Modeling the Effects of Size on Patch Dynamics of an Inert Tracer

Mesoscale iron enrichment experiments have revealed that additional iron affects the phytoplankton productivity and carbon cycle. However, the role of initial size of fertilized patch in determining the patch evolution is poorly quantified due to the limited observational capability and complex of physical processes. Using a three-dimensional ocean circulation model, we simulated different sizes of inert tracer patches that were only regulated by physical circulation and diffusion. Model results showed that during the first few days since release of inert tracer, the calculated dilution rate was found to be a linear function with time, which was sensitive to the initial patch size with steeper slope for smaller size patch. After the initial phase of rapid decay, the relationship between dilution rate and time became an exponential function, which was also size dependent. Therefore, larger initial size patches can usually last longer and ultimately affect biogeochemical processes much stronger than smaller patches.

Regional-Scale Mean Copepod Concentration Indicates Relative Abundance of North Atlantic Right Whales

Management plans to reduce human-caused deaths of North Atlantic right whales Eubalaena glacialis depend, in part, on knowing when and where right whales are likely to be found. Local environmental conditions that influence movements of feeding right whales, such as ultra-dense copepod patches, are unpredictable and ephemeral. We examined the utility of using the regional-scale mean copepod concentration as an indicator of the abundance of right whales in 2 critical habitats off the northeastern coast of the United States: Cape Cod Bay and Great South Channel. Right whales are usually found in Cape Cod Bay during the late winter and early spring, and in the Great South Channel during the late spring and early summer. We found a significant positive relationship between mean concentration of the copepod Calanus finmarchicus in the western Gulf of Maine and the frequency of right whale sightings in the Great South Channel. In Cape Cod Bay we found a significant positive relationship between the mean concentration of other copepods (largely Pseudocalanus spp. and Centropages spp.) and the frequency of right whale sightings. This information could be used to further our understanding of the environmental factors that drive seasonal movement and aggregation of right whales in the Gulf of Maine, and it offers a tool to resource managers and modelers who seek to predict the movements of right whales based upon the concentration of copepods.

SYNTHETIC PROBES FOR STUDYING TUFTSIN-RECEPTOR INTERACTIONS ON HUMAN POLYMORPHONUCLEAR LEUKOCYTES

Tuftsin is an immunopotentiating tetrapeptide of the sequence L-Thr-L-Lys-L-Pro-L-Arg with anti-microbial and anti-tumor enhancing capabilities. These enhancing functions are manifested through the host's granulocytes and monocytes. In delineating tuftsin's mechanism of action, both radiolabeled and fluorescent probes were synthesized. The radiolabeled probe of tuftsin, L-proly-3,4-('3)H(N) -tuftsin, was obtained through the synthesis and subsequent catalytic hydrogenation of L-3,4-dehydroprolyl ('3)-tuftsin using tritium gas. This procedure yielded a probe with a specific activity of 44.9 Ci/mmole. This radiolabeled probe of tuftsin was used in competitive inhibition studies with tuftsin, the tuftsin analogues Lys-Pro-Arg, Thr-Lys-Pro-Arg(NO(,2)) and (DELTA)('3)-pro('3) -tuftsin as well as with the chemotactic peptide f-Met-Leu-Phe. From the competitive binding curves, the K(,D) for tuftsin was estimated to be 80 nM, a value that approaches the concentration of tuftsin that evokes a half maximal biological response. The approximate Ki's for the tuftsin analogues (33 nM) approached that of tuftsin itself (40 nM). On the other hand, approximately a two log difference in the Ki was seen with the chemotactic tripeptide, indicating that tuftsin may indeed be acting through the chemotactic peptide receptor. This conclusion is further strengthened by studies using an N-terminal derivitized mono-fluoresceinated tuftsin probe and image intensification microscopy. These studies showed that like the chemotactic peptide, tuftsin initially binds to diffusely distributed receptors on the surface of human granulocytes. The tuftsin-receptor complexes then rapidly redistribute to form patches (5 min @ 37(DEGREES)C) which are then internalized. Whether redistribution and internalization of tuftsin-receptor complexes is crucial in effecting a biological response, or simply an intermediary point leading ultimately to degradation, is still not clear. This process, however, may provide the target cell with an early time point in modulating the biological effects of tuftsin through down-regulation of cell surface receptor sites. ^

Mechanism of damage sensing and cell killing following the inhibition of nucleotide excision repair by fludarabine in quiescent cells

Inhibition of DNA repair by the nucleoside of fludarabine (F-ara-A) induces toxicity in quiescent human cells. The sensing and signaling mechanisms following DNA repair inhibition by F-ara-A are unknown. The central hypothesis of this project was that the mechanistic interaction of a DNA repair initiating agent and a nucleoside analog initiates an apoptotic signal in quiescent cells. The purpose of this research was to identify the sensing and signaling mechanism(s) that respond to DNA repair inhibition by F-ara-A. Lymphocytes were treated with F-ara-A, to accumulate the active triphosphate metabolite and subsequently DNA repair was activated by UV irradiation. Pre-incubation of lymphocytes with 3 μM F-ara-A inhibited DNA repair initiated by 2 J/m2 UV and induced greater than additive apoptosis after 24 h. Blocking the incorporation of F-ara-A nucleotide into repairing DNA using 30 μM aphidicolin considerably lowered the apoptotic response. ^ Wild-type quiescent cells showed a significant loss in viability than did cells lacking functional sensor kinase DNA-PKcs or p53 as measured by colony formation assays. The functional status of ATM did not appear to affect the apoptotic outcome. Immunoprecipitation studies showed an interaction between the catalytic sub-unit of DNA-PK and p53 following DNA repair inhibition. Confocal fluorescence microscopy studies have indicated the localization pattern of p53, DNA-PK and γ-H2AX in the nucleus following DNA damage. Foci formation by γ-H2AX was seen as an early event that is followed by interaction with DNA-PKcs. p53 serine-15 phosphorylation and accumulation were detected 2 h after treatment. Fas/Fas ligand expression increased significantly after repair inhibition and was dependent on the functional status of p53. Blocking the interaction between Fas and Fas ligand by neutralizing antibodies significantly rescued the apoptotic fraction of cells. ^ Collectively, these results suggest that incorporation of the nucleoside analog into repair patches is critical for cytotoxicity and that the DNA damage, while being sensed by DNA-PK, may induce apoptosis by a p53-mediated signaling mechanism. Based on the results, a model is proposed for the sensing of F-ara-A-induced DNA damage that includes γ-H2AX, DNA-PKcs, and p53. Targeting the cellular DNA repair mechanism can be a potential means of producing cytotoxicity in a quiescent population of neoplastic cells. These results also provide mechanistic support for the success of nucleoside analogs with cyclophosphamide or other agents that initiate excision repair processes, in the clinic. ^

The role of Lmx1b in the control of dorsoventral compartmentalization in the distal mesenchyme of the developing mouse limb

Lmx1b encodes a LIM-homeodomain transcription factor required for dorso-ventral (D-V) patterning in the mesenchyme of the vertebrate limb. In the absence of Lmx1b function, limbs exhibit a bi-ventral pattern indicating that Lmx1b is required for cells to adopt a dorsal cell fate. However, how Lmx1b specifies dorsal cell fates in the mesenchyme of the distal limb is unknown. Lmx1b is initially expressed throughout the dorsal and ventral limb bud mesenchyme, then becomes dorsally restricted around E10.5. At this stage, there is a sharp boundary between Lmx1b expressing and Lmx1b non-expressing cells. How the dorso-ventral Lmx1b expression boundary is formed and maintained is currently unknown. One mechanism that may contribute to establishing and/or maintaining the Lmx1b expression boundary is if the dorsal mesenchyme is a lineage-based compartment, where different groups of non-mingling cells are separated. Compartment formation has been proposed to rely on compartment-specific selector gene activity which functions to restrict cells to a compartment and specifies the identity of cells within that compartment. Based on the evidence that the dorsal limb identity relies on the expression of Lmx1b in the dorsal half of the limb mesenchyme, we hypothesized that Lmx1b might function as a dorsal limb bud mesenchyme selector gene to set up a dorsal compartment. To test this hypothesis, we developed an inducible CreERT2/ loxP based fate mapping approach that permanently marks Lmx1b wild-type and mutant cells and examined the distribution of their descendents in the developing limb. Our data is the first to show that dorso-ventral lineage compartments exist in the limb bud mesenchyme. Furthermore, Lmx1b is required for maintenance of the dorso-ventral compartment lineage boundary. The behavior of Lmx1b mutant cells that cross into the ventral mesenchyme, as well as previous chimera analysis in which mutant cells spread evenly in the ventral limb and form patches in the dorsal side, suggest that cell affinity differences prevent intermingling of dorsal and ventral cells. ^

Association of pellicle growth morphological characteristics and clinical presentation of Mycobacterium tuberculosis isolates

Trehalose dimycolate (TDM) is a mycobacterial glycolipid that is released from the surface of virulent M. tuberculosis. We evaluated the rate of growth, colony characteristics and production of TDM by Mycobacterium tuberculosis strains isolated from different clinical sites. Since detergent removes TDM from organisms, we analyzed growth rate and colony morphology of 79 primary clinical isolates grown as pellicles on the surface of detergent free Middlebrook 7H9 media. The genotype of each had been previously characterized. TDM production was measured by thin layer chromatography on 32 of these isolates. We found that strains isolated from pulmonary sites produced large amounts of TDM, grew rapidly as thin spreading pellicles, showed early cording (<1 week) and climbed the sides of the dish. In contrast, the extrapulmonary isolates (lymph node and bone marrow) produced less TDM (p<0.01), grew as discrete patches with little tendency to spread or climb the walls (p<0.02). The Beijing pulmonary (BP) isolates produced more TDM than non Beijing pulmonary isolates. The largest differences were observed in Beijing strains. The Beijing pulmonary isolates produced more TDM and grew faster than the Beijing extrapulmonary isolates (p<0.01). This was true even when the pulmonary and extrapulmonary isolates were derived from the same clade. These growth characteristics were consistently observed only on the first passage after primary isolation. This suggests that the differences in growth rate and TDM production observed reflect differences in gene expression patterns of pulmonary and extrapulmonary infections, that Mycobacterium tuberculosis in the lung grows more rapidly and produces more TDM than it does in extrapulmonary sites. This provides new opportunities to investigate gene expression of Mycobacterium tuberculosis in human.^

Soil properties of western Wright Valley, Antarctica

Western Wright Valley, from Wright Upper Glacier to the western end of the Dais, can be divided into three broad geomorphic regions: the elevated Labyrinth, the narrow Dais which is connected to the Labyrinth, and the North and South forks which are bifurcated by the Dais. Soil associations of Typic Haplorthels/Haploturbels with ice-cemented permafrost at < 70 cm are most common in each of these geomorphic regions. Amongst the Haplo Great Groups are patches of Salic and Typic Anhyorthels with ice-cemented permafrost at > 70 cm. They are developed in situ in strongly weathered drift with very low surface boulder frequency and occur on the upper erosion surface of the Labyrinth and on the Dais. Typic Anhyorthels also occur at lower elevation on sinuous and patchy Wright Upper III drift within the forks. Salic Aquorthels exist only in the South Fork marginal to Don Juan Pond, whereas Salic Haplorthels occur in low areas of both South and North forks where any water table is > 50 cm. Most soils within the study area have an alkaline pH dominated by Na+ and Cl- ions. The low salt accumulation within Haplorthels/Haploturbels may be due to limited depth of soil development and possibly leaching.

Parches de vegetación arvense en una toposecuencia de altos y bajos en cultivos de manzanos : Mendoza (Argentina)

En un cultivo de manzanos en la provincia de Mendoza, Argentina, se observó la presencia de las comunidades dominadas por Cynodon dactylon y Galinsoga parviflora localizadas entre y bajo las copas de los árboles frutales, en coincidencia con una toposecuencia de relieves de altos y bajos, respectivamente. Ante el hecho de estar frente a un interesante ejemplo agronómico de establecimiento de comunidades arvenses se las analizó fisonómica, florística y sociológicamente, relacionándolas con las condiciones ecológicas, físico-químicas de los suelos y bioclimáticas de los sitios que las contienen. Mientras la comunidad de Cynodon dactylon presente en los altos o entre plantas resultó más luminosa, cálida, seca y menos fértil, la de Galinsoga parviflora en los bajos fue más sombría, fría, húmeda y más fértil. En esta última, la alta concentración de materia orgánica, nutrientes minerales y humedad de los suelos parece estar relacionada con la presencia de plantas anuales bajo las copas. Los resultados obtenidos muestran la importancia de las toposecuencias de relieves de altos y bajos en la distribución, estructura y composición florística de las comunidades vegetales arvenses, las cuales pueden resultar potenciadas con las coberturas de las copas de los árboles frutales.

Physalis viscosa : un nuevo hospedero de Leveillula taurica en Argentina

Leveillula taurica (Lév.) Salm. es un hongo patógeno que se encuentra actualmente en expansión en nuestro país y en particular en la provincia de Mendoza. Physalis viscosa (camambú) es una especie muy difundida en Argentina. La misma es principalmente una maleza que crece espontáneamente en numerosos cultivos de interés económico y en sus alrededores. El hallazgo de L. taurica sobre una especie tan difundida fue el motivo de su estudio. Los síntomas característicos observados fueron parches cuneiformes amarillos en la cara adaxial de las hojas y en correspondencia con los mismos, en la abaxial se presentó un afelpado blanquecino formado por las fructificaciones asexuales del patógeno. El estudio etiológico realizado mediante la histopatología de los órganos afectados y la morfometría del patógeno confirmó la presencia del hongo parásito obligado Leveillula taurica (Lév.) Salm., en su forma anamórfica Oidiopsis taurica Sal. [= Oidiopsis sicula (Scal)]. La enfermedad en el camambú se ha difundido en forma importante en la provincia de Mendoza desde su primer hallazgo en el departamento de Tupungato en 1996. Se encuentra presente desde diciembre hasta mayo. Este prolongado período puede representar una importante fuente de inóculo para cultivos susceptibles al patógeno. La presente constituye la primera cita, no sólo a nivel nacional sino también mundial, de L. taurica sobre Physalis viscosa.

Effect of Prosopis flexuosa on understory species and its importance to pastoral management in woodlands of the Central Monte Desert

In the Monte Biogeographic Province, located in the arid region of Argentina, the presence of Prosopis flexuosa DC. produces spatial heterogeneity through edaphic modifications and microclimate changes. This results in vegetation patches differing in species composition and abundance. However, this interaction can be modified by the occurrence of gradients of biotic stress or disturbance intensity. In particular, grazing has been observed to enhance or reduce vegetation heterogeneity. Such complex of interactions could determine forage availability for cattle in one of the driest areas of the Monte Desert. We assessed the effect of Prosopis on understory species and analyzed whether the outcomes of this interaction differed with distance to watering points, as a proxy of grazing intensity, in the Northeast of Mendoza Province, Argentina. We used a two-way factorial design including the following factors: 1) microsite (under the cover of P. flexuosa trees and in intercanopy microsites) and 2) distance to watering points ("near the watering point", 500-700 m away, and "far from the watering point", 3-4 km away). Cover of each species, total cover, bare soil, and litter were recorded, and plant diversity, richness, and evenness were estimated with the modified Point Quadrat method. Results showed that P. flexuosa cover, distance from watering points, and the interaction between them determined species composition, abundance and spatial distribution of understory species, and were, consequently, a determining factor for forage availability. The presence of P. flexuosa enhances carrying capacity by supporting higher abundance of grasses under its canopy. Near watering points, high grazing intensity appears to disrupt the patches formed under P. flexuosa canopies, reducing the differences between microsites.

Diet selection by the lesser rhea (Rhea pennata pennata) in Payunia, Northern Patagonia (Mendoza, Argentina)

The lesser rhea (family Rheidae) is a flightless large bird of South America, threatened due to habitat loss, hunting and egg collecting, with special concern in Northern Patagonia. Diet and food availability were estimated throughout the year by micro-histological analysis and point-quadrat transects in a landscape inside and another outside the Payunia Reserve, the northernmost part of the Rhea pennata pennata distribution. Significant differences were detected by Kruskall-Wallis ANOVA, food selection by Chi-square test and Bailey’s confidence interval. A strong food selection characterized the diet of lesser rheas, dominated by leaves of shrubs and forbs, complemented by dicot seeds and a few insects. This agrees with the documented low dietary overlap with other herbivores in Payunia. Dietary changes agree with the expected from the selective quality hypothesis. Food availability was better inside than outside the protected area, with probable conservation effects for lesser rheas. Seeds, forbs and soft grasses could be for lesser rheas some key food resources to survive during unfavorable seasons in arid environments without "mallines", as Payunia. Shrubby patches, with high availability of preferred food items (tall shrubs and forbs), stood out as key habitats. Therefore, avoiding fire and woody plant removal is crucial for the conservation of lesser rheas in the northern of its range.

Dinámica temporal de la masa de broza en distintos microhábitats del desierto del Monte Central (Mendoza, Argentina)

Uno de los mecanismos propuestos para el enriquecimiento del suelo generado bajo la cobertura de leñosas en zonas áridas es la relocalización de nutrientes absorbidos por sus extensos sistemas radicales hacia el área bajo su dosel. Sin embargo, el efecto final sobre la fertilidad del suelo depende de los distintos procesos que transforman la broza y liberan nutrientes. Prosopis flexuosa D.C. (algarrobo) es la especie leñosa de mayor producción de broza y genera islas de fertilidad bajo su dosel en el Monte Central. En este trabajo analizamos la dinámica temporal de la masa de la broza caída bajo P. flexuosa, en distintos microhábitats (bajo la copa de P. flexuosa, bajo Larrea divaricata, en áreas próximas a árboles talados, y en áreas expuestas). Encontramos una mayor disminución en la masa de broza en invierno, sin diferencias entre microhábitats, y menores tasas de pérdida y mayor heterogeneidad espacial en primavera y verano. Nuestros resultados sugieren que la dinámica de la broza depende principalmente de su composición, ya que es mayor la tasa de pérdida, inmediatamente después del ingreso de broza producida por la caída de hojas de P. flexuosa no obstante las condiciones ambientales desfavorables para la actividad de microorganismos. A pesar de observarse diferencias en la dinámica de la broza entre los microhábitats, la magnitud total de los cambios de masa de broza no presenta una variabilidad espacial importante. Por el contrario, se detectó relocalización secundaria de broza, producto de la actividad de artrópodos y posiblemente otros factores (agua-viento), los que podrían actuar como moderadores de las diferencias generadas por la concentración de broza bajo las leñosas.

Export of algal biomass from the melting Arctic sea ice

In the Arctic, under-ice primary production is limited to summer months and is not only restricted by ice thickness and snow cover but also by the stratification of the water column, which constrains nutrient supply for algal growth. RV Polarstern visited the ice-covered Eastern Central basins between 82 to 89°N and 30 to 130°E in summer 2012 when Arctic sea ice declined to a record minimum. During this cruise, we observed a widespread deposition of ice algal biomass of on average 9 g C per m**2 to the deep-sea floor of the Central Arctic basins. Data from this cruise will contribute to assessing the impact of current climate change on Arctic productivity, biodiversity, and ecological function.

Preliminary results and documentation of sediment cores CRP2 and CRP-2A from the Ross Sea off Cape Roberts, Antarctica

The site for CRP-2, 14 km east of Cape Roberts (77.006°S; 163.719°E), was selected to overlap the early Miocene strata cored in nearby CRP-1, and to sample deeper into the east-dipping strata near the western margin ofe he Victoria Land Basin to investigate Palaeogene climatic and tectonic history. CRP-2 was cored from 5 to 57 mbsf (metres below the sea floor) (core recovery 91 %), with a deviation resulting in CRP-2A being cored at the same site. CRP-2A reached down to 624mbsf (recovery 95%), and to strata with an age of c. 33-35 Ma. Drilling took place from 16 October to 25 November 1998, on 2.0-2.2 m of sea ice and through 178 m of water. Core fractures and other physical properties, such as sonic velocity, density and magnetic susceptibility, were measured throughout the core. Down-hole logs for these and other properties were run from 63 to 167 mbsf and subsequently from 200 to 623 mbsf, although density and velocity data could be obtained only to 440 mbsf because of hole collapse. Sonic velocity averages c. 2.0 km S-1 for the upper part of the hole, but there is an sharp increase to c. 3.0 km s-1 and also a slight angular unconformity, at 306 mbsf, corresponding most likely to the early/late Oligocene boundary (c. 28-30 Ma). Velocity then increases irregularly to around 3.6 km s-1 at the bottom of the hole, which is estimated to lie 120 m above the V4/V5 boundary. The higher velocities below 306 mbsf probably reflect more extensive carbonate and common pyrite cementation, in patches, nodules, bedding-parallel masses and as vein infills. Dip of the strata also increases down-hole from 3° in the upper 300 in to over 10° at the bottom. Temperature gradient is 21° k-1. Over 2 000 fractures were logged through the hole. Borehole televiewer imagery was obtained for the interval from 200 to 440 mbsf to orient the fractures for stress field analysis. Lithostratigraphical descriptions on a scale of 1:20 are presented for the full length of the core, along with core box images, as a 200 page supplement to this issue. The hole initially passed through a layer of muddy gravel to 5.5 mbsf (Lithological Sub-Unit or LSU 1.1), and then into a Quaternary diatom-bearing clast-rich diamicton to 21 mbsf (LSU 2. l), with an interval of alternating compact diamicton and loose sand, and containing a rich Pliocene foraminiferal fauna, to 27 mbsf (LSU 2.2). The unit beneath this (LSU 3.1) has similar physical properties (sonic velocity, porosity, magnetic susceptibility) and includes diamictites of similar character to those of LSU 2.1 and 2.2, but an early Miocene (c. 19 Ma) diatom assemblage at 28 mbsf (top of LSU 3.1) shows that this sub-unit is part of the older section. The strata beneath 27 mbsf, primary target for the project, extend from early Miocene to perhaps latest Eocene age, and are largely cyclic glacimarine nearshore to offshore sediments. They are described as 41 lithological sub-units and interpreted in terms of 12 recurrent lithofacies. These are 1) mudstone, 2) inter-stratified mudstone and sandstone, 3) muddy very fine to coarse sandstone, 4) well-sorted stratified fine sandstone, 5) moderately to well-sorted, medium-grained sandstone, 6) stratified diamictite, 7) massive diamictite, 8) rhythmically inter-stratified sandstone and mudstone, 9) clast-supported conglomerate, 10) matrix-supported conglomerate, 11) mudstone breccia and 12) volcaniclastic sediment. Sequence stratigraphical analysis has identified 22 unconformity-bounded depositional sequences in pre- Pliocene strata. They typically comprise a four-part architecture involving, in ascending order, 1) a sharp-based coarse-grained unit (Facies 6,7,9 or 10), 2) a fining-upward succession of sandstones (Facies 3 and 4), 3) a mudstone interval (Facies l), in some cases coarsening upward to muddy sandstones (Facies 3), and 4) a sharp-based sandstone dominated succession (mainly Facies 4). The cyclicity recorded by the strata is interpreted in terms of a glacier ice margin retreating and advancing from land to the west, and of rises and falls in sea level. Analysis of sequence periodicity awaits afirmer chronology. However, apreliminary spectral analysis of magnetic susceptibility for a deepwater mudstone within one of the sequences (from 339 to 347 mbsf) reveals ratios between hierarchical levels that are similar to those of the three Milankovitch orbital forcing periodicities. The strata contain a wide range of fossils, the most abundant being marine diatoms. These commonly form up to 5% of the sediment, though in places the core is barren (notably between 300 and 412 mbsf). Fifty samples out of 250 reviewed were studied in detail. The assemblages define ten biostratigraphical zones, some of them based on local or as yet undescribed forms. The assemblages are neritic, and largely planktonic, suggesting that the sea floor was mostly below the photic zone throughout deposition of the corcd sequence. Calcareous nannofossils, representing incursions of ocean surface waters, are much less common (72 out of 183 samples examined) and restricted to mudstone intervals a few tens of metres thick, but are important for dating. Foraminifera are also sparse (73 out of 135 samples) and represented only by calcareous benthic species. Changing assemblages indicate a shift from inshore environments in the early Oligocenc to outer shelf in the late Oligocenc, returning to inshore in the early Miocene. Marine palynomorplis yielded large numbers of well-preserved forms from most of the 116 samples examined. The new in situ assemblagc found last year in CRP-1 is extended down into the late Oligocene and a further new assemblage is found in the early Oligoccnc. Many taxa are new, and cannot us yet contribute to an improved understanding of chronology or ecology. Marine invertebrate macrofossils, mostly molluscs and serpulid tubes, are scattered throughout the core. Preservation is good in mudstones but poor in other lithologies. Climate on land is reflected in the content of terrestrial palynomorphs, which are extremely scarce down to c. 300 mbsf. Some forms are reworked, and others represent a low growing sparse tundra with at least one species of Nothofagus. Beneath this level, a significantly greater diversity and abundance suggests a milder climate and a low diversity woody vegetation in the early Oligocene, but still far short of the richness found in known Eocene strata of the region. Sedimentary facies in the oldest strata also suggest a milder climate in the oldest strata cored, with indications of substantial glacial melt-water discharges, but are typical of a coldcr climate in late Oligocene and early Miocene times. Clast analyses from diamictites reveal weak to random fabrics, suggesting either lack of ice-contact deposition or post-depositional modification, but periods when ice grounded at the drill site are inferred from thin zones of in-situ brecciated rock and soft-sediment folding. These are more common above c. 300 mbsf, perhaps reflecting more extensive glacial advances during deposition of those strata. Erosion of the adjacent Transantarctic Mountains through Jurassic basalt and dolerite-intruded Beacon strata into basement rocks beneath is recorded by petrographical studies of clast and sand grain assemblages. Core below 310 mbsf contains a dominance of fine-grained Jurassic dolerite and basalt fragments along with Beacon-derived coal debris and rounded quartz grains, whereas the strata above this level have a much higher proportion of basement derived granitoids, implying that the large areas of the adjacent mountains had been eroded to basement by the end of the early Oligocene. There is little indication of rift-related volcanism below 310 mbsf. Above this, however, basaltic and trachytic tephras are common, especially from 280 to 200 mbsf, from 150 to 46 mbsf, and in Pliocene LSU 2.2 from 21 to 27 mbsf. The largest volcanic eruptions generated layers of coarse (up to 1 cm) trachytic pumice lapilli between 97 and 114 mbsf. The thickest of these (1.2 m at 112 mbsf) may have produced an eruptive column extending tens of km into the stratosphere. A source within a few tens of km of the drill site is considered most likely. Present age estimates for the pre-Pliocene sequence are based mainly on biostratigraphy (using mainly marine diatoms and to a lesser extent calcareous nannofossils), with the age of the tephra from 112 to 114 mbsf (21.44k0.05 Ma from 84 crystals by Ar-Ar) as a key reference point. Although there are varied and well-preserved microfossil assemblages through most of the sequence (notably of diatoms and marine palynomorphs), they comprise largely taxa either known only locally or as yet undescribed. In addition, sequence stratigraphical analysis and features in the core itself indicate numerous disconformities. The present estimate from diatom assemblages is that the interval from 27 to 130 mbsf is early Miocene in age (c. 19 to 23.5 Ma), consistent with the Ar-Ar age from 112 to 114 mbsf. Diatom assemblages also indicate that the late Oligocene epoch extends from c. 130 to 307 mbsf, which is supported by late Oligocene nannofossils from 130 to 185 mbsf. Strata from 307 to 412 mbsf have no age-diagnostic assemblages, but below this early Oligocene diatoms and nannofossils have been recovered. A nannoflora at the bottom of the hole is consistent with an earliest Oligocene or latest Eocene age. Magnetostratigraphical studies based on about 1000 samples, 700 of which have so far undergone demagnetisation treatment, have provided a polarity stratigraphy of 12 pre-Pliocene magnetozones. Samples above 270 mbsf are of consistently high quality. Below this, magnetic behaviour is more variable. A preliminary age-depth plot using the Magnetic Polarity Time Scale (MPTS) and constrained by biostratigraphical data suggests that episodes of relatively rapid sedimentation took place at CRP-2 during Oligocene times (c. 100 m/My), but that more than half of the record was lost in a few major and many minor disconformities. Age estimates from Sr isotopes in shell debris and further tephra dating are expected to lead to a better comparison with the MPTS. CRP-2/2A has recorded a history of subsidence of the Victoria Land Basin margin that is similar to that found in CIROS-170 km to the south, reflecting stability in both basin and the adjacent mountains in late Cenozoic times, but with slow net accumulation in the middle Cenozoic. The climatic indicators from both drill holes show a similar correspondence, indicating polar conditions for the Quaternary but with sub-polar conditions in the early Miocene-late Oligocene and indications of warmer conditions still in the early Oligocene. Correlation between the CRP-2A core and seismic records shows that seismic units V3 and V4, both widespread in the Victoria Land Basin, represent a period of fluctuating ice margins and glacimarine sedimentation. The next drill hole, CRP-3, is expected to core deep into V5 and extend this record of climate and tectonics still further back in time.

Variación temporal y espacial de parches, corredores y matriz en un humedal ("mallín") del centro-oeste de la provincia de Neuquén

Los procesos naturales, como las actividades humanas, cambian los paisajes. Esta realidad no es ajena a los humedales (mallines) en Patagonia. Los mallines son importantes ecosistemas naturales que sirven como recurso forrajero para la ganadería extensiva. Los mismos representan el 4 de la superficie patagónica. Los períodos húmedos y secos modifican la dinámica hidrológica del mallín. Esto repercute en la evolución de los parches, corredores y matriz, que se agrava con la actividad antrópica. En una secuencia temporal se puede apreciar la fragmentación del hábitat: en la variación y tamaño del número de parches, su forma, conectividad y aislamiento, que entre otros factores inciden sobre numerosos procesos ecológicos. El conocimiento de la dinámica temporal y espacial de los parches, corredores y matriz entre un período húmedo y uno seco en un humedal permite la planificación del uso del recurso vegetación, ya que los patrones espaciales controlan fuertemente sus movimientos, flujos y cambios.