San Luis : Del empleo industrial al refugio estatal : Cambios y desplazamientos en la estructura ocupacional

A partir de la implementación de las leyes de promoción industrial, en la Provincia de San Luis se configuró una estructura sectorial del empleo con características particulares respecto de la del resto del país. En efecto, hasta la década de 1990, el sector secundario de la economía concentraba aproximadamente el 50 de los ocupados. Sin embargo, desde 1991 este escenario se modifica y aumentan los ocupados en el sector terciario de la economía. La pérdida de peso de la industria como generadora de empleo no fue compensada por un incremento de otros sectores productivos: las ramas que muestran un comportamiento expansivo son Servicios y Sector Público. Como resultado de estos desplazamientos, se modificaron también la estructura de las ocupaciones y las calificaciones requeridas: quienes se habían capacitado laboralmente trabajando en la industria se encuentran hoy en un escenario en el cual sus calificaciones han perdido valor en un mercado que ahora demanda distintos saberes y capacidades. Frente a esto, el empleo estatal y las ocupaciones de baja calificación en el sector Servicios configuran un refugio, una alternativa a la desocupación. Este trabajo analiza los cambios, rupturas y continuidades en la estructura ocupacional de la Provincia de San Luis a partir de datos provenientes de los Censos Nacionales de Población y Vivienda y de la Encuesta Permanente de Hogares

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

Proyecto de Investigación. Aproximaciones teóricas. Identidades en juego: prácticas lúdicas en jóvenes mapuches

El siguiente artículo tiene dos lecturas: una primera parte en la que expongo de manera sucinta, algunas razones por las cuales considero necesario llevar a cabo éste proyecto de investigación, lo que podría ser leído, como el área de interés. En segundo término, me sumerjo en cuestiones más complejas, concretamente, desde que perspectivas es posible enmarcar conceptualmente, algunas de las categorías que sustenten teóricamente el "proyecto" de investigación. Muchos conceptos provienen de diferentes autores, por lo que éste eclecticismo, intentará ser compensado con precisiones teóricas mas ajustadas en una fase posterior, el marco teórico de la tesis. En ésta propuesta, la cuestión central, es comprender de qué manera, los jóvenes de ascendencia mapuche, logran a través de diferentes prácticas lúdicas significar diferentes procesos de identificaciones culturales. Por tal motivo, algunas referencias, a los conceptos de: Alteridad-otredad, Identidad Cultural, Prácticas, Representaciones, Juego, aparecen como categorías necesarias a ser explicitadas en el marco del trabajo. Aquí, por cuestiones de espacio haré un desarrollo dispar, priorizando algunas sobre otras. La investigación se vinculará, a la vertiente cualitativa-etnográfica, pues, éste parece ser el camino mas adecuado para captar la comprensión de un fenómeno social, desde la perspectiva de los "actores" ("agentes" o "sujetos sociales)" (Guber, R. 2001:20).

San Luis : Del empleo industrial al refugio estatal : Cambios y desplazamientos en la estructura ocupacional

A partir de la implementación de las leyes de promoción industrial, en la Provincia de San Luis se configuró una estructura sectorial del empleo con características particulares respecto de la del resto del país. En efecto, hasta la década de 1990, el sector secundario de la economía concentraba aproximadamente el 50 de los ocupados. Sin embargo, desde 1991 este escenario se modifica y aumentan los ocupados en el sector terciario de la economía. La pérdida de peso de la industria como generadora de empleo no fue compensada por un incremento de otros sectores productivos: las ramas que muestran un comportamiento expansivo son Servicios y Sector Público. Como resultado de estos desplazamientos, se modificaron también la estructura de las ocupaciones y las calificaciones requeridas: quienes se habían capacitado laboralmente trabajando en la industria se encuentran hoy en un escenario en el cual sus calificaciones han perdido valor en un mercado que ahora demanda distintos saberes y capacidades. Frente a esto, el empleo estatal y las ocupaciones de baja calificación en el sector Servicios configuran un refugio, una alternativa a la desocupación. Este trabajo analiza los cambios, rupturas y continuidades en la estructura ocupacional de la Provincia de San Luis a partir de datos provenientes de los Censos Nacionales de Población y Vivienda y de la Encuesta Permanente de Hogares

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

Proyecto de Investigación. Aproximaciones teóricas. Identidades en juego: prácticas lúdicas en jóvenes mapuches

El siguiente artículo tiene dos lecturas: una primera parte en la que expongo de manera sucinta, algunas razones por las cuales considero necesario llevar a cabo éste proyecto de investigación, lo que podría ser leído, como el área de interés. En segundo término, me sumerjo en cuestiones más complejas, concretamente, desde que perspectivas es posible enmarcar conceptualmente, algunas de las categorías que sustenten teóricamente el "proyecto" de investigación. Muchos conceptos provienen de diferentes autores, por lo que éste eclecticismo, intentará ser compensado con precisiones teóricas mas ajustadas en una fase posterior, el marco teórico de la tesis. En ésta propuesta, la cuestión central, es comprender de qué manera, los jóvenes de ascendencia mapuche, logran a través de diferentes prácticas lúdicas significar diferentes procesos de identificaciones culturales. Por tal motivo, algunas referencias, a los conceptos de: Alteridad-otredad, Identidad Cultural, Prácticas, Representaciones, Juego, aparecen como categorías necesarias a ser explicitadas en el marco del trabajo. Aquí, por cuestiones de espacio haré un desarrollo dispar, priorizando algunas sobre otras. La investigación se vinculará, a la vertiente cualitativa-etnográfica, pues, éste parece ser el camino mas adecuado para captar la comprensión de un fenómeno social, desde la perspectiva de los "actores" ("agentes" o "sujetos sociales)" (Guber, R. 2001:20).

San Luis : Del empleo industrial al refugio estatal : Cambios y desplazamientos en la estructura ocupacional

A partir de la implementación de las leyes de promoción industrial, en la Provincia de San Luis se configuró una estructura sectorial del empleo con características particulares respecto de la del resto del país. En efecto, hasta la década de 1990, el sector secundario de la economía concentraba aproximadamente el 50 de los ocupados. Sin embargo, desde 1991 este escenario se modifica y aumentan los ocupados en el sector terciario de la economía. La pérdida de peso de la industria como generadora de empleo no fue compensada por un incremento de otros sectores productivos: las ramas que muestran un comportamiento expansivo son Servicios y Sector Público. Como resultado de estos desplazamientos, se modificaron también la estructura de las ocupaciones y las calificaciones requeridas: quienes se habían capacitado laboralmente trabajando en la industria se encuentran hoy en un escenario en el cual sus calificaciones han perdido valor en un mercado que ahora demanda distintos saberes y capacidades. Frente a esto, el empleo estatal y las ocupaciones de baja calificación en el sector Servicios configuran un refugio, una alternativa a la desocupación. Este trabajo analiza los cambios, rupturas y continuidades en la estructura ocupacional de la Provincia de San Luis a partir de datos provenientes de los Censos Nacionales de Población y Vivienda y de la Encuesta Permanente de Hogares

Distribution of calcareous nannofossils in upper Cretaceous and Cenozoic sediments of the Kerguelen Plateau

ODP Leg 119 drilled 11 sites on the Kerguelen Plateau (southern Indian Ocean) and Prydz Bay (East Antarctica). Upper Pliocene through Quaternary sediments were recovered at Site 736 on the northern Kerguelen Plateau; calcareous nannofossils occurred in only a few samples. Over 700 m of middle Eocene through Quaternary sediments was cored at Site 737 on the northern Kerguelen Plateau, and calcareous nannofossils are abundant in the middle Eocene through the middle Miocene sediments. Nearly 500 m of sediments ranging from the lower Turanian to the Quaternary was recovered at Site 738 on the southern Kerguelen Plateau; calcareous nannofossils are abundant from the Miocene downward. Calcareous nannofossils are also abundant in the upper Eocene through Miocene section from Site 744 on the southern Kerguelen Plateau. Except for Core 119-746A-13H, the Neogene sequences drilled at deep-water Sites 745 and 746 off the southern Kerguelen Plateau are devoid of calcareous nannofossils. Occurrences of calcareous nannofossils were generally rare and sporadic at Sites 739 and 742 in Prydz Bay and suggest that the diamictite sequences recovered is as old as middle Eocene-early Oligocene age. Other sites drilled in Prydz Bay (Sites 740, 741, and 743) did not yield calcareous nannofossils. Species diversity of calcareous nannofossils was low (about a dozen) in the southern Indian Ocean in the Late Cretaceous. High-latitude nanno floral characteristics are apparent after the Cretaceous/Tertiary boundary extinctions. Cold climatic conditions limited Oligocene calcareous nannofossil assemblages to fewer than a dozen species, and extinctions of species generally were not compensated by originations of new species. Only a few species of calcareous nannofossils were found in the Miocene sequences, in which Coccolithuspelagicus and one or two species of Reticulofenestra exhibit extreme (0%-100%) fluctuations in assemblage dominance, and these fluctuations may reflect rapid fluctuations in the surface-water temperatures. Further deterioration of climate in the late Neogene essentially excluded calcareous nannoplankton from the Southern Ocean. Significantly warmer water conditions during part of the early-middle Pleistocene were inferred by a few lower-middle Pleistocene calcareous nannofossil species found on the Kerguelen Plateau. The calcareous nannofossil zonation of Roth (1978 doi:10.2973/dsdp.proc.44.134.1978) can be applied to the Upper Cretaceous section recovered at Site 738, and the zonation of Okada and Bukry (1980 doi:10.1016/0377-8398(80)90016-X) can be applied without much difficulty to the Paleocene to middle Eocene sequences from the Kerguelen Plateau. However, some conventional upper Paleogene markers are not useful for southern high latitudes, whereas a few nonconventional species events are useful for subdividing the upper Paleogene sequences. The latter species events include the first occurrence (FO) of Reticulofenestra reticulata, the FO and last occurrence (LO) of Reticulofenestra oamaruensis, the LO of Isthmolithus recurvus, and the LO of Chiasmolithus altus. As the Neogene sequences from the southern Indian Ocean contain only a few long-ranging, cold-water species, or are devoid of coccoliths, calcareous nannofossil zonations remain virtually unworkable for the Neogene in the high-latitude southern Indian Ocean as in other sectors of the Southern Ocean.

Absorption coefficients of particulate matter and chlorophyll a concentrations at time series station OLIPAC

Spectral absorption coefficients of total particulate matter ap (lambda) were determined using the in vitro filter technique. The present analysis deals with a set of 1166 spectra, determined in various oceanic (case 1) waters, with field chl a concentrations ([chl]) spanning 3 orders of magnitude (0.02-25 mg/m**3). As previously shown [Bricaud et al., 1995, doi:10.1029/95JC00463] for the absorption coefficients of living phytoplankton a phi (lamda), the ap (labda) coefficients also increase nonlinearly with [chl]. The relationships (power laws) that link ap (lambda) and a phi (lambda) to [chl] show striking similarities. Despite large fluctuations, the relative contribution of nonalgal particles to total absorption oscillates around an average value of 25-30% throughout the [chl] range. The spectral dependence of absorption by these nonalgal particles follows an exponential increase toward short wavelengths, with a weakly variable slope (0.011 ± 0.0025/nm). The empirical relationships linking ap (lambda) to ([chl]) can be used in bio-optical models. This parameterization based on in vitro measurements leads to a good agreement with a former modeling of the diffuse attenuation coefficient based on in situ measurements. This agreement is worth noting as independent methods and data sets are compared. It is stressed that for a given ([chl]), the ap (lambda) coefficients show large residual variability around the regression lines (for instance, by a factor of 3 at 440 nm). The consequences of such a variability, when predicting or interpreting the diffuse reflectance of the ocean, are examined, according to whether or not these variations in ap are associated with concomitant variations in particle scattering. In most situations the deviations in ap actually are not compensated by those in particle scattering, so that the amplitude of reflectance is affected by these variations.

Surface carbon dioxide measurements between 1994 and 2004 at site Estoc

Seasonal patterns in hydrography, partial pressure of CO2, fCO2, pHt, total alkalinity, AT, total dissolved inorganic carbon, CT, nutrients, and chlorophyll a were measured in surface waters on monthly cruises at the European Station for Time Series in the Ocean at the Canary Islands (ESTOC) located in the northeast Atlantic subtropical gyre. With over 5 years of oceanographic data starting in 1996, seasonal and interannual trends of CO2 species and air-sea exchange of CO2 were determined. Net CO2 fluxes show this area acts as a minor source of CO2, with an average outgassing value of 179 mmol CO2/m**2 yr controlled by the dominant trade winds blowing from May to August. The effect of short-term wind variability on the CO2 flux has been addressed by increasing air-sea fluxes by 63% for 6-hourly sampling frequency. The processes governing the monthly variations of CT have been determined. From March to October, when CT decreases, mixing at the base of the mixed layer (11.5 ± 1.5 mmol/m**3) is compensated by air-sea exchange, and a net organic production of 25.5 ± 5.7 mmol/m**3 is estimated. On an annual scale, biological drawdown accounts for the decrease in inorganic carbon from March to October, while mixing processes control the CT increase from October to the end of autumn. After removing seasonality variability, fCO2sw increases at a rate of 0.71 ± 5.1 µatm/yr, and as a response to the atmospheric trend, inorganic carbon increases at a rate of 0.39 ± 1.6 µmol/kg yr.

(Table 1) Results of measurements of production characteristics of phytoplankton and some physical parameters of the environment in the northeastern Norwegian Sea in July 1995

From July 4 to 18,1995 surface chlorophyll a concentrations (C_cs) and integral primary production (C_ps) were studied in the northeastern part of the Norwegian Sea (73°42'N; 13°16'E), over a test area where an accident of the nuclear submarine Komsomolets had taken place. It was found that during this interval C_cs decreased by factor of about 3.3 (from 0.78 to 0.24 mg/m**3); average chlorophyll concentration within the photo-synthetic layer (C_cl) decreased by factor of about 3.5 (from 0.97 to 0.28 mg/m**3). The value of C_ps in the water column varied slightly (from 445 to 539 mg C/m**2 per day), since decrease in C_cl was compensated both by 1.5-fold growth of the photosynthetic layer thickness (from 40 to 60 m) and by 2.1-fold increase in its average assimilation number (from 0.58 to 1.20 mg C/mg chl a per hour). Monthly averages of C_ps were obtained from published data on seasonal C_cs changes and on the level of incident solar irradiation. They were found to be less than 100 mg C/m**2 per day in March and October and 100-500 mg C/m**2 per day in April-June. Annual primary production calculated from above values was equal to 105 g C/m**2.

Site characteristics and ice speed at four sites on Kangiata Nunata Sermia glacier, southwest Greenland

We present subdaily ice flow measurements at four GPS sites between 36 and 72 km from the margin of a marine-terminating Greenland outlet glacier spanning the 2009 melt season. Our data show that >35 km from the margin, seasonal and shorter-time scale ice flow variations are controlled by surface melt-induced changes in subglacial hydrology. Following the onset of melting at each site, ice motion increased above background for up to 2 months with resultant up-glacier migration of both the onset and peak of acceleration. Later in our survey, ice flow at all sites decreased to below background. Multiple 1 to 15 day speedups increased ice motion by up to 40% above background. These events were typically accompanied by uplift and coincided with enhanced surface melt or lake drainage. Our results indicate that the subglacial drainage system evolved through the season with efficient drainage extending to at least 48 km inland during the melt season. While we can explain our observations with reference to evolution of the glacier drainage system, the net effect of the summer speed variations on annual motion is small (~1%). This, in part, is because the speedups are compensated for by slowdowns beneath background associated with the establishment of an efficient subglacial drainage system. In addition, the speedups are less pronounced in comparison to land-terminating systems. Our results reveal similarities between the inland ice flow response of Greenland marine- and land-terminating outlet glaciers.

Gill tissue masses and oxygen consumption of Gobionotothen gibberifrons, Notothenia coriiceps and Zoarces viviparus

Mechanisms responsive to hypercapnia (elevated CO2 concentrations) and shaping branchial energy turnover were investigated in isolated perfused gills of two Antarctic Notothenioids (Gobionotothen gibberifrons, Notothenia coriiceps). Branchial oxygen consumption was measured under normo- versus hypercapnic conditions (10,000 ppm CO2) at high extracellular pH values. The fractional costs of ion regulation, protein and RNA synthesis in the energy budgets were determined using specific inhibitors. Overall gill energy turnover was maintained under pH compensated hypercapnia in both Antarctic species as well as in a temperate zoarcid (Zoarces viviparus). However, fractional energy consumption by the examined processes rose drastically in G. gibberifrons (100-180%), and to a lesser extent in N. coriiceps gills (7-56%). In conclusion, high CO2 concentrations under conditions of compensated acidosis induce cost increments in epithelial processes, however, at maintained overall rates of branchial energy turnover.

Sedimentary facies, clay mineralogy and geochemistry of the Paleogene sediments of ODP Site 105-647

Claystones immediately overlying the early Eocene age ocean-floor basalt, cored at Ocean Drilling Program (ODP) Site 647, underwent hydrothermal and thermal alterations originating from the basalt, which resulted in changes in both the mineralogical and chemical composition of the sediments. Chlorites and higher magnesium and iron concentrations were found in the lowermost sediment sequence. Upcore, changes in the bulk chemical composition of the sediments become smaller, when compensated for variations in the carbonate content originating from biogenic and authigenic components. Chlorite disappears upcore, but still only part of the swelling clay minerals have survived the thermal influence. Thirty meters above the basalt, the clay mineralogy and chemical composition become uniform throughout the Paleogene section. Iron-rich smectites (i.e., nontronitic types), totally dominate the clay mineral assemblage. Biogenic components, responsible for the dominant part of the calcite and cristobalite contents, vary in amount in the upper part, and so do the authigenic carbonate and sulfide contents. Detrital components, such as kaolinite, illite, quartz, and feldspars, make up a very small proportion of the sediment record. The nontronitic smectites are believed to be authigenic, formed by a supply of iron from the continuous formation of ocean-floor basalt in the ridge area that reacted with the detrital and biogenic silicates and alumina silicates.

Pollen records and lithology of profiles from Lobsigensee, Switzerland

Lobsigensee is a small kettle hole lake 15 km north-west of Bern on the Swiss Plateau, at an altitude of 514 m asl. Its surface is 2ha today, its maximum depth 2.7 m; it has no inlet and the overflow functions mainly during snow melting. The area was covered by Rhone ice during the Last Glaciation (map in Fig.2). Local geology, climate and vegetation are summarized in Figure 3A-C, the history of settlement in Figures 5-7. In order to reconstruct the vegetational and environmental history of the lake and its surroundings pollen analysis and other bio- and isotope stratigraphies were applied to twelve profiles cored across the basin with modified Livingstone corers (Fig.3 D). (1) The standard diagram: The central core LQ-90 is described as the standard pollen diagram (Chapter 3) with 10 local pollen assemblage zones of the Late-Glacial (local PAZ Ll to Ll0, from about 16'000(7) to 10'000 years BP) and 20 PAZ of the Holocene (local PAZ L11 to L30), see Figs. 8-10 and 20-24. Local PAZ L 1 to L3 are in the Late-Glacial clay and record the vegetational development after the ice retreat: L1 shows very low pollen concentration and high Pinus percentages due to long-distance transport and reworking; the latter mechanism is corroborated by the findings of thermophilous and pre-Quaternary taxa. Local PAZ L2 has a high di versi ty of non-arboreal pollen (NAP) and reflects the Late-Glacial steppe rich in heliophilous species. Local PAZ L3 is similar but additionally rich in Betula nana and Sal1x, thus reflecting a "shrub tundra". The PAZ L1 to L3 belong to the Oldest Dryas biozone. Local PAZ L4 to L 10 are found in the gyttja of the profundal or in the lake marl of the littoral and record the Late-Glacial forests. L4 is the shrub phase of reforestation with very high Junlperus and rapidly increasing Betula percentages. L5 is the PAZ with a first, L7 with a second dominance of tree-birches, separated by L6 showing a depression in the Betula curve. L4 to L7 can be assigned to the Balling biozone. Possible correlation of the Betula depression to the Older Dryas biozone is discussed. In local PAZ L8 Plnus immigrates and expands. L9 shows a facies difference in that Plnus dominates over Betula in littoral but not in profundal spectra. L8 and L9 belong to the Allerod biozone. In its youngest part the volcanic ash from Laach/Eifel is regularly found (11,000 BP). The local PAZ Ll0 corresponds to the Younger Dryas blozone. The merely slight increase of the NAP indicates that the pine forests of the lowland were not strongly affected by a cooler climate. In order to evaluate the significance of the littoral accumulation of coniferous pollen the littoral profile LQ-150 is compared to the profundal. Radiocarbon stratigraphies derived from different materials are presented in Figures 13 and 14 and in Tables 2 and 3. The hard-water errors in the gyttja samples and the carbonate samples are similar. The samples of terrestrial plant macrofossils are not affected by hard-water errors. Two plateaux of constant age appear in the age-depth relationship; their consequence for biostratigraphy as well as pollen concentration and influx diagrams are discussed. Radiocarbon ages of the Late-Glacial pollen zones are shown in Table 10. The Holocene vegetational history is recorded in the local PAZ L 11 to L30. After a Preboreal (PAZ L11) dominated by pine and birch the expansions of Corylus, Ulmus and Quercus are very rapid. Among these taxa Corylus dominates dur ing the Boreal (PAZ L 12 and L 1 3), whereas the components of the mixed oak forest dominate in the Older Atlantic (PAZ L14 to L16). In the Younger Atlantic (PAZ L 17 to L 19) Fagus and Alnus play an increasing, the mixed oak forest a decreasing role. During the period of local PAZ L19 Neolithic settlers lived on the shore of Lobsigensee. During the Subboreal (PAZ L20 and L21) and the Older Subatlantic (L22 to L25) strong fluctuations of Fagus and often antagonistic peaks of NAP, Alnus, Betula and Corylus can be interpreted as signs of human impact on vegetation. L23 is characterized not only by high values of NAP (especially apophytes and anthropochorous species) but also by the appearance of Juglans, Castanea and Secale which point to the Roman colonization of the area. For a certain period during the Younger Subatlantic (PAZ L26 to L30) the lake was used for retting hemp (Cannabis). Later the dominance of Quercus pollen indicates the importance of wood pastures. The youngest sediments reflect the wide-spread agricultural grass lands and the plantation of Pinus and Picea. Radiocarbon dates for the Holocene are given in Figure 23 and Table 4, the extrapolated ages of the Holocene pollen zones in Table 15. (2) The cross sections: Figures 25 and 26 give a summary of the litho- and palynostratigraphy of the two cross sections. Based on 11 Late-Glacial and 9 Holocene pollen diagrams (in addition to the standard ones), the consistency of the criteria for the definition of the pollen zones is examined in Tables 7 and 8 for the Late-Glacial and in Tables 11 to 14 for the Holocene. Sediment thicknesses across the basin for each pollen zone are presented in these tables as well as in Figures 43 to 45 for the Late-Glacial and in Figures 59 to 65 for the Holocene. Sediment focusing can explain differences between the gyttja cores of the profundal. Focusing is more than compensated for through "stretching" by carbonate precipitation on the littoral terrace. Pollen influx to the cross section are discussed (Chapters 4.1.5. and 4.2.3.). (3) The regional pollen zones: Based on some selected sites between Lake Geneva and Lake Constance regional pollen zones are proposed (Table 16, 17 and 19). (4) Paleoecology: Climatic change in the Late-Glacial can be inferred from Coleoptera, Trichoptera, Chironomidae and d18O of carbonates: a distinct warming is recorded around 12' 600 BP and around 10' 000 BP. The Younger Dryas biozone (10'700-10'000 BP) was the only cooling found in the Late-Glacial. The Betula depression often correlated wi th the Older Dryas biozone was possibl not colder but dryer than the previous period. During the Holocene the lowland site is not very sensitive to the minor climatic changes. Table 22 summarizes climatic and trophic changes before 8'000 BP as deduced from various biostratigraphies studied by a number of authors. Ostracods, Chironomids and fossil pigments indicate that anoxic conditions prevailed during the BoIling (possibly meromixis). Changes in the lake level are illustrated in Figure 74. A first lake-level lowering occurred in the early Holocene (10'000 to 9'000 BP), a second during the Atlantic (about 6'800 to 5'200 BP). The first "shrinking" of the lake volume resulted in a eutrophication recorded by laminations in the profundal and by pigments of Cyanophyceae. The second fall in water level corresponds to an increase of Nymphaeaceae. Human impact can be inferred in three ways: eutrophication of the lake (since the Neolithic), changes of terrestrial vegetation by deforestations (cyclicity of Fagus, see Figures 78 to 80), and enhanced erosion (increasing sedimentation rates by inwashed clay, particularly since the Roman Colonization, see Figures 49 and 81). Summary: This paper was planned as the final report on Lobsigensee. However, a number of issues are not answered but can only be asked more precisely, for example: (1) For the two periods with the highest rates of change, Le. the Bolling and the Preboreal biozones, pollen influx may reflect vegetation dynamics. Detailed investigations of these periods in annually laminated sediments are planned. (2) Biostratigraphies other than palynostratigraphy are needed to estimate the degree of linkage or independence in the development of terrestrial and lacustrine ecosystems. Often our sampling intervals were not identical, thus influencing our temporal resolution. (3) 6180- and 14C-stratigraPhies with high resolution will elucidate the leads and lags of these dynamic periods. Plateaux of constant age in the age-depth relationship have a strong bearing on both biological and geophysical understanding of Late-Glacial and early Holocene developments. (4) Numerical methods applied to the pollen diagrams of the cross section will help to quantify the significance of similari ties and dissimilarities across a single basin (with Prof. Birks). (5) Numerical methods applied to different sites on the Swiss Plateau and on the transect across the Alps will be helpful in evaluating the influence of different environmental factors (with Prof. Birks). (6) A new map 1: 1000 with 50cm-contour lines prov ided by Prof. Zurbuchen will be combined with a grid of cores sampling the transition from lake marl to peat enabling us to calculate paleo-volumes of the lake. This is interesting for the two "shrinking periods" (in Fig. 74A numbers 2-6 and 7-10), both accompanied by eutrophication. The pal eo-volume during the Neoli thic set tlement of the Cortaillod culture linked wi th an est l.mate of trophic change derived from diatoms (Prof. Smol in prep.) could possibly give an indication of the size of the human population of this period. (7) For the period with the antagonism between Fagus peaks and ABC-peaks close collaboration between palynologists, geochemists and archeologists should enable us to determine the influence of prehistoric and historic people on vegetation (collaboration with Prof. Stockli and Prof. Herzig). (8) The core LL-75 taken with a "cold letter box" will be analysed for major and trace elements by Dr. Sturm for 210pb and 137Cs by Prof.von Gunten and for pollen. We will see if our local PAZ L30 really corresponds to the surface sediment and if the small seepage lake reflects modern pollution.