Pacific Neogene carbonate accumulation rates

I have compiled CaCO3 mass accumulation rates (MARs) for the period 0-25 Ma for 144 Deep Sea Drilling Project and Ocean Drilling Program drill sites in the Pacific in order to investigate the history of CaCO3 burial in the world's largest ocean basin. This is the first synthesis of data since the beginning of the Ocean Drilling Program. Sedimentation rates, CaCO3 contents, and bulk density were estimated for 0.5 Myr time intervals from 0 to 14 Ma and for 1 Myr time intervals from 14 to 25 Ma using mostly data from Initial Reports volumes. There is surprisingly little coherence between CaCO3 MAR time series from different Pacific regions, although regional patterns exist. A transition from high to low CaCO3 MAR from 23-20 Ma is the only event common to the entire Pacific Ocean. This event is found worldwide. The most likely cause of lowered pelagic carbonate burial is a rising sea-level trend in the early Miocene. The central and eastern equatorial Pacific is the only region with adequate drill site coverage to study carbonate compensation depth (CCD) changes in detail for the entire Neogene. The latitude-dependent decrease in CaCO3 production away from the equator is an important defining factor of the regional CCD, which shallows away from the equatorial region. Examination of latitudinal transects across the equatorial region is a useful way to separate the effects of changes in carbonate production ('productivity') from changes in bottom water chemistry ('dissolution') upon carbonate burial.

Global compilation of benthic data sets I

Approaches to quantify the organic carbon accumulation on a global scale generally do not consider the small-scale variability of sedimentary and oceanographic boundary conditions along continental margins. In this study, we present a new approach to regionalize the total organic carbon (TOC) content in surface sediments (<5 cm sediment depth). It is based on a compilation of more than 5500 single measurements from various sources. Global TOC distribution was determined by the application of a combined qualitative and quantitative-geostatistical method. Overall, 33 benthic TOC-based provinces were defined and used to process the global distribution pattern of the TOC content in surface sediments in a 1°x1° grid resolution. Regional dependencies of data points within each single province are expressed by modeled semi-variograms. Measured and estimated TOC values show good correlation, emphasizing the reasonable applicability of the method. The accumulation of organic carbon in marine surface sediments is a key parameter in the control of mineralization processes and the material exchange between the sediment and the ocean water. Our approach will help to improve global budgets of nutrient and carbon cycles.

Global data compilation of benthic data sets II

In this study we present a global distribution pattern and budget of the minimum flux of particulate organic carbon to the sea floor (J POC alpha). The estimations are based on regionally specific correlations between the diffusive oxygen flux across the sediment-water interface, the total organic carbon content in surface sediments, and the oxygen concentration in bottom waters. For this, we modified the principal equation of Cai and Reimers [1995] as a basic monod reaction rate, applied within 11 regions where in situ measurements of diffusive oxygen uptake exist. By application of the resulting transfer functions to other regions with similar sedimentary conditions and areal interpolation, we calculated a minimum global budget of particulate organic carbon that actually reaches the sea floor of ~0.5 GtC yr**-1 (>1000 m water depth (wd)), whereas approximately 0.002-0.12 GtC yr**-1 is buried in the sediments (0.01-0.4% of surface primary production). Despite the fact that our global budget is in good agreement with previous studies, we found conspicuous differences among the distribution patterns of primary production, calculations based on particle trap collections of the POC flux, and J POC alpha of this study. These deviations, especially located at the southeastern and southwestern Atlantic Ocean, the Greenland and Norwegian Sea and the entire equatorial Pacific Ocean, strongly indicate a considerable influence of lateral particle transport on the vertical link between surface waters and underlying sediments. This observation is supported by sediment trap data. Furthermore, local differences in the availability and quality of the organic matter as well as different transport mechanisms through the water column are discussed.

Corg, CaCO3, bulk densities, accumulation rates and ages of ODP Leg 167 sites and three piston cores, California margin

Sediments from five Leg 167 drill sites and three piston cores were analyzed for Corg and CaCO3. Oxygen isotope stratigraphy on benthic foraminifers was used to assign age models to these sedimentary records. We find that the northern and central California margin is characterized by k.y.-scale events that can be found in both the CaCO3 and Corg time series. We show that the CaCO3 events are caused by changes in CaCO3 production by plankton, not by dissolution. We also show that these CaCO3 events occur in marine isotope Stages (MIS) 2, 3, and 4 during Dansgaard/Oeschger interstadials. They occur most strongly, however, on the MIS 5/4 glaciation and MIS 2/1 deglaciation. We believe that the link between the northeastern Pacific Ocean and North Atlantic is primarily transmitted by the atmosphere, not the ocean. Highest CaCO3 production and burial occurs when the surface ocean is somewhat cooler than the modern ocean, and the surface mixed layer is somewhat more stable.

Carbon and oxygen isotopic composition of benthic foraminifers from ODP Leg 167 sites

Three sites, drilled during Ocean Drilling Program (ODP) Leg 167, were chosen for detailed late Pleistocene paleoceanographic studies of intermediate water along the California margin. These sites are Site 1011 (Animal Basin, 31°17'N, 117°38'W, 2033 m water depth, 1600 m sill depth), Site 1012 (East Cortez Basin, 32°17'N, 118°23'W, 1783 m water depth, 1415 m sill depth), and Site 1018 (Guide Seamount, 36°59'N, 123°17'W, 2476 m water depth). Here we present carbon and oxygen isotopic measurements of benthic foraminifers from these three sites. We made 135 measurements from Site 1011, 387 measurements from Site 1012, and 231 measurements from Site 1018. This data report includes an explanation of the methods used to generate these isotopic records and the age models for each site. Detailed paleoceanographic interpretations of the isotopic records are currently under way.

The Roman Republican Navy : from the sixth century to 167 BC

Työ käsittelee Rooman laivaston kehitystä, toimintaa ja osallistumista laajenemispolitiikkaan, jossa Rooma kasvoi kaupunkivaltiosta Välimeren hallitsijaksi. Rooma on aikaisemmissa tutkimuksissa nähty maavaltiona vailla kiinnostusta merenkulkuun. On katsottu, että ainoa merkittävä merisota Rooman historiassa on ensimmäinen puunilaissota (264-241 eKr.) ja että siinäkin roomalaiset (jotka historioitsija Polybius kuvaa vasta-alkajiksi) menestyivät Karthagoa vastaan turvautumalla laskusiltoihin, joiden avulla he saattoivat muuttaa meritaistelun maataisteluksi. Polybiuksen kuvaukseen on aina tähän asti luotettu. On katsottu että Roomalla ei ollut laivastoa ennen ensimmäistä puunilaissotaa ja että Rooma kaikissa sodissaan panosti merisodankäyntiin mahdollisimman vähän. Tämä työ pyrkii kumoamaan nämä käsitykset. Laivasto oli osallisena ja ehdottoman välttämätön kaikissa Rooman laajenemispolitiikan käänteissä. Arkeologian tiedot osoittavat, että ennen ensimmäistä puunilaissotaa Rooma kehittyi ja siitä tuli merkittävä kaupunki nimenomaan kaupankäynnin ja ulkomaisten kontaktien seurauksena. Se ei siis ollut puhdas agraarivaltio. Roomalaisilla oli laivasto jo viimeistään 500-luvulta lähtien eKr. ja sitä käytettiin Rooman laajentaessa valtaansa Italiassa. Näin ollen ensimmäisessä puunilaissodassa läntisen Välimeren herruudesta kilpaili kaksi merivaltiota, Rooma ja Karthago. Toinen puunilaissota (218-201) tunnetaan yleensä Hannibalin tulosta Alppien yli Italiaan, mutta se oli myöskin merkittävä merisota ja karthagolaiset hävisivät sen nimenomaan merellä. Rooma osallistui kilpailuun itäisen Välimeren hallinnasta ja kukisti Makedonian ja Syyrian laivastot, jotka eivät olleet mitenkään Rooman laivaston veroisia. Kaikista Rooman vastustajista Karthagolla olisi ollut suurin mahdollisuus pysäyttää Rooman laivaston voittokulu toisessa puunilaissodassa. Laivastoa käytettiin moniin eri tarkoituksiin. Suuret meritaistelut eivät ole ainoa osoitus laivastojen mukanaolosta ja merkityksestä, vaan on myös otettava huomion sotalaivojen rakenne ja toimintaedellytykset. Sotalaivat oli rakennettu taisteluita varten ja niissä oli hyvin niukasti säilytystilaa. Niiden oli päästävä laskemaan maihin aina kun miehistö tarvitsi vettä, ruokaa ja lepoa. Laivastot saattoivat toimia vain niiden rannikoiden tuntumassa, joiden satamiin ja laskupaikkoihin niillä oli turvallinen pääsy. Roomalaiset olivat hyvin tietoisia tästä. Suuret merentakaiset sotaretket Afrikkaan, Espanjaan, Kreikkaan ja Vähän-Aasian rannikolle perustuivat kaikki siihen, että Rooman laivasto hallitsi purjehdusreittejä ja sopivia laskupaikkoja ja saattoi huolehtia joukkojen ja varusteiden kuljettamisesta kaukana taisteleville armeijoille. Samalla Rooman laivasto kävi itsenäistä sotaa merellä ja haastoi ja kukisti kaikki Välimeren merivaltiot. 130-luvulle eKr. tultaessa se oli lyönyt vihollisensa ja riisunut aseista liittolaisensa; Rooman laivasto hallitsi Välimerta yksin.

Sapientia, 1988, Vol. XLIII, nº 167-168 (número completo)

Contenido: El tema de la libertad en Santo Tomás : fuentes y desarrollo / Gustavo E. Ponferrada – Emergencia y sentido del hombre en la reflexión ética de la Suma contra Gentiles / Julio R. Méndez – Azar y contingencia / Juan J. Sanguineti – Indeterminismo y racionalidad : en torno al problema de la causalidad en física / Ramón Queraltó – La tridimensionalidad crítica de la reflexión completa / Stanislavs Ladusans – Humanismo y humanismos / Iulio Brandao – Limitación de la antropología filosófica / José M. de Estrada – Afectividad, obrar humano, moralidad / María C. Donadío de Gandolfi – Naturaleza y ética en Hobbes y Tomás de Aquino / María L. Lukac de Stier – Derecho, pensamiento y lenguaje / Carlos I. Massini-Correas – Derecho natural y positivismo jurídico / Ylves J. de Miranda Guimaraes – La verdad política es el ideal de una sociedad participativa / José P. Galvao de Sousa – Hombre y moral : la “pietas” patriótica / Héctor H. Hernández – Filosofía, teología y cultura cristiana en el pensamiento de San Agustín / Battista Mondin – Amor Ruibal, genial renovador de la filosofía cristiana / Emilio Silva de Castro – La problemática filosófica de las ciencias humanas / Edgardo J. Castro

Aperfeiçoamentos no DL nº 167/67 : emolumentos extrajudiciais e garantias reais em Cédulas de Crédito Rural-CCR e em Cédulas de Crédito Bancário-CCB

Consultoria de Orçamento e Fiscalização Financeira.

Diário da Constituinte [gravação de vídeo] : [programa n. 167]

Começa a primeira sessão dedicada ao debate dos temas mais polêmicos na Constituinte. O Líder do PMDB Mário Covas (PMDB-SP) fez o sorteio dos debatedores do partido que vão ficar encarregados de cada sessão. O primeiro assunto é o regime de governo, presidencialismo ou parlamentarismo. O Conselho de Comunicação também é tema polêmico na Assembleia Nacional Constituinte (ANC). A Deputada Rita Furtado (PFL-RO) informa que seu grupo não aceita a figura do Conselho. O Deputado Bernardo Cabral (PMDB-AM), Relator da Comissão de Sistematização, opta pela existência do Conselho, previsto no substitutivo do Deputado Artur da Távola (PMDB-RJ). O Deputado Arolde de Oliveira (PFL-RJ) informa que o Conselho é desnecessário, pois o Congresso tem função fiscalizadora. Armando Rollemberg, Presidente da Federação Nacional dos Jornalistas, defende o controle público para a concessão de canais de rádio e de televisão. O Deputado Roberto D`Ávila (PDT-RJ) declara que é favorável ao Conselho de Comunicação, com pessoas representativas da sociedade brasileira, de tal forma que o poder de outorga de canais de comunicação não seja mais prerrogativa apenas do Presidente da República. Histórico da ideia de criação do Conselho de Comunicação. O Deputado Jorge Maluly Neto (PFL-SP) declara que a opinião pública há de ser pública e não uma opinião publicada por poucos, porque isso leva a um problema de segurança do país. O Deputado Arolde de Oliveira (PFL-RJ) considera que não tem havido alternância do poder porque, se houvesse, também a distribuição de canais de rádio e de tv seria absolutamente democrática. O Deputado Carlos Alberto Oliveira Caó (PDT-RJ) afirma ser necessário pensar em mecanismos que assegurem a pluralidade de informações, que garanta a qualquer grupo social o acesso aos meios de informação. O Deputado Antônio Brito (PMDB-RS) declara que é certo que nada nesta matéria será da forma como é hoje, o que já significa um avanço.

Prey consumption of Steller sea lions (Eumetopias jubatus) off Alaska: How much prey do they require?

The effects of seasonal and regional differences in diet composition on the food requirements of Steller sea lions (Eumetopias jubatus) were estimated by using a bioenergetic model. The model considered differences in the energy density of the prey, and differences in digestive efficiency and the heat increment of feeding of different diets. The model predicted that Steller sea lions in southeast Alaska required 45–60% more food per day in early spring (March) than after the breeding season in late summer (August) because of seasonal changes in the energy density of the diets (along with seasonal changes in energy requirements). The southeast Alaska population, at 23,000 (±1660 SD) animals (all ages), consumed an estimated 140,000 (±27,800) t of prey in 1998. In contrast, we estimated that the 51,000 (±3680) animals making up the western Alaska population in the Gulf of Alaska and Aleutian Islands consumed just over twice this amount (303,000 [±57,500] t). In terms of biomass removed in 1998 from Alaskan waters, we estimated that Steller sea lions accounted for about 5% of the natural mortality of gadids (pollock and cod) and up to 75% of the natural mortality of hexagrammids (adult Atka mackerel). These two groups of species were consumed in higher amounts than any other. The predicted average daily food requirement per individual ranged from 16 (±2.8) to 20 (±3.6) kg (all ages combined). Per capita food requirements differed by as much as 24% between regions of Alaska depending on the relative amounts of low–energy-density prey (e.g. gadids) versus high–energy-density prey (e.g. forage fish and salmon) consumed. Estimated requirements were highest in regions where Steller sea lions consumed higher proportions of low–energy-density prey and experienced the highest rates of population decline