Collection of data on plant height along the plant diversity gradient in the Jena Experiment (Main Experiment, time series since 2002)

This data set contains a time series of plant height measurements (vegetative and reproductive) from the main experiment plots of a large grassland biodiversity experiment (the Jena Experiment; see further details below). In addition, data on species specific plant heights for the main experiment are available from 2002. In the main experiment, 82 grassland plots of 20 x 20 m were established from a pool of 60 species belonging to four functional groups (grasses, legumes, tall and small herbs). In May 2002, varying numbers of plant species from this species pool were sown into the plots to create a gradient of plant species richness (1, 2, 4, 8, 16 and 60 species) and functional richness (1, 2, 3, 4 functional groups). Plots were maintained by bi-annual weeding and mowing. 1. Plant height was recorded, generally, twice a year just before biomass harvest (during peak standing biomass in late May and in late August). Methodologies of measuring height have varied somewhat over the years. In earlier year the streched plant height was measured, while in later years the standing height without streching the plant was measured. Vegetative height was measured either as the height of the highest leaf or as the length of the main axis of non-flowering plants. Regenerating height was measured either as the height of the highest flower on a plant or as the height of the main axis of flowering. Sampled plants were either randomly selected in the core area of plots or along transects in defined distances. For details refer to the description of individual years. Starting in 2006, also the plots of the management experiment, that altered mowing frequency and fertilized subplots (see further details in the general description of the Jena Experiment) were sampled. 2. Species specific plant height was recorded two times in 2002: in late July (vegetative height) and just before biomass harvest during peak standing biomass in late August (vegetative and regenerative height). For each plot and each sown species in the species pool, 3 plant individuals (if present) from the central area of the plots were randomly selected and used to measure vegetative height (non-flowering indviduals) and regenerative height (flowering individuals) as stretched height. Provided are the means over the three measuremnts per plant species per plot.

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.

Ultimate and failure strengths of normal muds and serpentinite muds of ODP Leg 125 samples

Serpentinite seamounts in the Mariana forearc have been explained as diapirs rising from the Benioff zone. This hypothesis predicts that the serpentinites should have low strengths as well as low densities relative to the surrounding rocks. Drilling during Leg 125 showed that the materials forming Conical Seamount in the Mariana forearc and Torishima Forearc Seamount in the Izu-Bonin forearc are water-charged serpentinite muds of density <2 g/cm**3. Wykeham-Farrance torsion-vane tests showed that they are plastic solids with a rheology that bears many similarities to the idealized Cam clay soil model and is well described by critical-state soil mechanics. The serpentinite muds have ultimate strengths of 1.3 to 273.7 kPa and yield strengths of approximately 1.0 to 50 kPa. These muds thus are orders of magnitude weaker than salt and are, in fact, comparable in density and strength to common deep-sea clay muds. Such weak and low-density materials easily become diapiric. Serpentinite muds from the summit of Conical Seamount are weaker and more ductile than those on its flanks or on Torishima Forearc Seamount. Moreover, the summit muds do not contain the pronounced pure- and simple-shear fabrics that characterize those on the seamount flanks. The seamounts are morphologically similar to shield volcanoes, and anastomosing serpentinite debris flows descending from their summits are similar in map view to pahoehoe flows. These morphologic features, together with the physical properties of the muds and their similarities to other oceanic muds and the geochemistry of the entrained waters, suggest that many forearc serpentinite seamounts are gigantic (10-20 km wide, 1.5-2.0 km high) mud volcanoes that formed by the eruption of highly liquid serpentinite muds. Torishima Forearc Seamount, which is blanketed by more ìnormalî pelagic/volcaniclastic sediment, has probably been inactive since the Miocene. Conical Seamount, which seems to consist entirely of serpentinite mud and is venting fresh water of unusual chemistry from its summit, is presently active. Muds from the flanks of Conical Seamount are stronger and more brittle than those from the summit site, and muds from Torishima Forearc Seamount are stronger yet; this suggests that the serpentinite debris flows are compacted and dewatered as they mature. The shear fabrics probably result from downslope creep and flow, but may also be inherited.

El contrato territorial en España : Régimen jurídico y grado de implementación

El contrato territorial es una figura jurídica de aparición reciente destinada a promover el desarrollo sostenible del medio rural. Mediante él, se busca concretar el potencial de una explotación agropecuaria para proveer ciertas funciones sociales y ambientales (no tradicionales) tendientes a un desarrollo rural sostenible. A cambio de estas externalidades positivas, la explotación agropecuaria es compensada. En España, el contrato territorial ha surgido a la luz de dos ámbitos programáticos diferentes: al amparo de la legislación comunitaria europea y de las normas dictadas en su consecuencia a nivel nacional por un lado, y al abrigo de normas estrictamente de origen nacional, por el otro. Por el momento, sólo seis Comunidades Autónomas se han animado a implementarlo; sin embargo, de cara al nuevo Real Decreto 1336/2011 que regula las bases comunes del contrato territorial se espera mayor coherencia, eficiencia y utilización en el uso de esta herramienta

Proceso de institucionalización de la agricultura familiar y nuevo referencial para el desarrollo rural en la Argentina

Este artículo pone en relieve las ideas y los intereses políticos y económicos que condujeron a la reciente institucionalización de la agricultura familiar en la Argentina. Este sector, que fue motor de la primera agriculturización de la Argentina, había perdido toda representación a partir de la centralidad que tuvo el desarrollo tecnológico desde mediados de los años '70. Se analiza el proceso que relegitimó esta categoría socio-política y productiva y se presentan los dispositivos que muestran la consecuente transformación de la acción pública. El paso de una política social y paliativa hacia una políticade sectorización de la agricultura familiar refleja la transformación del referencial de desarrollo rural y las nuevas representaciones del sector agrícola en la Argentina y más ampliamente en el Cono Sur. Así, se reconstituye una representación de la agricultura familiar que identifica y reconoce la dimensión multifuncional de su actividad productiva. Esto conduce a una fragmentación del sector agrícola en dos referenciales: uno centrado en la agricultura familiar y otro centrado en la agricultura empresarial.

Proceso de institucionalización de la agricultura familiar y nuevo referencial para el desarrollo rural en la Argentina

Este artículo pone en relieve las ideas y los intereses políticos y económicos que condujeron a la reciente institucionalización de la agricultura familiar en la Argentina. Este sector, que fue motor de la primera agriculturización de la Argentina, había perdido toda representación a partir de la centralidad que tuvo el desarrollo tecnológico desde mediados de los años '70. Se analiza el proceso que relegitimó esta categoría socio-política y productiva y se presentan los dispositivos que muestran la consecuente transformación de la acción pública. El paso de una política social y paliativa hacia una políticade sectorización de la agricultura familiar refleja la transformación del referencial de desarrollo rural y las nuevas representaciones del sector agrícola en la Argentina y más ampliamente en el Cono Sur. Así, se reconstituye una representación de la agricultura familiar que identifica y reconoce la dimensión multifuncional de su actividad productiva. Esto conduce a una fragmentación del sector agrícola en dos referenciales: uno centrado en la agricultura familiar y otro centrado en la agricultura empresarial.

El contrato territorial en España : Régimen jurídico y grado de implementación

El contrato territorial es una figura jurídica de aparición reciente destinada a promover el desarrollo sostenible del medio rural. Mediante él, se busca concretar el potencial de una explotación agropecuaria para proveer ciertas funciones sociales y ambientales (no tradicionales) tendientes a un desarrollo rural sostenible. A cambio de estas externalidades positivas, la explotación agropecuaria es compensada. En España, el contrato territorial ha surgido a la luz de dos ámbitos programáticos diferentes: al amparo de la legislación comunitaria europea y de las normas dictadas en su consecuencia a nivel nacional por un lado, y al abrigo de normas estrictamente de origen nacional, por el otro. Por el momento, sólo seis Comunidades Autónomas se han animado a implementarlo; sin embargo, de cara al nuevo Real Decreto 1336/2011 que regula las bases comunes del contrato territorial se espera mayor coherencia, eficiencia y utilización en el uso de esta herramienta

Proceso de institucionalización de la agricultura familiar y nuevo referencial para el desarrollo rural en la Argentina

Este artículo pone en relieve las ideas y los intereses políticos y económicos que condujeron a la reciente institucionalización de la agricultura familiar en la Argentina. Este sector, que fue motor de la primera agriculturización de la Argentina, había perdido toda representación a partir de la centralidad que tuvo el desarrollo tecnológico desde mediados de los años '70. Se analiza el proceso que relegitimó esta categoría socio-política y productiva y se presentan los dispositivos que muestran la consecuente transformación de la acción pública. El paso de una política social y paliativa hacia una políticade sectorización de la agricultura familiar refleja la transformación del referencial de desarrollo rural y las nuevas representaciones del sector agrícola en la Argentina y más ampliamente en el Cono Sur. Así, se reconstituye una representación de la agricultura familiar que identifica y reconoce la dimensión multifuncional de su actividad productiva. Esto conduce a una fragmentación del sector agrícola en dos referenciales: uno centrado en la agricultura familiar y otro centrado en la agricultura empresarial.

El contrato territorial en España : Régimen jurídico y grado de implementación

El contrato territorial es una figura jurídica de aparición reciente destinada a promover el desarrollo sostenible del medio rural. Mediante él, se busca concretar el potencial de una explotación agropecuaria para proveer ciertas funciones sociales y ambientales (no tradicionales) tendientes a un desarrollo rural sostenible. A cambio de estas externalidades positivas, la explotación agropecuaria es compensada. En España, el contrato territorial ha surgido a la luz de dos ámbitos programáticos diferentes: al amparo de la legislación comunitaria europea y de las normas dictadas en su consecuencia a nivel nacional por un lado, y al abrigo de normas estrictamente de origen nacional, por el otro. Por el momento, sólo seis Comunidades Autónomas se han animado a implementarlo; sin embargo, de cara al nuevo Real Decreto 1336/2011 que regula las bases comunes del contrato territorial se espera mayor coherencia, eficiencia y utilización en el uso de esta herramienta

Proceso de institucionalización de la agricultura familiar y nuevo referencial para el desarrollo rural en la Argentina

Este artículo pone en relieve las ideas y los intereses políticos y económicos que condujeron a la reciente institucionalización de la agricultura familiar en la Argentina. Este sector, que fue motor de la primera agriculturización de la Argentina, había perdido toda representación a partir de la centralidad que tuvo el desarrollo tecnológico desde mediados de los años '70. Se analiza el proceso que relegitimó esta categoría socio-política y productiva y se presentan los dispositivos que muestran la consecuente transformación de la acción pública. El paso de una política social y paliativa hacia una políticade sectorización de la agricultura familiar refleja la transformación del referencial de desarrollo rural y las nuevas representaciones del sector agrícola en la Argentina y más ampliamente en el Cono Sur. Así, se reconstituye una representación de la agricultura familiar que identifica y reconoce la dimensión multifuncional de su actividad productiva. Esto conduce a una fragmentación del sector agrícola en dos referenciales: uno centrado en la agricultura familiar y otro centrado en la agricultura empresarial.