Analysis of an ancient global warming event, the Paleocene-Eocene thermal maximum, under examination from ODP Holes 113-689B and 113-690B

Spatiotemporal patterns of carbonate dissolution provide a critical constraint on carbon input during an ancient (~55.5 Ma) global warming event known as the Paleocene-Eocene thermal maximum (PETM), yet the magnitude of lysocline shoaling in the Southern Ocean is poorly constrained due to limited spatial coverage in the circum-Antarctic region. This shortcoming is partially addressed by comparing patterns of carbonate sedimentation at the Site 690 PETM reference section to those herein reconstructed for nearby Site 689. Biochemostratigraphic correlation of the two records reveals that the first ~36 ka of the carbon isotope excursion (CIE) signaling PETM conditions is captured by the Site 689 section, while the remainder of the CIE interval and nearly all of the CIE recovery are missing due to a coring gap. A relatively expanded stratigraphy and higher carbonate content at mid-bathyal Site 689 indicate that dissolution was less severe than at Site 690. Thus, the bathymetric transect delimited by these two PETM records indicates that the lysocline shoaled above Site 689 (~1,100 m) while the calcite compensation depth remained below Site 690 (~1,900 m) in the Weddell Sea region. The ensuing recovery of carbonate sedimentation conforms to a bathymetric trend best explained by gradual lysocline deepening as negative feedback mechanisms neutralized ocean acidification. Further, biochemostratigraphic evidence indicates the tail end of the CIE recovery interval at both sites has been truncated by a hiatus most likely related to vigorous production and advection of intermediate waters.

Chemical and isotope compositions of bottom sediments from ODP Leg 168, Eastern Flank of the Juan de Fuca Ridge

Ten sites were drilled in the eastern flank of the Juan de Fuca Ridge (North East Pacific) along a 100 km-long east-west transect during Leg ODP 168. This study focuses on the mineralogical and chemical study of sediments that overly basaltic basement through which seawater circulates. Silicate authigenesis was observed in the sediment layer just above basement at sites located more than 30 km from the ridge axis. This sediment alteration is particularly abundant at ODP Sites 1031 and 1029 where authigenic formation of Fe-Mg rich smectite and zeolite and the dissolution of biogenic calcite are observed. Comparison of the distribution of the alteration in the basal sediment collected along this transect suggests that diffusional transport of aqueous solutes from the basement into the overlying sediment cannot produce the mineralogical and chemical changes in the basal sediments at Sites 1031 located on a basement topographic high, and at Site 1029 located at about 50 km from the ridge axis on a buried basement area. Vertical advection of basement fluid though the sediment section is required to produce this alteration. These processes are still active at Site 1031, based on systematic variations in pore-water profiles and temperatures obtained from stable isotopic data on calcium carbonates and the nature of authigenic minerals. At Site 1029, there is no present-day advection of basement fluids though the sediment section, suggesting that this is a relic site for fluid flow.

Monthly interpolated coral d18O records from Bonaire corals

Several proxy-based and modeling studies have investigated long-term changes in Caribbean climate during the Holocene, however, very little is known on its variability on short timescales. Here we reconstruct seasonality and interannual to multidecadal variability of sea surface hydrology of the southern Caribbean Sea by applying paired coral Sr/Ca and d18O measurements on fossil annually banded Diploria strigosa corals from Bonaire. This allows for better understanding of seasonal to multidecadal variability of the Caribbean hydrological cycle during the mid- to late Holocene. The monthly resolved coral Delta d18O records are used as a proxy for the oxygen isotopic composition of seawater (d18Osw) of the southern Caribbean Sea. Consistent with modern day conditions, annual d18Osw cycles reconstructed from three modern corals reveal that freshwater budget at the study site is influenced by both net precipitation and advection of tropical freshwater brought by wind-driven surface currents. In contrast, the annual d18Osw cycle reconstructed from a mid-Holocene coral indicates a sharp peak towards more negative values in summer, suggesting intense summer precipitation at 6 ka BP (before present). In line with this, our model simulations indicate that increased seasonality of the hydrological cycle at 6 ka BP results from enhanced precipitation in summertime. On interannual to multidecadal timescales, the systematic positive correlation observed between reconstructed sea surface temperature and salinity suggests that freshwater discharged from the Orinoco and Amazon rivers and transported into the Caribbean by wind-driven surface currents is a critical component influencing sea surface hydrology on these timescales.

Entre la homogeneización moralizante y la adaptación al entorno: la escolarización bonaerense durante la última dictadura (1976-1983)

Este trabajo se propone abordar los sentidos que organizaron las políticas educativas en la provincia de buenos Aires durante la última dictadura militar. A partir del análisis de fuentes primarias, exploraremos el modo en que se combinaron inestablemente una fuerte intervención destinada a 're-moralizar' una sociedad considerada 'caótica' y una serie de medidas tendientes a 'modernizar' un sistema educativo supuestamente 'en crisis'. Argumentaremos que estas últimas se estructuraron en torno a la idea de adaptar la escolarización a las demandas del entorno y que, desde allí, la dictadura intervino en un amplio debate sobre la 'modernización educativa' en nuestro país que la había preexistido, dando cuenta del agotamiento de ciertos significados para la educación escolar e instalando una forma de procesar la 'modernización' que tendría importantes consecuencias más allá del fin del régimen.

Geochemistry, fluxes and nitrogen isotopic composition data of traps LP1 and EBC2-1 and cores GeoB4242-4 and Geo4301-1

We compare total and biogenic particle fluxes and stable nitrogen isotope ratios (d15N) at three mooring sites along a productivity gradient in the Canary Islands region with surface sediment accumulation rates and sedimentary d15N. Higher particle fluxes and sediment accumulation rates, and lower d15N were observed in the upwelling influenced eastern boundary region (EBC) compared to the oligotrophic sites north of Gran Canaria [European Station for Time-Series in the Ocean, Canary Islands (ESTOC]] and north of La Palma (LP). The impact of organic matter degradation and lateral particle advection on sediment accumulation was quantified with respect to the multi-year flux record at the ESTOC. Remineralisation of organic matter in the water column and at the sediment surface resulted in an organic carbon preservation of about 0.8% and total nitrogen preservation of about 0.4% of the estimated export production. Higher total and carbonate fluxes and accumulation rates in the lower traps and surface sediment compared to the upper traps indicated that at least 50% of the particulate matter at the ESTOC was derived from allochthonous sources. Low d15N values in the lower traps of the ESTOC and LP point to a source region influenced by coastal upwelling. We conclude from this study that the reconstruction of export production or nutrient regimes from sedimentary records in regions with strong productivity gradients might be biased due to the mixture of particles originating from autochthonous and allochthonous sources. This could result in an imprint of high productivity signatures on sedimentation processes in oligotrophic regions.

Part of the global DOC versus AOU (dissolved organic carbon/apparent oxygen utilization) data compilation, WOCE14

Total organic carbon (TOC) samples were collected at 6 stations spaced ~800 km apart in the eastern South Atlantic, from the Equator to 45°S along 9°W. Analyses were performed by high temperature catalytic oxidation (HTCO) in the base laboratory. Despite the complex advection and mixing patterns of North Atlantic and Antarctic waters with extremely different degrees of ventilation, TOC levels below 500 m are quasi-constant at 55±3 µmol C/l, pointing to the refractory nature of deep-water TOC. On the other hand, a TOC excess from 25 to 38 g C/m**2 is observed in the upper 100 m of the permanently stratified nutrient-depleted Equatorial, Subequatorial and Subtropical upper ocean, where vertical turbulent diffusion is largely prevented. Conversely, TOC levels in the nutrient-rich upper layer of the Subantarctic Front only exceeds 9 g C/m**2 the deep-water baseline. As much as 70% of the TOC variability in the upper 500 m is due to simple mixing of reactive TOC formed in the surface layer and refractory TOC in deep ocean waters, with a minor contribution (13%) to oxygen consumption in the prominent subsurface AOU maximum at 200-400 m depth.

Malvinas a 30 años del conflicto : Un análisis sobre las propuestas de enseñanza en formato digital

Este artículo trata de definir los límites y posibilidades de los nuevos textos digitales en la enseñanza de la historia, especialmente de algunas propuestas didácticas producidas por el gobierno nacional, cuyo contenido versa sobre la guerra de Malvinas. ¿Cuáles son los nuevos significados que este tipo de textos digitales aportan a la enseñanza y el aprendizaje de la Guerra de las Malvinas? ¿Qué discursos y narrativas sobre Malvinas se presentan explícitos e implícitos en estos textos digitales? ¿Hay algún cambio entre estas narraciones que emergen en el 30 aniversario de la guerra en comparación con las narrativas anteriores? Son algunas de las preguntas que tratamos de resolver, a pesar de que los textos en formato digital para la enseñanza de la historia, parecen ser muy caóticos y poseen otro régimen de producción, lectura y propiedad, diferente al de los materiales curriculares impresos. Como primera aproximación al análisis podemos observar como las políticas educativas nacionales actuales en Argentina refuerzan el discurso de los derechos y la soberanía sobre las islas, introduciendo además, elementos nuevos que buscan un acercamiento emocional a la causa y desdibujan en parte, la enseñanza de la complejidad de Malvinas

Consideraciones sobre el desarrollo de la literatura pesimista egipcia en el Reino Medio

Durante el Reino Medio egipcio asistiremos al desarrollo de la denominada literatura pesimista, única por su contenido y sus mensajes, que se caracterizó por mostrar un mundo en caos, donde los ideales, los valores y las representaciones del orden en la tierra se encontraban alterados. Fueron los primeros textos que plantearon una visión alterada del orden, con el objetivo de mostrar cómo sería la vida sin un Estado fuerte que ordene y organice a la sociedad. Se analizarán obras las Admoniciones de Ipuwer, la Disputa de un hombre con su ba, la Profecía de Neferty y las Lamentaciones de Khakheperrasnebu

Planktic foraminiferal Mg/Ca and oxygen isotopes, plus estimated d18Oseawater and ice volume corrected d18Oseawater for the past 35000 years of sediment core GeoB10069-3

Evidence from geologic archives suggests that there were large changes in the tropical hydrologic cycle associated with the two prominent northern hemisphere deglacial cooling events, Heinrich Stadial 1 (HS1; ~19 to 15 kyr BP; kyr BP = 1000 yr before present) and the Younger Dryas (~12.9 to 11.7 kyr BP). These hydrologic shifts have been alternatively attributed to high and low latitude origin. Here, we present a new record of hydrologic variability based on planktic foraminifera-derived d18O of seawater (d18Osw) estimates from a sediment core from the tropical Eastern Indian Ocean, and using 12 additional d18Osw records, construct a single record of the dominant mode of tropical Eastern Equatorial Pacific and Indo-Pacific Warm Pool (IPWP) hydrologic variability. We show that deglacial hydrologic shifts parallel variations in the reconstructed interhemispheric temperature gradient, suggesting a strong response to variations in the Atlantic Meridional Overturning Circulation and the attendant heat redistribution. A transient model simulation of the last deglaciation suggests that hydrologic changes, including a southward shift in the Intertropical Convergence Zone (ITCZ) which likely occurred during these northern hemisphere cold events, coupled with oceanic advection and mixing, resulted in increased salinity in the Indonesian region of the IPWP and the eastern tropical Pacific, which is recorded by the d18Osw proxy. Based on our observations and modeling results we suggest the interhemispheric temperature gradient directly controls the tropical hydrologic cycle on these time scales, which in turn mediates poleward atmospheric heat transport.

Stable isotope record and distribution of foraminifera in sediment core GeoB3004-1

Fluctuations in the abundance of selected foraminiferal indicator species and diversity allowed the reconstruction of changes in deepwater oxygenation and monsoon-driven organic matter fluxes in the deep western Arabian Sea during the last 190 kyr. Times of maximum surface production coincide with periods of intensified SW monsoon as shown by the abundance of Globigerina bulloides and enhanced carbonate corrosion. Benthic ecosystem variability in the deep Arabian Sea is not exclusively driven by variations in monsoonal upwelling and related organic matter supply to the seafloor but also by changes in deepwater ventilation. Deepening of the base of the oxygen minimum zone (OMZ) below 1800 m water depth is strongly coherent on the precessional band but lags proxies of SW monsoon strength by 4 to 6 kyr. The "out-of-phase" relationship between OMZ deepening and maximum SW monsoon strength is explained by temporal changes in the advection of oxygen-rich deepwater masses of North Atlantic and Antarctic origin. This process affected the remineralization and burial efficiency of organic matter in the deep Arabian Sea, resulting in the observed phase lag between maximum monsoon strength and organic carbon preservation.

Sea surafce temperature reconstruction for sediment core SU81-18

Reconstructing the impact of Heinrich events outside the main belt of ice rafting is crucial to understanding the underlying causes of these abrupt climatic events. A high-resolution study of a marine sediment core from the Iberian margin demonstrates that this midlatitude area was strongly affected both by cooling and advection of low-salinity arctic water masses during the last three Heinrich events. These paleoclimatic time series reveal the internal complexity of each of the last three Heinrich events and illustrate the value of parallel studies of the organic and inorganic fractions of the sediments.

Entre la homogeneización moralizante y la adaptación al entorno: la escolarización bonaerense durante la última dictadura (1976-1983)

Este trabajo se propone abordar los sentidos que organizaron las políticas educativas en la provincia de buenos Aires durante la última dictadura militar. A partir del análisis de fuentes primarias, exploraremos el modo en que se combinaron inestablemente una fuerte intervención destinada a 're-moralizar' una sociedad considerada 'caótica' y una serie de medidas tendientes a 'modernizar' un sistema educativo supuestamente 'en crisis'. Argumentaremos que estas últimas se estructuraron en torno a la idea de adaptar la escolarización a las demandas del entorno y que, desde allí, la dictadura intervino en un amplio debate sobre la 'modernización educativa' en nuestro país que la había preexistido, dando cuenta del agotamiento de ciertos significados para la educación escolar e instalando una forma de procesar la 'modernización' que tendría importantes consecuencias más allá del fin del régimen.

Malvinas a 30 años del conflicto : Un análisis sobre las propuestas de enseñanza en formato digital

Este artículo trata de definir los límites y posibilidades de los nuevos textos digitales en la enseñanza de la historia, especialmente de algunas propuestas didácticas producidas por el gobierno nacional, cuyo contenido versa sobre la guerra de Malvinas. ¿Cuáles son los nuevos significados que este tipo de textos digitales aportan a la enseñanza y el aprendizaje de la Guerra de las Malvinas? ¿Qué discursos y narrativas sobre Malvinas se presentan explícitos e implícitos en estos textos digitales? ¿Hay algún cambio entre estas narraciones que emergen en el 30 aniversario de la guerra en comparación con las narrativas anteriores? Son algunas de las preguntas que tratamos de resolver, a pesar de que los textos en formato digital para la enseñanza de la historia, parecen ser muy caóticos y poseen otro régimen de producción, lectura y propiedad, diferente al de los materiales curriculares impresos. Como primera aproximación al análisis podemos observar como las políticas educativas nacionales actuales en Argentina refuerzan el discurso de los derechos y la soberanía sobre las islas, introduciendo además, elementos nuevos que buscan un acercamiento emocional a la causa y desdibujan en parte, la enseñanza de la complejidad de Malvinas

Strontium isotopes in pore waters of east equatorial Pacific sediments

Pore-water samples from the equatorial sedimentary bulge area show reversals in depth profiles of 87Sr/86Sr ratios at the sediment/basement interface. Results of this work support inferences made from previous pore-water data (from DSDP drilling in the area) that large-scale horizontal advection of seawater has occurred through the basement underlying the thick sedimentary sequence in this region. The area of apparent advection includes the eastern part of the equatorial high-productivity zone and part of the Guatemala Basin. We attempted to find links between the observed near-basement reversals in pore-water chemistry and sedimentary thickness, age, and topography of the area. Most of the sites that show horizontal advection have disturbed basement topography or outcrops within 10 to 20 km, suggesting that the cooling effects of outcrops may extend for at least 20 km horizontally. Heat-flow data from the area were compared to determine whether sites showing near-bottom chemistry reversals were consistent with areas of low conductive heat flow. This was generally true for the area of the sedimentary bulge and Guatemala Basin. Not enough pore-water data from the Nazca Plate were available to establish any reliable systematics. Because the high-productivity area is well-sealed from hydrothermal circulation, the missing heat must be lost by horizontal advective heat transport. From profiles of strontium isotopes and other elements that show departure from seawater values with increasing depth in the sediments, but return to seawater values near the basement, it appears that water flows relatively freely through much of the oceanic crust, even when sealed by considerable sedimentary cover.