowering (~130 m) of its base (top of the MBL), and clearing of coastal Sc (stratocumulus) clouds. Results from a numerical simulation of the atmospheric circulation in a mean zonal cross section over the study area capture the afternoon zonal wind divergence and resulting subsidence of about 2 cm s−1 along a narrow (~10 km) coastal strip maximizing at around 800 hPa. Day-to-day variability in the MBL depth during VOCALS-REx shows sub-synoptic oscillations, aside from two major disruptions in connection with a deep trough and a cutoff low, as described elsewhere. These oscillations are phase-locked to those in sea-level pressure and afternoon alongshore southerlies, as found in connection with coastal lows farther south.
From 24-h forward trajectories issued from significant points at the coast and inland at the extremes of the diurnal cycle, it can be concluded that the strong mean daytime Andean pumping prevents any possibility of continental sulfur sources from reaching the free troposphere above the Sc cloud deck in at least a one-day timescale, under mean conditions. Conversely, coastal sources could contribute with sulfur aerosols preferentially in the morning, provided that the weak daytime inland flow becomes partially blocked by the coastal terrain.
Año: 2013
Palabras claves:
Referencia APA: Rutllant, J., Muñoz, R., & Garreaud, R. (2013). Meteorological observations on the northern Chilean coast during VOCALS-REx. Atmospheric Chemistry And Physics, 13(6), 3409-3422.