Seawater carbonate chemistry, respiration, maximum photochemical efficiency and mortality of brooded larvae of Pocillopora//damicornis in a laboratory experiment

To evaluate the effects of temperature and pCO2 on coral larvae, brooded larvae of Pocillopora damicornis from Nanwan Bay, Taiwan (21°56.179' N, 120°44.85' E), were exposed to ambient (419-470 µatm) and high (604-742 µatm) pCO2 at ~25 and ~29 °C in two experiments conducted in March 2010 and March 2012. Larvae were sampled from four consecutive lunar days (LD) synchronized with spawning following the new moon, incubated in treatments for 24 h, and measured for respiration, maximum photochemical efficiency of PSII (F v/F m), and mortality. The most striking outcome was a strong effect of time (i.e., LD) on larvae performance: respiration was affected by an LD × temperature interaction in 2010 and 2012, as well as an LD × pCO2 × temperature interaction in 2012; F v/F m was affected by LD in 2010 (but not 2012); and mortality was affected by an LD × pCO2 interaction in 2010, and an LD × temperature interaction in 2012. There were no main effects of pCO2 in 2010, but in 2012, high pCO2 depressed metabolic rate and reduced mortality. Therefore, differences in larval performance depended on day of release and resulted in varying susceptibility to future predicted environmental conditions. These results underscore the importance of considering larval brood variation across days when designing experiments. Subtle differences in experimental outcomes between years suggest that transgenerational plasticity in combination with unique histories of exposure to physical conditions can modulate the response of brooded coral larvae to climate change and ocean acidification.

Estudio de la selección y desplazamiento de bellotas por roedores bajo diferentes condiciones lumínicas y de microhábitat; implicaciones en el regenerado natural del género Quercus.

Este estudio se centra en la actividad de selección y acopio de bellotas por parte de pequeños roedores, en concreto el ratón de campo (Apodemus sylvaticus), que se ha demostrado como la principal especie dispersora de bellotas en la zona de estudio. La prioridad de este trabajo ha sido estudiar la influencia de ciertos factores ambientales (luminosidad lunar y disponibilidad de refugio para el roedor) en el fenómeno de selección. Se tomaron datos bajo diferentes condiciones de luminosidad lunar (luna llena y luna nueva) y de disponibilidad de refugio (bajo cobertura de matorral y sin cobertura). La zona de estudio se ubicó en el Hayedo de Montejo, Madrid. La razón de la elección de este lugar fue la existencia de estudios genéticos llevados a cabo en él que revelaron largos y curiosos movimientos de semillas, que sólo podían ser fruto de una contribución de la fauna dispersora.

Athanasii Kircheri Fuldensis Buchonii... Ars magna lucis et umbrae, in decem libros digesta. Quibus admirandae lucis et umbrae in mundo, atque adeò vniuersa natura, vires effectusq. vti noua, uti varia nouorum reconditiorumq. speciminum exhibitione, ad varios mortalium vsus, panduntur...

En port. grab. xil. de sol con lema: "Sicuti tenebrae eius ita & lumen eius. Psal. 138"

Ferromanganese nodules and micro-hardgrounds associated with the Cadiz Contourite Channel (NE Atlantic): Palaeoenvironmental records of fluid venting and bottom currents

Ferromanganese nodule fields and hardgrounds have recently been discovered in the Cadiz Contourite Channel in the Gulf of Cadiz (850–1000 m). This channel is part of a large contourite depositional system generated by the Mediterranean Outflow Water. Ferromanganese deposits linked to contourites are interesting tools for palaeoenviromental studies and show an increasing economic interest as potential mineral resources for base and strategic metals. We present a complete characterisation of these deposits based on submarine photographs and geophysical, petrographic, mineralogical and geochemical data. The genesis and growth of ferromanganese deposits, strongly enriched in Fe vs. Mn (av. 39% vs. 6%) in this contourite depositional system result from the combination of hydrogenetic and diagenetic processes. The interaction of the Mediterranean Outflow Water with the continental margin has led to the formation of Late Pleistocene–Holocene ferromanganese mineral deposits, in parallel to the evolution of the contourite depositional system triggered by climatic and tectonic events. The diagenetic growth was fuelled by the anaerobic oxidation of thermogenic hydrocarbons (δ13CPDB=−20 to −37‰) and organic matter within the channel floor sediments, promoting the formation of Fe–Mn carbonate nodules. High 87Sr/86Sr isotopic values (up to 0.70993±0.00025) observed in the inner parts of nodules are related to the influence of radiogenic fluids fuelled by deep-seated fluid venting across the fault systems in the diapirs below the Cadiz Contourite Channel. Erosive action of the Mediterranean Outflow Water undercurrent could have exhumed the Fe–Mn carbonate nodules, especially in the glacial periods, when the lower core of the undercurrent was more active in the study area. The growth rate determined by 230Thexcess/232Th was 113±11 mm/Ma, supporting the hypothesis that the growth of the nodules records palaeoenvironmental changes during the last 70 ka. Ca-rich layers in the nodules could point to the interaction between the Mediterranean Outflow Water and the North Atlantic Deep Water during the Heinrich events. Siderite–rhodochrosite nodules exposed to the oxidising seabottom waters were replaced by Fe–Mn oxyhydroxides. Slow hydrogenetic growth of goethite from the seawaters is observed in the outermost parts of the exhumed nodules and hardgrounds, which show imprints of the Mediterranean Outflow Water with low 87Sr/86Sr isotopic values (down to 0.70693±0.00081). We propose a new genetic and evolutionary model for ferromanganese oxide nodules derived from ferromanganese carbonate nodules formed on continental margins above the carbonate compensation depth and dominated by hydrocarbon seepage structures and strong erosive action of bottom currents. We also compare and discuss the generation of ferromanganese deposits in the Cadiz Contourite Channel with that in other locations and suggest that our model can be applied to ferromanganiferous deposits in other contouritic systems affected by fluid venting.

Polymetallic ferromanganese deposits research on the Atlantic Spanish continental margin

Seamounts, submarine banks, volcanoes and undercurrent channels are prominent geomorphic features that have become an important target for minerals research and exploration with the goal of future exploitation. Polymetallic ferromanganese deposits are common types of mineralization on these settings. Co-rich ferromanganese crusts are important as potential resources of Mn and Co, but also Ti, Ni, Tl, REEs, PGEs, and other metals. Many seamounts and channels along the Atlantic Spanish continental margin are known to hold mineral deposits but are poorly studied. This work presents and briefly describes the most recent activities of the Spanish Geological Survey (IGME) on exploration and investigation of ferromanganese deposits along the Atlantic Spanish continental margin. Different submarine areas from the northwestern margin of the Iberian Peninsula to the west off Canary Islands have been surveyed by geophysical, sampling and underwater observations from 89 to 4000 m water depth. The mineral deposits cover a large diversity of submarine geological and geomorphical features: mud volcanoes and diapirs related to hydrocarbon seeps, seamounts associated with hot spot volcanism, hydrothermal vents in active magmatic volcanoes, structural basement highs and banks or contourite channels. Considering the collected dataset, we present the preliminary results of the study of these mineral deposits, including ferromanganese nodules and crusts and phosphate pavements and nodules, which can be considered as potential sources of raw materials.

Possible forcing of global temperature by the oceanic tides

An approximately decadal periodicity in surface air temperature is discernable in global observations from A.D. 1855 to 1900 and since A.D. 1945, but with a periodicity of only about 6 years during the intervening period. Changes in solar irradiance related to the sunspot cycle have been proposed to account for the former, but cannot account for the latter. To explain both by a single mechanism, we propose that extreme oceanic tides may produce changes in sea surface temperature at repeat periods, which alternate between approximately one-third and one-half of the lunar nodal cycle of 18.6 years. These alternations, recurring at nearly 90-year intervals, reflect varying slight degrees of misalignment and departures from the closest approach of the Earth with the Moon and Sun at times of extreme tide raising forces. Strong forcing, consistent with observed temperature periodicities, occurred at 9-year intervals close to perihelion (solar perigee) for several decades centered on A.D. 1881 and 1974, but at 6-year intervals for several decades centered on A.D. 1923. As a physical explanation for tidal forcing of temperature we propose that the dissipation of extreme tides increases vertical mixing of sea water, thereby causing episodic cooling near the sea surface. If this mechanism correctly explains near-decadal temperature periodicities, it may also apply to variability in temperature and climate on other times-scales, even millennial and longer.

Successful external fertilization in turbulent environments.

Mathematical and experimental simulations predict that external fertilization is unsuccessful in habitats characterized by high water motion. A key assumption of such predictions is that gametes are released in hydrodynamic regimes that quickly dilute gametes. We used fucoid seaweeds to examine whether marine organisms in intertidal and subtidal habitats might achieve high levels of fertilization by restricting their release of gametes to calm intervals. Fucus vesiculosus L. (Baltic Sea) released high numbers of gametes only when maximal water velocities were below ca. 0.2 m/s immediately prior to natural periods of release, which occur in early evening in association with lunar cues. Natural fertilization success measured at two sites was always close to 100%. Laboratory experiments confirmed that (i) high water motion inhibits gamete release by F. vesiculosus and by the intertidal fucoids Fucus distichus L. (Maine) and Pelvetia fastigiata (J. Ag.) DeToni (California), and (ii) showed that photosynthesis is required for high gamete release. These data suggest that chemical changes in the boundary layer surrounding adults during photosynthesis and/or mechanosensitive channels may modulate gamete release in response to changing hydrodynamic conditions. Therefore, sensitivity to environmental factors can lead to successful external fertilization, even for species living in turbulent habitats.

Estudio geológico y metalogénico de la mineralización argentífera de Hiendelaencina, Sistema Central

En este trabajo se estudian las características geológicas, mineralógicas y texturales de la mineralización argentífera de Hiendelaencina. Se establece la morfología y la disposición del yacimiento, así como la paragénesis y sucesión mineral, definiéndose los distintos tipos de sulfosales de plata presentes.

Un software FOSS para la gestión de las fotografías obtenidas por fototrampeo

La constante innovación tecnológica y al abaratamiento de los dispositivos, han hecho que el fototrampeo se convierta en una técnica ampliamente utilizada para la realización de inventarios biológicos, generando gran cantidad de registros de alto interés ecológico. El principal objetivo de esta comunicación es presentar una herramienta de software libre (FOSS), desarrollada para facilitar el manejo de datos, obtenidos mediante fototrampeo en un espacio protegido de la Comunidad Valenciana. Así, a partir de un estudio iniciado en 2009, se ha analizado la composición de la comunidad de vertebrados en el Parque Natural de la Sierra de Mariola. Para la realización de los muestreos se han empleado cámaras de infrarrojos con sensor de movimiento (Moultrie Game Spy I-60®), obteniendo un total de 29,941 contactos que han servido para determinar la abundancia de las especies muestreadas en las 63 cuadrículas (2*2 Km) establecidas en la zona de estudio. La aplicación FOSS, denominada “Camera Trap Manager”, se ha diseñado para agilizar el tratamiento de esta información y funciona sobre la plataforma .NET, pudiendo ser utilizada en varios sistemas operativos. Además, este software dispone de un interfaz de usuario muy intuitivo, capacidad de extraer automáticamente distintos tipos de metadatos (fecha, hora, fase lunar, localización, temperatura, presión atmosférica, etc), basados en el estándar Exif; disponibilidad de listas taxonómicas para permitir a los usuarios etiquetar fácilmente las imágenes con las identidades de las especies, capacidad de análisis y creación de informes. El uso de esta aplicación ha permitido simplificar el procesado, análisis y edición de datos, consiguiendo una significativa reducción de los costes económicos y temporales. Mientras que en el procesado manual se alcanzaba una media de 55 fotografías/hora, el uso de esta herramienta permite procesar más de 1,000 fotografías/hora, obteniendo una mayor cantidad de información. Finalmente, se pone de manifiesto la gran utilidad de esta aplicación, que puede ser adaptada a las necesidades de otros proyectos de gestión de fauna, haciendo su uso extensivo no solamente a los profesionales del sector, sino a todos aquellos que requieran procesar gran cantidad de imágenes de fototrampeo.

Letter from William Croswell to James Scott, 1803 November 1

One-page letter from Croswell to Captain James Scott, Master of the Boston Marine Society, that accompanied Croswell's work on lunar observations.

Memorial to the Academy of Arts and Sciences, 1826 April

Four drafts of a letters requesting support to reprint Croswell's 1791 Tables for Computing the Longitude by the Lunar Observations, with two related documents.

Memorial to the Academy of Arts and Sciences, 1828 April

Five drafts of a letters requesting support to reprint Croswell's 1791 Tables for Computing the Longitude by the Lunar Observations.

Annotated almanac, 1766

Almanac containing three laid-in pages with handwritten notes and a few sporadic corrections to the rising and setting times of the moon on the calendar pages. The three laid-in pages consist of a small scrap of paper with the weights of the family, and two folded pages with notes about a lunar eclipse on August 20, 1766.

John Winthrop's proposal respecting electrical globes and jars, ca. 1758

In this proposal, John Winthrop explains the need to replace damaged "electric globes" used in the College's collection of scientific apparatus. He states that Benjamin Franklin, at the time residing in London, was willing to seek replacement globes for the College's collection. Winthrop then proceeds to assert that the College should acquire "square bottles, of a moderate size, fitted in a wooden box, like what they call case bottles for spirits" instead of the large jars included in the scientific apparatus, because those jars cracked frequently.

Letter from James Winthrop to William Bentley, 1801 February 12

Two folio-sized leaves containing a one-and-a-half-page handwritten letter from Winthrop to Bentley discussing lunar tables, plans to publish, and a recent gem acquisition. The letter ends, "So Adams is OUT," referring to United States President John Adams's reelection defeat.