Environmental modeling with precision navigation using ROAZ autonomous surface vehicle

The use of robotic vehicles for environmental modeling is discussed. This paper presents diverse results in autonomous marine missions with the ROAZ autonomous surface vehicle. The vehicle can perform autonomous missions while gathering marine data with high inertial and positioning precision. The underwater world is an, economical and environmental, asset that need new tools to study and preserve it. ROAZ is used in marine environment missions since it can sense and monitor the surface and underwater scenarios. Is equipped with a diverse set of sensors, cameras and underwater sonars that generate 3D environmental models. It is used for study the marine life and possible underwater wrecks that can pollute or be a danger to marine navigation. The 3D model and integration of multibeam and sidescan sonars represent a challenge in nowadays. Adding that it is important that robots can explore an area and make decisions based on their surroundings and goals. Regard that, autonomous robotic systems can relieve human beings of repetitive and dangerous tasks.

Assessment of non-steroidal anti-inflammatory and analgesic pharmaceuticals in seawaters of North of Portugal: Occurrence and environmental risk

The occurrence of seven pharmaceuticals and two metabolites belonging to non-steroidal anti-inflammatory drugs and analgesics therapeutic classes was studied in seawaters. A total of 101 samples covering fourteen beaches and five cities were evaluated in order to assess the spatial distribution of pharmaceuticals among north Portuguese coast. Seawaters were selected in order to embrace different bathing water quality (excellent, good and sufficient). Acetaminophen, ketoprofen and the metabolite hydroxyibuprofen were detected in all the seawater samples at maximum concentrations of 584, 89.7 and 287 ng L− 1, respectively. Carboxyibuprofen had the highest seawater concentration (1227 ng L− 1). The temporal distribution of the selected pharmaceuticals during the bathing season showed that, in general, higher concentrations were detected in August and September. The environmental risk posed by the pharmaceuticals detected in seawaters towards different trophic levels (fish, daphnids and algae) was also assessed. Only diclofenac showed hazard quotients above one for fish, representing a potential risk for aquatic organisms. These results were observed in seawaters classified as excellent bathing water. Additional data is needed in order to support the identification and prioritization of risks posed by pharmaceuticals in marine environment.

Regional change in the Algarve: A Geographic Information System approach

Thesis submitted to the Instituto Superior de Estatística e Gestão de Informação da Universidade Nova de Lisboa in partial fulfillment of the requirements for the Degree of Doctor of Philosophy in Information Management – Geographic Information Systems

New natural hydraulic lime mortars – Physical and microstructural properties in different curing conditions

Construction and Building Materials 54 (2014) 378–384

Dieta da torda-mergulheira, Alca torda, capturada acidentalmente em Portugal Continental

Dissertação de mestrado em Ecologia

Ingestão de plásticos por aves marinhas na Costa Norte de Portugal

Dissertação de mestrado em Ecologia

Plastic ingestion by sea turtles in Paraíba State, Northeast Brazil

ABSTRACT Currently, plastics are recognized as a major pollutant of the marine environment, representing a serious threat to ocean wildlife. Here, we examined the occurrence and effects of plastic ingestion by sea turtles found stranded along the coast of Paraíba State, Brazil from August 2009 to July 2010. Ninety-eight digestive tracts were examined, with plastic found in 20 (20.4%). Sixty five percent (n = 13) of turtles with plastic in the digestive tract were green turtles (Chelonia mydas), 25% (n = 5) were hawksbills (Eretmochelys imbricata), and 10% (n = 2) were olive ridley (Lepidochelys olivacea). More plastic was found in the intestine (85%) than in other parts of the gastrointestinal tract. We observed complete blockage of the gastrointestinal tract due to the presence of plastic in 13 of the 20 turtles that had ingested plastic. No correlation was found between the curved carapace length (CCL) and the number or mass of the plastic ingested items. Significant differences were found between the intake of hard and soft plastic and the ingestion of white/transparent and colored plastic, with soft and white/transparent plastics being more commonly ingested. This study reveals the serious problem of plastic pollution to sea turtles at the area.

Migration of sharks into freshwater systems during the Miocene and implications for Alpine paleoelevation

Trace-element and isotopic compositions of fossilized shark teeth sampled from Miocene marine sediments of the north Alpine Molasse Basin, the Vienna Basin, and the Pannonian Basin generally show evidence of formation in a marine environment under conditions geochemically equivalent to the open ocean. In contrast, two of eight shark teeth from the Swiss Upper Marine Molasse locality of La Moliere have extremely low delta O-18 values (10.3% and 11.3%) and low Sr-87/Sr-86 ratios (0.707840 and 0.707812) compared to other teeth from this locality (21.1%,22.4%o and 0.708421-0.708630). The rare earth element (REE) abundances and patterns from La Moliere not only differ between dentine and enameloid of the same tooth, but also between different teeth, supporting variable conditions of diagenesis at this site. However, the REE patterns of enameloid from the ``exotic'' teeth analyzed for O and Sr isotopic compositions are similar to those of teeth that have O and Sr isotopic compositions typical of a marine setting at this site. Collectively, this suggests that the two ``exotic'' teeth were formed while the sharks frequented a freshwater environment with very low O-18-content and Sr isotopic composition controlled by Mesozoic calcareous rocks. This is consistent with a paleogeography of high-elevation (similar to 2300 m) Miocene Alps adjacent to a marginal sea.

From Naples 1963 to Rome 2013 - A brief review of how the International Research Group on Ostracoda (IRGO) developed as a social communication system

The 1st International Symposium on Ostracoda (ISO) was held in Naples (1963). The philosophy behind this symposium and the logical outcome of what is now known as the International Research Group on Ostracoda (IRGO) is here reviewed, namely ostracodology over the last 50 years is sociologically analysed. Three different and important historic moments for the scientific achievements of this domain are recognised. The first one, between about 1963-1983, is related to applied research for the oil industry as well as to the great interest in the better description of the marine environment by both zoologists and palaeontologists. Another important aspect during this period was the work by researchers dealing with Palaeozoic ostracods, who had their own discussion group, IRGPO. Gradually, the merger of this latter group with those dealing with post-Palaeozoic ostracods at various meetings improved communication between the two groups of specialists. A second period was approximately delineated between 1983 and 2003. During this time-slice, more emphasis was addressed to environmental research with topics such as the study of global events and long-term climate change. Ostracodologists profited also from the research "politics" within national and international programmes. Large international research teams emerged using new research methods. During the third period (2003-2013), communication and collaborative research reached a global dimension. Amongst the topics of research we cite the reconstruction of palaeoclimate using transfer functions, the building of large datasets of ostracod distributions for regional and intercontinental studies, and the implementation of actions that should lead to taxonomic harmonisation. Projects within which molecular biological techniques are routinely used, combined with sophisticated morphological information, expanded now in their importance. The documentation of the ostracod description improved through new techniques to visualise morphological details, which stimulated also communication between ostracodologists. Efforts of making available ostracod information through newsletters and electronic media are evoked.

Governança das áreas marinhas protegidas da província biogeográfica da Macaronésia

As áreas marinhas protegidas (AMPs), enquanto instrumentos de conservação da natureza, contribuem para a conservação, preservação e gestão dos ecossistemas costeiros e marinhos a nível mundial. Na Província Biogeográfica da Macaronésia, as AMPs existentes desempenham este papel de forma preponderante, principalmente no que diz respeito às espécies com impacte económico local. A governança consiste nas interacções entre estruturas, processos e tradições, as quais determinam como são exercidas as responsabilidades, como as decisões são tomadas e como é que a opinião dos cidadãos e grupos de interesse (stakeholders) é integrada no processo de decisão. Assim, a governança das AMPs é um factor determinante para o seu sucesso. Foi estudada a governança das AMPs na Província Biogeográfica da Macaronésia (arquipélagos dos Açores, Madeira, Canárias e Cabo Verde), com a finalidade de verificar se o actual estado de estabelecimento e gestão de AMPs nos quatro arquipélagos é ou não favorável a uma governança conjunta do meio marinho nesta província biogeográfica, tendo em vista os objectivos de conservação da natureza à escala global. Foi desenvolvida uma metodologia própria baseada na análise do quadro legal nacional e internacional e das estruturas governativas das AMPs, e ainda em entrevistas no arquipélago com menor disponibilidade de informação (Cabo Verde). Conclui-se que os três países que fazem parte da área de estudo detêm os quadros legais (internacional, regional e nacional) e institucional considerados suficientes para a conservação dos ecossistemas costeiros e marinhos. Esta análise permitiu a definição de acções que poderão ser desenvolvidas pelos quatro arquipélagos, visando uma gestão conjunta integrada das AMPs na área de estudo. Apesar de existirem vários diplomas e regulamentos jurídicos a nível nacional/regional sobre a conservação marinha, há ainda um longo caminho a percorrer no que diz respeito aos planos de gestão destinados a promover uma abordagem integrada da conservação à escala biogeográfica

Stable isotope and trace element stratigraphy across the Permian-Triassic transition: A redefinition of the boundary in the Velebit Mountain, Croatia

Stable isotopes of carbonates (delta(13)C(carb), delta(18)O(carb)), organic matter (delta(13)C(org), delta(15)N(org)) and major, trace and rare earth element (REE) compositions of marine carbonate rocks of Late Permian to Early Triassic age were used to establish the position of the Permian-Triassic boundary (PTB) at two continuous sections in the Velebit Mountain, Croatia. The chosen sections - Rizvanusa and Brezimenjaca - are composed of two lithostratigraphic units, the Upper Permian Transitional Dolomite and the overlying Sandy Dolomite. The contact between these units, characterized by the erosional features and sudden occurrence of ooids and siliciclastic grains, was previously considered as the chronostratigraphic PTB. The Sandy Dolomite is characterized by high content of non-carbonate material (up to similar to 30 wt.% insoluble residue), originated from erosion of the uplifted hinterland. A relatively rich assemblage of Permian fossils (including Geinitzina, Globivalvulina, Hemigordius, bioclasts of gastropods, ostracods and brachiopods) was found for the first time in Sandy Dolomite, 5 m above the lithologic boundary in the Rizvanusa section. A rather abrupt negative delta(13)C(carb) excursion in both sections appears in rocks showing no recognizable facies change within the Sandy Dolomite, -2 parts per thousand at Rizvanusa and -1.2 parts per thousand at Brezimenjaca, 11 m and 0.2 m above the lithologic contact, respectively. This level within the lower part of the Sandy Dolomite is proposed as the chemostratigraphic PTB. In the Rizvanusa section, the delta(13)C(org) values decline gradually from similar to-25 parts per thousand in the Upper Permian to similar to-29 parts per thousand in the Lower Triassic. The first negative delta(13)C(org) excursion occurs above the lithologic contact, within the uppermost Permian deposits, and appears to be related to the input of terrigenous material. The release of isotopically light microbial soil-biomass into the shallow-marine water may explain this sudden decrease of delta(13)C(org) values below the PTB. This would support the hypothesis that in the western Tethyan realm the land extinction, triggering a sudden drop of woody vegetation and related land erosion, preceded the marine extinction. The relatively low delta(15)N(org) values at the Permian-Triassic (P-Tr) transition level, close to approximate to 0 parts per thousand, and a secondary negative delta(13)C(org) excursion of -0.5 parts per thousand point to significant terrestrial input and primary contribution of cyanobacteria. The profiles of the concentrations of redox-sensitive elements (Ce, Mn, Fe, V), biogenic or biogenic-scavenged elements (P, Ba, Zn, V), Ce/Ce* values, and normalized trace elements, including Ba/Al, Ba/Fe, Ti/Al, Al/(Al + Fe + Mn) and Mn/Ti show clear excursions at the Transitional Dolomite-Sandy Dolomite lithologic boundary and the chemostratigraphic P-Tr boundary. The stratigraphic variations indicate a major regression phase marking the lithologic boundary, transgressive phases in the latest Permian and a gradual change into shallow/stagnant anoxic marine environment towards the P-Tr boundary level and during the earliest Triassic. (C) 2010 Elsevier B.V. All rights reserved.

Reconstructing mid-to-recent Holocene paleoenvironments in the vicinity of ancient Amarynthos (Euboea, Greece).

This article examines the shoreline evolution and human occupation in the vicinity of the important archeological site of Amarynthos (Euboea Island, Greece) over the last six millennia. Archeological evidence indicates a continuous occupation of the site from the Bronze Age to the Roman period and the site is well-known, thanks to the existence of a sanctuary dedicated to the goddess Artemis. Based on the study of four boreholes, a paleogeographic reconstruction of the coastal landscape is proposed. Facies were determined based on mollusc identification, and sedimentology based on grain-size measurements (hand sieving for the fraction above 2 mm and LASER technique for particles below 2 mm) and loss-on-ignition. In addition, a series of 12 AMS radiocarbon dates define a reliable chronostratigraphy. Results suggest the presence of a fully marine environment from the early Holocene to ca. 2600-2400 cal. BC, which developed into a brackish environment from ca. 2600-2400 cal. BC to ca. 750 cal. BC due to the deltaic progradation of the nearby stream (Sarandapotamos River). From ca. 750 cal. BC onward, coastal swamps prevailed in the study area. Human-environmental interaction is discussed and particular attention is paid to the paleolandscape configuration of Amarynthos.

El ambiente marino durante el invierno 2002: Crucero demersal BIC Humboldt 0209

El Crucero BIC Humboldt 0209 se realizó del 8 al 27 de setiembre entre Huarmey y Puerto Pizarro. Las observaciones más importantes fueron: (1) recuperación de las condiciones frías al sur de 5°S, con ATSM por encima de lo normal, principalmente entre 4°-5°S (+3 °C), debido al desplazamiento hacia el sur del frente ecuatorial; (2) mayor presencia de las aguas costeras frías (ACF) asociadas al afloramiento, que dio lugar al retiro parcial de las aguas subtropicales superficiales (ASS), que estuvieron próximas a la costa en meses anteriores, y al repliegue de la Extensión Sur de la Corriente de Cromwell (ESCC); (3) ascenso de isoter-mas subsuperficiales, que en los cruceros 0205 y 0208 se hallaron profundizadas; (4) reactivación de zonas de afloramiento, aunque no muy marcadas, frente a Casma, Chicama, Punta Falsa y Paita.

El ambiente marino costero de la Región La Libertad 2010

Entre el 26 abril y 10 mayo 2010, se efectuó la evaluación del ambiente costero de la región La Libertad, determinándose que Huanchaco, Salaverry y Magdalena de Cao tienen el más alto grado de contaminación marina. Salaverry y Magdalena de Cao presentan los valores más bajos de diversidad bentónica y de volumen de plancton. Las variables oceanográficas primarias se debieron a procesos de surgencia recientes. La concentración de sólidos suspendidos totales de Chérrepe cumplió con los Estándares Nacionales de Calidad Ambiental para Agua. La calidad acuática del río Moche presenta valores que sobrepasan la norma vigente.

Producción primaria en el ambiente marino en el Pacífico sudeste, Perú, 1960-2000

Los resultados de investigación sobre producción primaria dentro del alcance interdisciplinario del ambiente marino frente a la costa peruana incluyen estudios nacionales, extranjeros y de investigación conjunta a través de proyectos internacionales (1960-2000). La circulación en la costa peruana es dominada por una corriente hacia el ecuador en una capa de 20 a 50 m. La estructura de plumas del afloramiento se presenta en cada área y podría ser la clave para el desarrollo de cadenas cortas y productivas: fitoplancton peces clupeidos. La distribución de nutrientes sigue la pluma de temperatura, con altos valores en la costa y bajos lejos de la costa; la clorofila muestra mínimos valores cerca de la costa (10 mn) que se incrementa al alejarse. El crecimiento del fitoplancton en aguas peruanas, varía de 0,5 a 0,8 d/d. En aguas recién afloradas el crecimiento es limitado por falta de “condicionamiento biológico” y de compuestos orgánicos (15°S). Estos tipos de agua pueden estar relacionados con las “aguas azules” de altos nutrientes y pobre fitoplancton con células de pequeño tamaño (clorofila <2 μg/L) y con “aguas marrones” con denso fitoplancton, (clorofila >5 μg/L), mayor diversidad y con células de diámetro >5μ. La media de producción primaria fue 3 gC/m2/d (1960-1985), comparable a la mayoría de estudios en los cuales varía entre 3 y 4 gC/m2/d en la franja costera, el último valor es altamente variable en espacio, siendo más frecuente dentro de 10 km. Valores mayores de 12 gC/m2/d se encontraron en el afloramiento de Chimbote. El Niño, La Niña y fases del ENSO, afectan la producción primaria. Las temperaturas bajas originan cambios en la composición química del fitoplancton y reducen el índice de productividad mgC/mgclor-a/d que también es atribuido a limitaciones de luz.