Propuesta de metodología para la calificación bio-ambiental de espacios verdes mediante coeficientes ecofisiológicos

Uno de los mayores problemas que enfrentan las urbes modernas es su crecimiento horizontal en base a cemento y asfalto, cubriendo grandes extensiones. Su resultado es un importante incremento de la temperatura llamado efecto "isla de calor", aspecto de particular importancia en años venideros por el creciente calentamiento global, a lo cual se añade la contaminación por gases y partículas. Las áreas destinadas a mitigar parcialmente estos efectos son los denominados espacios verdes, los cuales representan una mancha en el mapa. Sin embargo, su impacto termodinámico a nivel ambiental desde el punto de vista del confort y calidad de vida humanos puede ser muy variable según como esté diseñado. Este trabajo pretende establecer una metodología de aplicación en cualquier región, para calificar cuantitativamente el valor de los diferentes tipos de espacios verdes como modificadores ambientales, ya sean ejecutados o a nivel de proyecto. A través de esta metodología se determinan índices o coeficientes regionales objetivos y de sencilla aplicación. Para desarrollar estos índices, a los espacios verdes se aplican, adaptados, principios de la termodinámica de superficies húmedas y de la ecofisiología. A través de procedimientos matemáticos y conceptos fisiológicos se concluye en fórmulas para calcular índices regionales de aplicación directa en la evaluación de proyectos. A modo de comprobación de la metodología se determina el valor ambiental comparativo de diferentes tipos de espacios verdes correspondientes al sistema integrado de espacios verdes de la ciudad de Mendoza

(Table 2) Chemical composition of quenched glasses from the Mohns and Knipovich Ridges

The aim of this project was a petrogeochemical study of igneous rocks in the areas of the Mohns and Knipovich Ridges, both being the northern extensions of the Mid-Atlantic Ridge (MAR), using data available for quenching glass samples collected during Cruises 36 and 38 of R/V Akademic Mstislav Keldysh and during Cruise 15 of R/V Professor Logachev. Results of igneous rock studying from the Mohns and Knipovich Ridges at the background of evolution of the total North Atlantic Province, which had been identified earlier from tectonic and geophysical data, showed that igneous rocks of the Knipovich Ridge can be ranked as shallow tholeiites, primary melts of which were relatively rich in Na and Si and poor in Fe. This type of magma is characteristic of colder regions of the oceanic lithosphere. Its occurrence in the Knipovich Ridge and its potential propagation up to the Gakkel Ridge suggest that igneous rocks of this region originated under conditions of passive spreading in contrast to the MAR region in vicinity of Iceland and Azores, where substantial contribution of hotter material of a rising plume contributed to formation of the oceanic crust. The North Atlantic Ocean is the youngest province in terms of ocean-floor opening. Geologically and geophysically it is one of well studied regions of the World Ocean. Nevertheless some basic key items of its origin still remain to be clarified. In 1975 Scatler et al. proved specifics of this region manifested in growth of the gravity field, and also in relative height of the ocean floor in the region of 33-70°N, which was associated by them with rise of the hotter mantle, as compared with common regions of the Mid-Atlantic Ridge. Later this view was confirmed by character of magmatism, which differed in depth of generation and by melting degree of the resulting primary magma. Uniqueness of the North Atlantic region was also proved by the fact that this region was marked by extensive geochemical anomalies associated with Azores, Iceland, and Jan Mayen. All of these data allow to consider the northern part of the MAR (north of 33°N) as an united global geotectonic province. The Mohns and Knipovich Ridges located north of Iceland locate at the northern end of this province. This is the least known region. Therefore, new data for ridge areas of 73-77°N are needed for more complete geologic history of the Arctic Basin. The aim of this study was to carry out a complex comparison of magmatism at the Mohns and Knipovich Ridges with magmatism at large segments of the MAR northern province and to reconstruct mechanisms of primary magma formation, as well as conditions of their fractionation. This paper was based on results of studying quenched glasses, which reflect evolution of melt in the course of its formation.

Fases en la derivación e interpretación semántico pragmática

En trabajos anteriores (Romero, 2008a y b, Alabart Lago, L., P. Díaz y G. Herrera, 2012, Alabart Lago, L. y Herrera, G., 2013) se intentó mostrar que el mecanismo interpretativo que propone la TR podría resultar adecuado como uno de los sistemas externos (también interpretativos) postulados por la GG, más precisamente, el sistema llamado CI. La relación que intentamos establecer tendrá en cuenta lo siguiente como marco teórico: a) En TR se afirma que la interpretación de un enunciado se deriva de las estructuras sintácticas, y esta derivación se realiza "en paralelo" con la derivación de estructuras llevada a cabo por las operaciones del componente sintáctico. b) En las últimas propuestas de la GG, extensiones y revisiones del PM propuesto en Chomsky (1995) no solo se dejan de lado los niveles de representación internos SP y ES sino también se considera prescindible la interfaz FL (Chomsky, 2005). Las estructuras generadas se transfieren a los sistemas externos en cuanto rasgos formales de las Categorías Funcionales son valorados. Mantendremos la noción de que el sistema computacional es relativamente irrestricto y que sus operaciones son condicionadas solo por Atracción y las llamadas "condiciones de legibilidad" impuestas por los sistemas externos, fundamentalmente el Principio de Interpretación Completa (PIC). c) Tendremos en cuenta la propuesta de Leonetti y Escandell Vidal (2004), que sostiene que las CCFF de la GG pueden considerarse equivalentes a las Categoría Procedimentales propuestas por la TR. En este sentido consideraremos válida la afirmación de Chomsky (1998) acerca de que las CCFF centrales (C, T, v y D) tienen propiedades semánticas. d) Otro factor que tendremos en cuenta es la noción de fase en la derivación, considerándola correcta en los términos expuestos en Chomsky (2001 y 2005) y Gallego (2007 y 2009), con ciertas modificaciones. Nuestra hipótesis puede resumirse en lo siguiente: Las operaciones de extracción de inferencias propuestas por TR se aplican durante la derivación sintáctica independientemente de que se haya transferido o no una fase. Es más, esperamos poder demostrar que algunos mecanismos inferenciales imponen ciertas condiciones que afectan a la valoración de los rasgos de las CCFF. Pretendemos también intentar mostrar que además de los núcleos de fase reconocidos, C y v, debe considerarse fase a SD, porque contiene rasgos específicos de cuyo cotejo y valoración se desprende el valor que recibirán otros rasgos en el curso de la derivación. Con estos fundamentos esperamos poder elaborar una descripción de cómo interactúan ambos sistemas en la derivación de una oración y la asignación (casi simultánea) de significado

Se nas pedras faz feguras parecer... Consideraciones sobre iconografía mariana y figuras poéticas en las Cantigas de Santa María de Alfonso X

La iconografía mariana ha quedado reflejada en la poesía hispánica medieval de muchas maneras: desde versos que describen a la Virgen y sus atributos hasta conceptos teológicos y mariológicos expresados plásticamente mediante formas retóricas. Por ejemplo, el jardín y las flores como ornamentos y símbolos personales de Santa María, o bien la imagen de la luz a través de un cristal o una ventana de vidrio en escenas de la Anunciación -con abundantes testimonios pictóricos en el arte medieval-, se encuentran en la poesía en forma de descripciones simbólicas de diversa extensión y género y, por otro lado, de advocaciones marianas o tópicos mariológicos (Ave/Eva, Flos, Hortus, Radix-Virga, Regina, Stella). Este artículo propone, pues, un estudio de conjunto y comparativo de algunos de estos procedimientos, concentrándose en las Cantigas de Santa María del rey Alfonso X. En este sentido, las figuras retóricas, como herramientas que tienden un puente entre lo pictórico y lo poético, dirigen necesariamente la lectura hacia una interpretación simbólica proporcionada por la figuración o typologia, tal como la ha postulado Erich Auerbach para la textualidad medieval. En última instancia, el valor sagrado de la imagen mariana (una herencia del arte icónico bizantino) se representa también en los milagros de las Cantigas de Santa María, obra maestra que evidencia una fuerte influencia de la doctrina iconodúlica.

Se nas pedras faz feguras parecer... Consideraciones sobre iconografía mariana y figuras poéticas en las Cantigas de Santa María de Alfonso X

La iconografía mariana ha quedado reflejada en la poesía hispánica medieval de muchas maneras: desde versos que describen a la Virgen y sus atributos hasta conceptos teológicos y mariológicos expresados plásticamente mediante formas retóricas. Por ejemplo, el jardín y las flores como ornamentos y símbolos personales de Santa María, o bien la imagen de la luz a través de un cristal o una ventana de vidrio en escenas de la Anunciación -con abundantes testimonios pictóricos en el arte medieval-, se encuentran en la poesía en forma de descripciones simbólicas de diversa extensión y género y, por otro lado, de advocaciones marianas o tópicos mariológicos (Ave/Eva, Flos, Hortus, Radix-Virga, Regina, Stella). Este artículo propone, pues, un estudio de conjunto y comparativo de algunos de estos procedimientos, concentrándose en las Cantigas de Santa María del rey Alfonso X. En este sentido, las figuras retóricas, como herramientas que tienden un puente entre lo pictórico y lo poético, dirigen necesariamente la lectura hacia una interpretación simbólica proporcionada por la figuración o typologia, tal como la ha postulado Erich Auerbach para la textualidad medieval. En última instancia, el valor sagrado de la imagen mariana (una herencia del arte icónico bizantino) se representa también en los milagros de las Cantigas de Santa María, obra maestra que evidencia una fuerte influencia de la doctrina iconodúlica.

Fases en la derivación e interpretación semántico pragmática

En trabajos anteriores (Romero, 2008a y b, Alabart Lago, L., P. Díaz y G. Herrera, 2012, Alabart Lago, L. y Herrera, G., 2013) se intentó mostrar que el mecanismo interpretativo que propone la TR podría resultar adecuado como uno de los sistemas externos (también interpretativos) postulados por la GG, más precisamente, el sistema llamado CI. La relación que intentamos establecer tendrá en cuenta lo siguiente como marco teórico: a) En TR se afirma que la interpretación de un enunciado se deriva de las estructuras sintácticas, y esta derivación se realiza "en paralelo" con la derivación de estructuras llevada a cabo por las operaciones del componente sintáctico. b) En las últimas propuestas de la GG, extensiones y revisiones del PM propuesto en Chomsky (1995) no solo se dejan de lado los niveles de representación internos SP y ES sino también se considera prescindible la interfaz FL (Chomsky, 2005). Las estructuras generadas se transfieren a los sistemas externos en cuanto rasgos formales de las Categorías Funcionales son valorados. Mantendremos la noción de que el sistema computacional es relativamente irrestricto y que sus operaciones son condicionadas solo por Atracción y las llamadas "condiciones de legibilidad" impuestas por los sistemas externos, fundamentalmente el Principio de Interpretación Completa (PIC). c) Tendremos en cuenta la propuesta de Leonetti y Escandell Vidal (2004), que sostiene que las CCFF de la GG pueden considerarse equivalentes a las Categoría Procedimentales propuestas por la TR. En este sentido consideraremos válida la afirmación de Chomsky (1998) acerca de que las CCFF centrales (C, T, v y D) tienen propiedades semánticas. d) Otro factor que tendremos en cuenta es la noción de fase en la derivación, considerándola correcta en los términos expuestos en Chomsky (2001 y 2005) y Gallego (2007 y 2009), con ciertas modificaciones. Nuestra hipótesis puede resumirse en lo siguiente: Las operaciones de extracción de inferencias propuestas por TR se aplican durante la derivación sintáctica independientemente de que se haya transferido o no una fase. Es más, esperamos poder demostrar que algunos mecanismos inferenciales imponen ciertas condiciones que afectan a la valoración de los rasgos de las CCFF. Pretendemos también intentar mostrar que además de los núcleos de fase reconocidos, C y v, debe considerarse fase a SD, porque contiene rasgos específicos de cuyo cotejo y valoración se desprende el valor que recibirán otros rasgos en el curso de la derivación. Con estos fundamentos esperamos poder elaborar una descripción de cómo interactúan ambos sistemas en la derivación de una oración y la asignación (casi simultánea) de significado

Se nas pedras faz feguras parecer... Consideraciones sobre iconografía mariana y figuras poéticas en las Cantigas de Santa María de Alfonso X

La iconografía mariana ha quedado reflejada en la poesía hispánica medieval de muchas maneras: desde versos que describen a la Virgen y sus atributos hasta conceptos teológicos y mariológicos expresados plásticamente mediante formas retóricas. Por ejemplo, el jardín y las flores como ornamentos y símbolos personales de Santa María, o bien la imagen de la luz a través de un cristal o una ventana de vidrio en escenas de la Anunciación -con abundantes testimonios pictóricos en el arte medieval-, se encuentran en la poesía en forma de descripciones simbólicas de diversa extensión y género y, por otro lado, de advocaciones marianas o tópicos mariológicos (Ave/Eva, Flos, Hortus, Radix-Virga, Regina, Stella). Este artículo propone, pues, un estudio de conjunto y comparativo de algunos de estos procedimientos, concentrándose en las Cantigas de Santa María del rey Alfonso X. En este sentido, las figuras retóricas, como herramientas que tienden un puente entre lo pictórico y lo poético, dirigen necesariamente la lectura hacia una interpretación simbólica proporcionada por la figuración o typologia, tal como la ha postulado Erich Auerbach para la textualidad medieval. En última instancia, el valor sagrado de la imagen mariana (una herencia del arte icónico bizantino) se representa también en los milagros de las Cantigas de Santa María, obra maestra que evidencia una fuerte influencia de la doctrina iconodúlica.

Benthic and substrate cover data derived from photo-transect surveys in Heron Reef

Underwater georeferenced photo-transect survey was conducted on September 23 - 27, 2007 at different sections of the reef flat, reef crest and reef slope in Heron Reef. For this survey a snorkeler or diver swam over the bottom while taking photos of the benthos at a set height using a standard digital camera and towing a surface float GPS which was logging its track every five seconds. A standard digital compact camera was placed in an underwater housing and fitted with a 16 mm lens which provided a 1.0 m x 1.0 m footprint, at 0.5 m height above the benthos. Horizontal distance between photos was estimated by three fin kicks of the survey diver/snorkeler, which corresponded to a surface distance of approximately 2.0 - 4.0 m. The GPS was placed in a dry-bag and logged its position as it floated at the surface while being towed by the photographer. A total of 3,586 benthic photos were taken. A floating GPS setup connected to the swimmer/diver by a line enabled recording of coordinates of each benthic. Approximation of coordinates of each benthic photo was done based on the photo timestamp and GPS coordinate time stamp, using GPS Photo Link Software (www.geospatialexperts.com). Coordinates of each photo were interpolated by finding the gps coordinates that were logged at a set time before and after the photo was captured. Benthic or substrate cover data was derived from each photo by randomly placing 24 points over each image using the Coral Point Count excel program (Kohler and Gill, 2006). Each point was then assigned to 1 out of 80 cover types, which represented the benthic feature beneath it. Benthic cover composition summary of each photo scores was generated automatically using CPCE program. The resulting benthic cover data of each photo was linked to gps coordinates, saved as an ArcMap point shapefile, and projected to Universal Transverse Mercator WGS84 Zone 56 South.

Photosynthetic production in the Central Arctic during POLARSTERN cruise ARK-XXVII/3 (IceArc) in 2012

The ice-covered Central Arctic Ocean is characterized by low primary productivity due to light and nutrient limitations. It has been speculated that the recent reduction in ice cover could lead to a substantial increase in primary production, but still little is known as to the fate of the ice-associated primary production, and of nutrient supply with increasing warming. This study presents results from the Central Arctic Ocean collected during summer 2012, when sea-ice reached a minimum extent since the onset of satellite observations. Net primary productivity (NPP) was measured in water column, sea ice and melt ponds by 14CO2 uptake at different irradiances. Photosynthesis vs. irradiance (PI) curves were established in laboratory experiments and used to upscale measured NPP to the deep Eurasian Basin (north of 78°N) using the irradiance-based Central Arctic Ocean Primary Productivity model (CAOPP). In addition, new annual production was calculated from the seasonal nutrient drawdown in the mixed layer since last winter. Results show that ice algae can contribute up to 60% to primary production in the Central Arctic at the end of the season. The ice-covered water column had lower NPP rates than open water probably due to light limitation. According to the nutrient ratios in the euphotic zone, nitrate limitation was detected in the Siberian Seas (Laptev Sea area), while silicate was the main limiting nutrient at the ice margin influenced by Atlantic waters. Although sea-ice cover was substantially reduced in 2012, total annual new production in the Eurasian Basin was 17 ± 7 Tg C/yr, which is similar to previous estimates. However, when including the contribution by sub-ice algal filaments, the annual production for the deep Eurasian Basin (north of 78°N) is 16 Tg C/yr higher than estimated before. Our data suggest that sub-ice algae might be responsible for potential local increases in NPP due to higher light availability under the ice, and their ability to benefit from a wider area of nutrients as they drift with the ice.

Epigeal spider occurrence, abundance and diversity in moist acidic and dry heath tundra at Toolik Lake, Alaska

For the 2004-2006 growing seasons, we trapped a total of 6980 spiders (5066 adults, 1914 immatures) using pitfall traps at the Arctic Long Term Experimental Research (LTER) site in Toolik Lake, Alaska. We found 10 families and 51 putative species, with 45 completely identified, in two distinct habitats: Moist Acidic Tundra (MAT) and Dry Heath (DH) Tundra. We captured spiders belonging to the following families (number of species captured): Araneidae (1), Clubionidae (1), Dictynidae (1), Gnaphosidae (4), Linyphiidae (26), Lycosidae (11), Philodromidae (2), Salticidae (1), Theridiidae (1), and Thomisidae (3). Statistical comparisons of families captured at MAT and DH Tundra indicate that the habitats have significantly different spider communities (Chi Square Test: p < 0.0001, and Fisher's Exact Test: p = 0.0018). This finding is further supported by differences in similarity, diversity, evenness, and species richness between the two habitats. In this report, we present eight new state records and five extensions of previously described ranges for spider species. The following species are new state records for Alaska: Emblyna borealis (O.P.-Cambridge 1877), Horcotes strandi (Sytschevskaja 1935), Mecynargus monticola (Holm 1943), Mecynargus tungusicus (Eskov 1981), Metopobactrus prominulus (O.P. -Cambridge 1872), Poeciloneta theridiformis Emerton 1911, and Poeciloneta vakkhanka (Tanasevitch 1989). The following five species have been reported previously in Alaska, but not near Toolik Lake: Hypsosinga groenlandica Simon 1889, Gnaphosa borea Kulczyn'ski 1908, Gnaphosa microps Holm 1939, Haplodrassus hiemalis (Emerton 1909), and Islandiana cristata Eskov 1987. Pairwise similarity indices were calculated across 13 other arctic and subarctic spider communities and statistical tests show that all sites are dissimilar (p = 0.25). These results fit the general pattern of both the patchiness and habitat specificity of arctic spider fauna.

Past circulation along the western Iberian margin

Fifteen Iberian margin sediment cores, distributed between 43°12'N and 35°53'N, have been used to reconstruct spatial and temporal (sub)surface circulation along the Iberian margin since the Last Glacial period. Time-slice maps of planktonic foraminiferal derived summer sea surface temperature (SST) and export productivity (Pexp) were established for specific time intervals within the last 35 ky: the Holocene (Recent and last 8 ky), Younger Dryas (YD), Heinrich Stadials (HS) 1, 2a, 2b, 3, and the Last Glacial Maximum (LGM). The SST during the Holocene shows the same latitudinal gradient along the western Iberian margin as present-day with cold but productive areas that reflect the influence of coastal upwelling centers. The LGM appears as a slightly less warm, but more productive period relative to the Holocene and present-day conditions, suggesting that sea-level minima forced a westward displacement of the coastal upwelling centers possibly accompanied by a strengthening of northward winds. During the YD, a longitudinal thermal front is depicted at 10°W, with cold polar waters offshore and warmer subtropical waters inshore, suggesting that the subtropical Paleo-Iberian Poleward Current more likely flowed at a more inshore location masking the local SST signal and amplitude of variation. A substantial cooling and drop in productivity is observed during all HS, in particular HS1 and HS3, reflecting the penetration of icebergs-derived meltwater. These most extreme southward extensions of very cold waters define a strong SST gradient that marks a possible Paleo-Azores Front. Higher production south of this front was likely fed by frontal nutrient advection.

Flux of ice-rafted detritus in the Fram Strait

A three-year particle flux record from the eastern Fram Strait, between Greenland and Svalbard, revealed a rather untypical seasonal flux pattern compared to other particle flux studies from the Nordic Seas. In the eastern Fram Strait this pattern is characterised by a sudden four- to six-fold increase of the particle flux in January, when no daylight is available to support any biological productivity. Comparison with sea-ice distribution maps led to the conclusion that the sudden increase in the flux is due to ice-rafted detritus released from sea ice, which originated from the Svalbard archipelago and from the northern Barents Sea. Detailed grain size analyses of the silt fraction indicated the >10 µm fraction of the lithogenic matter to be clearly enriched due to IRD input. Even more important is the observation that lithogenic material >40 µm occurs exclusively during the ice-rafting event and, therefore, appears to be a suitable indicator for IRD transported on sea ice. Thus, in addition to coarse IRD (e.g. >500 µm), which is mainly derived from icebergs, the analysis of fine IRD >40 µm in deep-sea sediments can be used to reconstruct paleo-sea-ice extensions.

Bulk geochemistry and grain-size composition of surface sediments from the SW Atlantic

Surface sediments from the South American continental margin surrounding tbe Argentine Basin were studied with respect to bulk geochemistry (Caeo) and C ) and grain-size composition (sand/silt/clay relation and terrigenous silt grain-size distribution). The grain-size distributions of the terrigenous silt fraction were unmixed into three end members (EMs), using an end-member modelling algorithm. Three unimodal EMs appear to satisfactorily explain the variations in the data set of the grain-size distributions ofterrigenous silt. The EMs are related to sediment supply by rivers, downslope transport, winnowing, dispersal and re-deposition by currents. The bulk geochemical composition was used to trace the distribution of prominent water masses within the vertical profile. The sediments of the eastern South American continental margin are generally divided into a coarse-grained and carbonate-depleted southwestern part, and a finer-grained and carbonate-rich northeastern part. The transition of both environments is located at the position of the Brazil Malvinas Confluence (BMC). The sediments below the confluence mixing zone of the Malvinas and Brazil Currents and its extensions are characterised by high concentrations of organic carbon, low carbonate contents and high proportions of the intennediate grain-size end member. Tracing these properties, the BMC emerges as a distinct north-south striking feature centered at 52-54°W crossing the continental margin diagonally. Adjacent to this prominent feature in the southwest, the direct detrital sediment discharge of the Rio de la Plata is clearly recognised by a downslope tongue of sand and high proportions of the coarsest EM. A similar coarse grain-size composition extends further south along the continental slope. However, it displays bener sorting due to intense winnowing by the vigorous Malvinas Current. Fine-grained sedimentary deposition zones are located at the southwestern deeper part of the Rio Grande Rise and the southern abyssal Brazil Basin, both within the AABW domain. Less conspicuous winnowing/accumulation panerns are indicated north of the La Plata within the NADW level according to the continental margin topography. We demonstrate that combined bulk geochemical and grain-size properties of surface sediments, unmixed with an end-member algorithm, provide a powerful tool to reconstruct the complex interplay of sedimentology and oceanography along a time slice.

(Table 1) List of studied samples with vestimentiferan tubes

Vestimentiferan tube worms are prominent members of modern methane seep communities and are totally reliant as adults on symbiotic sulphide-oxidizing bacteria for their nutrition. The sulphide is produced in the sediment by a biochemical reaction called the anaerobic oxidation of methane (AOM). A well-studied species from the Gulf of Mexico shows that seep vestimentiferans 'mine' sulphide from the sediment using root-like, thin walled, permeable posterior tube extensions, which can also be used to pump sulphate and possibly hydrogen ions from the soft tissue back into the sediment to increase the local rate of AOM. The 'root-balls' of exhumed seep vestimentiferans are intimately associated with carbonate nodules, which are a result of AOM. We have studied vestimentiferan specimens and associated carbonates from seeps at the Kouilou pockmark field on the Congo deep-sea fan and find that some of the posterior 'root' tubes of living specimens are enclosed with carbonate indurated sediment and other, empty examples are partially or completely replaced by the carbonate mineral aragonite. This replacement occurs from the outside of the tube wall inwards and leaves fine-scale relict textures of the original organic tube wall. The process of mineralization is unknown, but is likely a result of post-mortem microbial decay of the tube wall proteins by microorganisms or the precipitation from locally high flux of AOM derived carbonate ions. The aragonite-replaced tubes from the Kouilou pockmarks show similar features to carbonate tubes in ancient seep deposits and make it more likely that many of these fossil tubes are those of vestimentiferans. These observations have implications for the supposed origination of this group, based on molecular divergence estimates.

Benthic foraminifers in Mesozoic and Cenozoic sediments of the southwestern Atlantic

Benthic foraminiferal assemblages in Mesozoic and Cenozoic sediments were studied at Sites 511, 512, 513, and 514 drilled during Leg 71 in the southwestern Atlantic on the Maurice Ewing Bank and in the Argentine Basin. Benthic foraminifers in almost all stratigraphic subdivisions of Sites 511 and 512 reflect the gradual subsidence of the Falkland Plateau from shelf depths in the Barremian-Albian, when a semiclosed basin with restricted circulation of water masses and anaerobic conditions existed, to lower bathyal depths in the Late Cretaceous and Cenozoic, with an abrupt acceleration at the boundary of Lower and Upper Cretaceous. The composition, distribution, and preservation of Late Cretaceous assemblages of benthic foraminifers suggest considerable fluctuations of the foraminiferal lysocline and the CCD. This is evidenced by dissolution facies and foraminiferal assemblages in which agglutinated and resistant calcareous forms predominated during high stands of the CCD and by calcareous facies in which rich assemblages of calcareous species predominated during low stands. The highest position of the CCD on the Plateau (less than 1500-2000 m) was in the late Cenomanian, Turonian, and Coniacian. In the Santonian and Campanian the CCD was at depths below 1500-2000 meters. At the end of the Campanian the CCD shifted again to depths comparable with those of Cenomanian and Turonian time. In the latest Campanian and the Maestrichtian the CCD was low and nanno-foraminiferal oozes with a rich assemblage of benthic foraminifers accumulated. Foraminiferal assemblages at Sites 513 and 514 in the Argentine Basin also testify to oceanic subsidence from lower bathyal depths in the Oligocene to abyssal ones at present. This process was complicated by the influence of geographical migrations of the Polar Front caused by extensions of the ice sheet in the Antarctic after the opening of the Drake Passage during the Oligocene. In Mesozoic and Cenozoic deposits of the Falkland Plateau and the Argentine Basin seven assemblages of benthic foraminifers were distinguished by age: early-middle Albian, middle-late Albian, Late Cretaceous (including four groups), middle Eocene, late Eocene-early Miocene, middle-late Miocene, and Pliocene-Quaternary. The Albian assemblages contain many species common to the foraminiferal fauna of the Austral Biogeographical Province. The Late Cretaceous assemblage contains, along with Austral species, species common to foraminifers of North America, Western Europe, the Russian platform, and the south of the U.S.S.R. Deep-sea cosmopolitan species prevail in Cenozoic assemblages.