(Table 1) List of samples with carbonate mineralogy, stable isotope, and accessory-mineral information

Petrographic and stable-isotope (d13C, d18O) patterns of carbonates from the Logatchev Hydrothermal Field (LHF), the Gakkel Ridge (GR), and a Late Devonian outcrop from the Frankenwald (Germany) were compared in an attempt to understand the genesis of carbonate minerals in marine volcanic rocks. Specifically, were the carbonate samples from modern sea floor settings and the Devonian analog of hydrothermal origin, low-temperature abiogenic origin (as inferred for aragonite in serpentinites from elsewhere on the Mid-Atlantic Ridge), or biogenic origin? Aragonite is the most abundant carbonate mineral in serpentinites from the two modern spreading ridges and occurs within massive sulfides of the LHF. The precipitation and preservation of aragonite suggests high Mg2+ and sulfate concentrations in fluids. Values of d18OPDB as high as +5.3 per mill for serpentinite-hosted aragonite and as high as +4.2 per mill for sulfide-hosted aragonite are consistent with precipitation from cold seawater. Most of the corresponding d13C values indicate a marine carbon source, whereas d13C values for sulfide-hosted aragonite as high as +3.6 per mill may reflect residual carbon dioxide in the zone of methanogenesis. Calcite veins from the LHF, by contrast, have low d18OPDB (-20.0 per mill to -16.1 per mill) and d13C values (-5.8 per mill to -4.5 per mill), indicative of precipitation from hydrothermal solutions (~129°-186°C) dominated by magmatic CO2. Calcite formation was probably favored by fluid rock interactions at elevated temperatures, which tend to remove solutes that inhibit calcite precipitation in seawater (Mg2+ and sulfate). Devonian Frankenwald calcites show low d18O values, reflecting diagenetic and metamorphic overprinting. Values of d13C around 0 per mill for basalt-hosted calcite indicate seawater-derived inorganic carbon, whereas d13C values for serpentinite-hosted calcite agree with mantle-derived CO2 (for values as low as -6 per mill) with a contribution of amagmatic carbon (for values as low as -8.6 per mill), presumably methane. Secondary mineral phases from the LHF for which a biogenic origin appears feasible include dolomite dumbbells, clotted carbonate, and a network of iron- and silica-rich filaments.

Pollen profile from sediment core Höllerer See

(expanded by Eberhard Grüger, Göttingen) The site "Höllerer See" is a lake in the northern foreland of the Alps, about 30 km north of the city of Salzburg/Austria, situated in the south-western part of Oberösterreich/Austria. A 2 m long piston core from this locality, consisting entirely of calcareous gyttja, was studied by pollen analysis. The three lowermost samples (1.98, 1.95 and 1.92 m) were deposited during the Preboreal when Pinus and Betula were still the dominating forest trees. High pollen values of thermophilous woody species (mainly Corylus and Quercus, but also Ulmus, Tilia, Fraxinus) prove the Boreal age of the next younger sample (1.91 m). The following two pollen spectra attest that Alnus (1.89 m) and - later (1.88 m) - Fagus had become important members of the local (Alnus) and the regional (Fagus) vegetation. From this level up to the top of the profile these two tree taxa contribute - together with Betula - always 50 to 80 % to the arboreal pollen sum. The upper 1.89 m of sediment of the Höllerer See core evidently date from the Subboreal and the Subatlantic. As Preboreal sediment was stated at the base of the profile it must be concluded that most of the Boreal and the Atlantic is - for whatever reason - not represented by sediment in this core. As no radiocarbon dates are available age estimates of the distinguished pollen zones can be achieved only by correlating major changes of the former vegetation with historical events which probably influenced the then contemporary vegetation. The pollen grains of the Triticum and Hordeum type found in samples of zone 2.1 might indicate the growing of cereals in the region during the Late Bronze Age. The first pollen grains of Secale date from the boundary Hallstatt/Latène Age (zone 2.2). The cereal curves become continuous in Bavarian times (Bajuwarenzeit, Middle Ages, zone 3.3). The Plantago laceolata curve, continuous since 1.7 m depth (zone 2.1), points to animal breeding since the Early Subatlantic (Hallstattzeit). This curve reaches its absolute maximum in Roman time (zone 3.1). Roman time forest clearance caused a drastic decrease of tree pollen curves (start of zone 3.1). Values of anthropogenic indicators as high as in zone 3.1 are found again - after a distinct decrease in zone 3.2 - not till the Bavarians settled in the region (6th century). Maximal Fagus values and the simultaneous total lack of anthropogenic indicators mark the Migration Period (zone 3.2). The Younger Subatlantic (zone 4) is characterized by a decrease of deciduous forests due to medieval forest clearance. At the same time the conifers Pinus and Picea gained in importance. The lake was probably used for retting hemp in Medieval times. The distinction of the pollen grains of Cannabis and Humulus might not be certain in all cases. It is known that hemp as well as hop was cultivated in the study area. Markers were added to the samples at the beginning of pollen preparation (13500 Lycopodium spores, sample volume 0.5 cm**3) and counted together with the pollen grains. Therefore pollen concentrations can be calculated: Concentration = C * F / V (with C = number of grains of a particular pollen type, V = volume of the untreated pollen sample, F = marker added/marker counted). F ranges from 39 to 1688. Factors that large are not suited to produce reliably interpretable pollen concentrations. Consequently no use was made of the pollen concentrations in this thesis, although a concentration diagram is added.

Rammed earth walls in Serón de Nágima castle (Soria, Spain): Constructive lecture

The Raya or frontier between the kingdoms of Castile and Aragón was fortified with a system of castles and walled-cities that were useful during the several conflicts that took place in the Late Medieval Age. The Serón de Nágima castle defended the communication road between the axis of the Jalón river valley, which flows into the Ebro, and Duero valley. Its uniqueness stems from the fact that it is one of the few fortifications in the area where rammed earth is the only building system used. In this paper, the castle building fundaments are exposed mainly focusing on the techniques and building processes developed from the interpretation of the legible constructive signs in its walls.

Fundamentos constructivos de las fortificaciones fronterizas entre las coronas de Castilla y Aragón de los siglos XII al XV en la actual provincia de Soria

La tesis doctoral desarrolla una investigación original, dentro del marco disciplinario de la historia de la construcción, sobre los fundamentos constructivos de las fortificaciones bajomedievales fronterizas entre las Coronas de Castilla y Aragón en la actual provincia de Soria. En el título de la tesis ya queda expresado el objeto fundamental y fundacional, así como el ámbito temporal —desde la reconquista del oriente soriano por parte de Alfonso I el Batallador a principios del siglo XII hasta la unificación de las coronas hispánicas en el siglo XV bajo el común mandato de los Reyes Católicos— y la extensión territorial que delimita la investigación: aquéllas comarcas castellanas lindantes con Aragón pertenecientes a la actual provincia de Soria. Durante este período bajomedieval se produjeron una serie de enfrentamientos fronterizos que obligó a fortificar la frontera y las vías de comunicación entre ambas coronas. La falta de estudios de conjunto de estas fortificaciones entendiéndolas como participantes en un sistema fortificado ha constituido la justificación de la investigación, que se realiza en varios niveles de análisis: territorial, histórico, arquitectónico, poliorcético y constructivo. Así mismo, se ha detectado cierta falta de rigor acompañada de inexactitudes en las consideraciones constructivas publicadas sobre algunas de las fortificaciones del ámbito de estudio, lo que ha provocado errores en su datación al no más haber elementos de corte artístico o estilístico que marquen indudablemente la pertenencia a una época. En la tesis se ponen en duda las dataciones tradicionalmente aceptadas planteando la hipótesis que da pie a la investigación: ante la falta de elementos artísticos o estilísticos en unos sobrios edificios eminentemente funcionales es posible establecer con suficiente aproximación la fecha de construcción en base a criterios constructivos una vez formada una clasificación cronotipológica de cada técnica constructiva. La hipótesis, por lo tanto, plantea un objetivo principal —el estudio de la razón constructiva del sistema fortificado fronterizo— desarrollado en una serie de objetivos específicos cuya consecución programa los sucesivos niveles de análisis: - Conocer y detallar los elementos históricos que originaron los enfrentamientos entre las Coronas de Castilla y Aragón y su desarrollo mediante herramientas historiográficas y analizar las características naturales del territorio en litigio mediante instrumentos cartográficos. - Conocer y analizar los tipos arquitectónicos y las tradiciones constructivas empleadas en las construcciones castrenses en el ámbito temporal en que se enmarca la investigación. - Localizar, documentar y seleccionar para su análisis las fortalezas y construcciones militares erigidas durante dichas luchas fronterizas en la actual provincia de Soria a través del trabajo de campo y métodos cartográficos y bibliográficos. - Realizar un estudio general sobre el sistema fortificado a escala territorial - Investigar la tipología arquitectónica, poliorcética y constructiva del conjunto de estas fortificaciones bajomedievales fronterizas. - Analizar los fundamentos constructivos de los casos de estudio seleccionados entre estas construcciones y caracterizarlas en cuanto al material, elementos, sistemas y procesos constructivos. - Ordenar la información histórica dispersa y corregir errores para hacer una base sobre la que establecer un discurso histórico de cada caso de estudio. - Comparar y relacionar las técnicas constructivas empleadas en estas fortalezas con los utilizados en el mismo ámbito temporal. - Difundir para su debate los resultados de la investigación por los foros científicos habituales. El método empleado combina los trabajos de gabinete con una intensa labor de campo, en la que se han documentado cincuenta fortificaciones y se han redactado sus correspondientes fichas de toma de datos. La recopilación de datos se ha incluido en una base de datos que incluye aspectos generales, tipológicos, constructivos y bibliográficos básicos del conjunto, a modo de inventario, de fortificaciones de la provincia. Las fortificaciones seleccionadas se agrupan según una clasificación tipológica y constructiva que marca las líneas de estudio posteriores. Se desarrolla un capítulo de antecedentes en el que se estudia la historia de la construcción fortificada medieval tanto en Europa como en España analizando la evolución de los tipos arquitectónicos y las múltiples influencias culturales que surcaron el Mediterráneo desde el Oriente cruzado e islámico al Poniente donde se desarrollaba la empresa reconquistadora que mantuvo en estado de guerra continuo a la Península Ibérica durante ochocientos años. El análisis del territorio como contenedor del hecho fortificado revela que hay una relación íntima entre la ubicación de las fortificaciones y las formas naturales que definen las vías de comunicación entre los valles del Duero, del Ebro y del Tajo. En efecto, el ámbito de estudio ha supuesto desde la Antigüedad un territorio de paso fundamental en la articulación de las comunicaciones en la Península Ibérica. Este carácter de paso más que de frontera explica las inquietudes y la preocupación por su control tanto por Roma como por el califato cordobés como por los reinos cristianos medievales. El análisis de los elementos históricos se complementa con el estudio detallado de los enfrentamientos fronterizos entre Castilla y Aragón así como los aspectos sociales y políticos que provocaron la fortificación como sistema de definición de la frontera y de organización espacial, jurisdiccional, social y administrativa del territorio. La arquitectura fortificada es esencialmente funcional: su cometido es la defensa. En este sentido, tras un estudio morfológico de los castillos seleccionados se realiza un extenso análisis poliorcético de sus elementos, investigando su origen y aplicación para servir también de parámetros de datación. Siendo el objeto inaugural de la tesis el estudio de los fundamentos constructivos, se explican los distintos materiales de construcción empleados y se agrupan las fábricas de las fortificaciones seleccionadas en dos grandes grupos constructivos: las fábricas aparejadas y las fábricas encofradas. Se han destacado y estudiado la evolución histórica y la tipología y mensiología constructiva de tres técnicas destacadas: el uso del ladrillo, la tapia de cal y canto o mampostería encofrada y la tapia de tierra. Para el estudio de la componente histórica y de la dimensión constructiva de cada técnica ha sido necesario documentar numerosos casos tanto en el ámbito de estudio como en la Península Ibérica con el fin de establecer grupos cronotipológicos constructivos entre los que poder ubicar las fábricas de estas técnicas presentes en el ámbito de estudio. Se ha observado una evolución dimensional de las fábricas de tapia que es más evidente en las hispanomusulmanas al modularse en codos pero que también se advierte significativamente en las cristianas bajomedievales. De cada una de las técnicas analizadas se ha seleccionado un caso de estudio singular y representativo. El castillo de Arcos de Jalón es un ejemplo significativo del empleo de la fábrica mixta de mampostería con verdugadas de ladrillo, así como las murallas de la ciudad fortificada de Peñalcázar lo es de la fábrica de mampostería encofrada y el castillo de Serón de Nágima constituye un caso característico y principal de la utilización de la tapia de tierra en la arquitectura militar bajomedieval. Cada uno de estos tres casos de estudios se examina bajo los mismos cuatro niveles anteriormente mencionados: territorial, histórico, arquitectónico y defensivo y constructivo. El sistemático método de estudio ha facilitado el orden en la investigación y la obtención de unos resultados y conclusiones que verifican la hipótesis y cumplen los objetivos marcados al comienzo. Se ha revisado la datación en la construcción de las fortificaciones analizadas mediante el estudio cronotipológico de sus fábricas, pudiendo trasladarse el método a otros sistemas fortificados. La tesis abre, finalmente, dos vías principales de investigación encaminadas a completar el estudio del sistema fortificado fronterizo bajomedieval en la raya oriental soriana de Castilla: la caracterización y datación por métodos físico-químicos de las muestras de piezas de madera de construcción que se conservan embebidas en las fábricas y la búsqueda documental y archivística que pueda revelar nuevos datos respecto a la fundación, reparación, venta o cualquier aspecto económico, legislativo, organizativo o administrativo relativo a las fortificaciones en documentos coetáneos. ABSTRACT The doctoral thesis develops an original research, held in the field of the Construction History, about the constructive reason of the frontier fortifications in the Late Middle Age between the Crowns of Castile and Aragón in the actual province of Soria, Spain. In the title is expressed the main objective, and also the temporal scope —from the reconquest in the 12th Century by Alfonso the First of Aragón to the unification under the common kingdom of the Catholic Kings— and the territorial extension that the research delimits: those Castilian regions in the border with Aragón in the actual province of Soria. During this period, a series of border wars were been, and this is the reason for the fortification of the border line and the main roads between both Crowns. The lack of studies of these fortifications as participants in a fortified system is the justification of the research. There is several analysis levels: territorial, historical, architectonic, defensive and constructive. Likewise, there is a lack of strictness and inaccuracy in the constructive items in the publications about several fortifications of this study field. This aspect has caused mistakes in the dating because there is neither artistic nor stylistic elements which determines a epoch. The traditionally accepted datings are challenged. An hypothesis is formulated: in the absence of artistic or stylistic elements in a sober and functional buildings is possible to date the time of construction with sufficiently approximation based on construction criteria once formed a cronotypologic classification of each building technique. The hypothesis, therefore, propose a main aim: the study of the constructive reason of the fortified border system. This aim is developed in a series of specifically targets whose achievement programs the analysis levels: - To know and to detail the historical elements which started the wars between Castile and Aragon and its development using historiographical tools, and to analyze the natural characteristic of the territory through cartographical tools. - To understand and to analyze the different architectural types and the building traditions employed in the military buildings in the time researched. - To locate, to document, and to select for their analysis the fortresses and military constructions erected during these border wars in the actual province of Soria through fieldwork and bibliographical and cartographical methods. - To conduct a general study on the fortified system in territorial scale. - To research the architectural, constructive and defensive typology of the system of these border late medieval fortifications. - To analyze the construction logic of the selected case studies and to characterize in the items of material, elements, systems and construction processes. - To sort scattered historical information and to correct mistakes to make a base by which to establish a historic speech of each case study. - To compare and to relate the construction techniques employed in these fortresses with those used in the same time range . - To spread for discussion the research results in the usual scientists forums. The method combines the destock work with an intense fieldwork. Fifty fortifications have been documented and it has written their corresponding data collection card. Data collection has been included in a database that includes general aspects, typological, constructive and basic bibliographical data, as an inventory of fortifications in the province. The selected fortifications are grouped according to a typological and constructive classification which lead the lines of the later study. There is a chapter for the antecedents in which the history of the medieval fortified construction in Europe and in Spain is studied by analyzing the evolution of architectural types and the many cultural influences along the opposite seasides of the Mediterranean Sea, from the Islamic and Crusader East to the Iberian Peninsula in where there were a long and continuous war during eight hundred years. The territory is analyzed as a container of fortifications. This analysis reveals that there is an intimate relationship between the location of the fortifications and the natural forms that define the communication roads between the Duero, Ebro and Tajo valleys. Indeed, the study area has been a cross-territory from ancient times more than a frontierterritory. This communication character explains the concerns about its control both by Rome and by the Muslims of Córdoba as medieval Christian kingdoms. The analysis of historical elements is supplemented by detailed study of border war between Castile and Aragon and the social and political issues that led to the fortification as border definition system and spatial, jurisdictional, social and administrative planning. The fortified architecture is essentially functional: it is responsible for defense. In this sense, after a morphological study of selected castles is performed an extensive analysis of its defensive elements, investigating its origin and application. This analisis serves for the definition of parameters for dating. The purpose of the thesis is the study of the constructive logic. First, various building materials are explained. Then, masonry is grouped into two major constructive groups: rigged masonry and formwork masonry. The historical evolution and the constructive typology and mensiology are studied for each one of the three main techniques: the use of brickwork, the mortar wall and rammed-earth. Many case studies have been documented along the Iberian Peninsula and also in the study area. As conclusion, there is a dimensional evolution of the rammed-earth walls. This evolution is more evident into the Muslim masonry than in the late medieval walls: the reason is the use of the cubit as module. From each of the techniques discussed, a singular and representative case of study has been selected. The castle of Arcos de Jalon is a significant example of mix masonry of stone and brick rows. The walled city of Peñalcázar is built with masonry formwork. Serón de Nágima castle, at last, is a typical and main case of the use of the rammedearth wall of late medieval military architecture. Each of these three case studies were examined under the same four analysis levels above mentioned: territorial, historical, architectural and defensive and constructive. The systematic method of study has facilitated the order in the research and the obtaining of results and conclusions that verify the hypotheses and achieve the research objectives. Dating of the fortifications construction has been revised by studying the cronotypological issues of its masonry. The method can be transferred to the study of other fortified systems. Finally, the thesis describes two main research new ways aimed at completing the study of the late medieval fortified border of Castile in the actual province of Soria. The first of them is the characterization and datig by physicochemical methods the sample pieces of wood construction preserved embedded in the masonry. The second research way is the investigation of the documents in archives that may reveal new information about the foundation, repair, sale or any aspect to economic, legal, organizational or administrative concerning fortifications in contemporary documents.

Interpretación constructiva de la fábrica de tapia de tierra del castillo de Serón de Nágima (Soria)

The article analyzes the particular construction history of the Castle of Serón de Nágima (Soria, Spain). Its constructive technique is the rammed-earth and it has not any singular or stylistic element which could be taken as chronological: for this reason the castle has been traditionally understood as a hispanic-muslim building. However, the analysis and constructive lecture and interpretation of the rammed-earth walls, putting them in comparison with others contemporaries and the study of the documentation can be used as a method to know the date of construction. The town of Serón is mentioned several times during the frontier wars between the Crowns of Castile and Aragon, but the castle is only mentioned in written documents since the 15th Century. The constructive characteristics of the rammed-earth walls are very different to the hispanic-muslim rammed-earth whereas similar to those of the Late Middle Age castles. The article also shows the constructive process of these rammed-earth walls through graphical methods.

BALAÃO – O QUE OUVE AS PALAVRAS DE EL, TEM O CONHECIMENTO DE ELYON E VÊ A VISÃO DE SHADDAI: UM ESTUDO DE NÚMEROS 22-24

A presente pesquisa busca avaliar exegeticamente o texto que se encontra na Bíblia, especificamente no livro de Números capítulos 22-24 que relata sobre um personagem conhecido como Balaão. A pesquisa tem também como objeto o estudo sobre o panteão de divindades relatado no mesmo texto, assim como também o estudo dos textos descobertos em Deir Alla, na Jordânia, que apresentam um personagem designado como Balaão, possivelmente o mesmo personagem de Nm 22-24. A motivação que levou ao desenvolvimento dessa pesquisa foi o fato de se ter deparado com os conceitos dos diversos nomes divinos exibidos no texto, além da questão do profetismo fora de Israel, assim como as possibilidades hermenêuticas que se abrem para a leitura desse texto bíblico. O conceito geral sempre foi o de que Israel era a única nação onde existiam “verdadeiros” profetas e uma adoração a um único Deus, o “monoteísmo”. O que despertou interesse foi perceber, especialmente por meio da leitura dos livros bíblicos, que o profetismo não se restringiu somente a Israel. Ele antecede à formação do antigo Israel e já existia no âmbito das terras do antigo Oriente Médio, e que Israel ainda demorou muito tempo para ser monoteísta. Quem é esse Balaão, filho de Beor? Estudaremos sobre sua pessoa e sua missão. Examinaremos os textos de Deir Alla sobre Balaão e sua natureza de personagem mediador entre o divino e o humano. Esse personagem é apresentado como um grande profeta e que era famoso como intérprete de presságios divinos. Analisaremos a importante questão sobre o panteão de deuses que são apresentados na narrativa de Balaão nomeados como: El, Elyon Elohim e Shaddai, além de Yahweh. Entendemos, a princípio, que o texto possui uma conexão com a sociedade na qual foi criado e usando da metodologia exegética, faremos uma análise da narrativa em questão, buscando compreender o sentido do texto, dentro de seu cenário histórico e social. Cenário este, que nos apresentou esse profeta, não israelita, que profere bênçãos dos deuses sobre Israel e que, além disso, pronuncia maldições sobre os inimigos desse mesmo Israel. Percebemos que, parte do texto pesquisado é apresentado sob a ótica de Israel sobre as outras nações. A pesquisa defende, portanto, que o texto de Nm 22-24, além de nos apresentar um profeta fora de Israel igual aos profetas da Bíblia, defende que, o panteão de divindades também era adorado por Israel e que tais nomes são epítetos de uma mesma divindade, no caso YHWH. Defende, também, um delineamento de um projeto de domínio político e militar de Israel sobre as nações circunvizinhas.

Biostratigraphy and paleobiogeographic affinities of the Jurassic brachiopod assemblages from Sierra Espuña (Maláguide Complex, Internal Betic Zones, Spain)

The assemblages of Early Jurassic brachiopods (Pliensbachian - Toarcian) from Sierra Espuña (Murcia Province, SE Spain) are described. This is the only area in the Internal Zones of the Betic Cordillera, corresponding to the margins of the Alborán Terrane, where Jurassic brachiopods are known to occur. In the tectonic Unit of Morrón de Totana (more southward located) assemblage MT1 of Late Pliensbachian age has been characterized. This assemblage has been subdivided into three successive sub-assemblages: MT1a (Algovianum Zone), MT1b (Emaciatum Zone, Solare Subzone) and MT1c (Emaciatum Zone, Elisa Subzone). Northward, in the Perona tectonic Unit two distinct assemblages, P1 (Latest Sinemurian - Early Pliensbachian) and P2 (Early Toarcian, Serpentinum Zone) have been recognized. Differences between the assemblages from the two tectonic units are evident after the paleobiogeographical analysis. In the Morrón de Totana Unit, taxa with Mediterranean affinities occur. MT1 assemblage is very similar to assemblages previously known in the Eastern Subbetic as well as in other areas of the Mediterranean Province. In the Perona Unit the Mediterranean affinity of the assemblages is not so evident. P1 Assemblage consists of widely distributed taxa, lacking in the most characteristic elements of the Mediterranean Province which, however, are present in neighbouring Betic areas. P2 Assemblage belongs to the Spanish Province that develops in Western Tethys after the Early Toarcian Mass Extinction Event. The occurrence in this assemblage of Prionorhynchia aff. msougari Rousselle, until now only found in North Africa, indicates a closer connection of the Perona Unit with the African paleomargin of the Tethys than with the South Iberian paleomargin. The paleobiogeographical data suggest a more southern and marginal (close to epicontinental areas) position of the Perona Unit than the Morrón de Totana Unit.

(Table 3) Textural and bulk mineralogy of Pliocene and Pleistocene sediments from ODP Hole 161-976B

The Pliocene and Pleistocene deposits recovered at Site 976 from the northwestern Alboran Sea at the Málaga base-of-slope include five main sedimentary facies: hemipelagic, turbidite, homogeneous gravity-flow, contourite, and debris-flow facies. The thickness and vertical distribution of these facies into lithostratigraphic Units I, II, and III show that the turbidites and hemipelagic facies are the dominant associations. The Pliocene and Pleistocene depositional history has been divided into three sedimentary stages: Stage I of early Pliocene age, in which hemipelagic and low-energy turbidites were the dominant processes; Stage II of early Pleistocene/late Pliocene age, in which the dominant processes were the turbidity currents interrupted by short episodes of other gravity flows (debris-flows and homogeneous gravity-flow facies) and bottom currents; and Stage III of Pleistocene age, in which both hemipelagic and low-energy gravity-flow processes occurred. The sedimentation during these three stages was controlled mainly by sea-level changes and also by the sediment supply that caused rapid terrigenous sedimentation variations from a proximal source represented by the Fuengirola Canyon.

Chronostratigraphic summary and raw counts of selected dinoflagellate cysts and architarch taxa of ODP Hole 151-907A

A detailed dinoflagellate cyst investigation of the almost continuous Middle Miocene through Pliocene of Ocean Drilling Program Hole 907A in the Iceland Sea has been conducted at 100-kyr resolution. The investigated section is well constrained by magnetostratigraphy, providing for the first time an independent temporal control on a succession of northern high-latitude dinoflagellate cyst bioevents. Based on the highest/lowest occurrences (HO/LO) and highest common occurrence (HCO) of 20 dinoflagellate cyst taxa and one acritarch species, 26 bioevents have been defined and compared with those recorded at selected DSDP, ODP, and IODP sites from the North Atlantic and contiguous seas, and in outcrops and boreholes from the onshore and offshore eastern U.S.A., and the North Sea and Mediterranean basins. Comparisons reveal near-synchronous HOs of the dinoflagellate cysts Batiacasphaera micropapillata (3.8-3.4 Ma, mid-Pliocene) and Reticulatosphaera actinocoronata (4.8-4.2 Ma, Lower Pliocene) across the Nordic Seas and North Atlantic, highlighting their value on a supraregional scale. This probably applies also to Hystrichosphaeropsis obscura (upper Tortonian), when excluding ODP Hole 907A where its sporadic upper stratigraphic range presumably relates to cooling in the early Tortonian. Over a broader time span within the upper Tortonian, the HO of Operculodinium piaseckii likely also permits correlation across the Nordic Seas and North Atlantic, and the HO of Labyrinthodinium truncatum appears useful in the Labrador and Nordic Seas. Biostratigraphic markers useful for regional rather than supraregional correlation are the HOs of Batiacasphaera hirsuta (c. 8.4 Ma, upper Tortonian) and Unipontidinium aquaeductus (c. 13.6-13.9 Ma, upper Langhian), the HCO of the acritarch Decahedrella martinheadii (c. 6.7-6.3 Ma, Messinian), and possibly the LO of Cerebrocysta irregulare sp. nov. (c. 13.8 Ma, uppermost Langhian) across the Nordic Seas. Since Habibacysta tectata, B. micropapillata, R. actinocoronata and D. martinheadii have been observed in the Arctic Ocean, they are potentially useful for high latitude correlations in the polar domain. The LOs of Habibacysta tectata and Unipontidinium aquaeductus suggest a mid- to late Langhian age (15.1-13.7 Ma) for deposits at the base of Hole 907A, thus providing new constraints on the age of basalts at the base of ODP Hole 907A. The stratigraphically important dinoflagellate cysts Cerebrocysta irregulare sp. nov., and Impagidinium elongatum sp. nov. are formally described.

(Table 1) 10 Beryllium and CaCO3 at DSDP Holes 86-576B, 86-576, and 86-578

Extension of the 10Be geochronology for deep-sea sediments beyond the limit of late Pliocene age found in published works has been attempted. The results obtained on sediments from Deep Sea Drilling Project (DSDP) Sites 576 and 578 of Leg 86 suggest the feasibility of dating sediments as old as 12 to 15 m.y. At both sites, there have been large changes in sedimentation rate, with the Pleistocene sediments accumulating several times faster than those of the Pliocene, which in turn were deposited several times more rapidly than the late Miocene sediments. The Pleistocene-Pliocene section is considerably thicker in Hole 578 than in Hole 576B: the respective depths for the 7 m.y. time boundary in the two holes are about 125 and about 25 m. These 10Be-based age estimates are in agreement with the paleomagnetic stratigraphies established for the two sites. The suggested enhancement in the oceanic deposition of 10Be before 7 to 9 m.y. ago, as noticed in manganese crusts, has found tentative support from the present sedimentary records. A preliminary search for 10Be production variation during a geomagnetic field reversal has been conducted. In Hole 578, an enhanced 10Be concentration is found in a sample close to the Brunhes/Matuyama reversal boundary. More detailed and systematic measurements are required to confirm this observation, which bears on the detailed behavior of the geomagnetic field during the reversal.