Ley orgánica y reglamentaria de instrucción pública, reformada por los decretos números 3-193-268-295-297-301-312-333-432-445-469-604 y acuerdos gubernativos que figuran al fin.

Mode of access: Internet.

Discurso sobre contribuciones : presentado al Gobierno en 3 de marzo de 1817 /

Palau,

Esposicion [sic] dirijida [sic] al Congreso de Señores Diputados en 3 de abril de 1943 : sobre que se declaren acrisolados sus servicios y se le reponga en su destino, de que se halla separado hace mas de cinco años por la injusticia mas escandalosa /

Mode of access: Internet.

Aviso al publico sobre el proximo paso de Venus por delante del Sol, que debe suceder el 3 de junio de 1769 :

Mode of access: Internet.

Apuntaciones sobre el plebiscito pactado en el artc̕ulo 3. del Tratado de Ancn̤, puestas en forma de exposicin̤ al arbitro, designado en el protocolo Billinghurst-Latorre, del 16 de abril de 1898.

At head of title: Contribucin̤ al rescate de las provincias cautivas.

Sopra la lingua italiana ed altro appartenente al buon gusto [To which is added "A sua eccellenza il Signor Marchese Luigi Rangoni, epistola 3."]

Mode of access: Internet.

Storia dell'amministrazione del Regno d'Italia durante il dominio francese : preceduta l. Da un indice cronologico de' principali avvenimenti risguardanti l'Italia dal 1792 fino al 1814 : 2. da un catalogo alfabetico di quegl'Italiani e Francesi, che servendo dello regno, si fecero distinguere colle loro azioni, colle lor'opere, o cogl'impieghi che hanno coperti : 3. da una introduzione, nella quale si esamina la situazione d'Italia al momento, in cui fu invasa da' Francesi nel 1796, non che lo stato di questo paese fino al 1805, epoca della fondazione del regno : terminata da una tavola dei nomi e delle materie /

Includes index.

Memoria que en cumplimiento á lo prescrito en el reglamento de aguas del Reino de 3. de Febrero de 1834, dirige al Esmo Señor Ministro de la Governacion del Reino el Dor. en Medicina y Cirujia Dn. Juan Carlos Guerra, Director de las aguas hidro-sulfurosas y ferruginosas de Sta. Agueda en Mondragon, relatibo á lo obserbado en la temporada de uso de aguas del año de 1848.

Carece de portada.

Actas, informes, resoluciones y locumentación general de la Alta Comisión Internacional de Legislación Uniforme, reunida en Buenos Aires del 3 al 12 de Abril de 1916,

Mode of access: Internet.

Isotopes content, mineralogical composition, Uranium and Thorium contents and determined activity ratios from METEOR cruise M74/3 in 2007

Authigenic carbonate deposits have been sampled with the remotely operated vehicle 'MARUM-QUEST 4000 m' from five methane seeps between 731 and 1823 m water depth along the convergent Makran continental margin, offshore Pakistan (northern Arabian Sea). Two seeps on the upper slope are located within the oxygen minimum zone (OMZ; ca. 100 to 1100 m water depth), the other sites are situated in oxygenated water below the OMZ (below 1100 m water depth). The carbonate deposits vary with regard to their spatial extent, sedimentary fabrics, and associated seep fauna: Within the OMZ, carbonates are spatially restricted and associated with microbial mats, whereas in the oxygenated zone below the OMZ extensive carbonate crusts are exposed on the seafloor with abundant metazoans (bathymodiolin mussels, tube worms, galatheid crabs). Aragonite and Mg-calcite are the dominant carbonate minerals, forming common early diagenetic microcrystalline cement and clotted to radial-fibrous cement. The delta18O carbonate values range from 1.3 to 4.2 per mil V-PDB, indicating carbonate precipitation at ambient bottom-water temperature in shallow sediment depth. Extremely low delta13Ccarbonate values (as low - 54.6per mil V-PDB) point to anaerobic oxidation of methane (AOM) as trigger for carbonate precipitation, with biogenic methane as dominant carbon source. Prevalence of biogenic methane in the seepage gas is corroborated by delta13C methane values ranging from - 70.3 to - 66.7per mil V-PDB, and also by back-calculations considering delta 13C methane values of carbonate and incorporated lipid biomarkers.

Phytoplankton composition derived from CHEMTAX along 10°E during POLARSTERN cruise ANT-XXVIII/3, Jan-March 2012

Phytoplankton community structure and their physiological response in the vicinity of the Antarctic Polar Front (APF; 44°S to 53°S, centred at 10°E) were investigated as part of the ANT-XXVIII/3 Eddy-Pump cruise conducted in austral summer 2012. Our results show that under iron-limited (< 0.3 µmol/m**3) conditions, high total chlorophyll-a (TChl-a) concentrations (> 0.6 mg/m**3) can be observed at stations with deep mixed layer (> 60 m) across the APF. In contrast, light was excessive at stations with shallower mixed layer and phytoplankton were producing higher amounts of photoprotective pigments, diadinoxanthin (DD) and diatoxanthin (DT), at the expense of TChl-a, resulting in higher ratios of (DD+DT)/ TChl-a. North of the APF, significantly lower silicic acid (Si(OH)4) concentrations (< 2 mmol/m**3) lead to the domination of nanophytoplankton consisting mostly of haptophytes, which produced higher ratios of (DD+DT)/TChl-a under relatively low irradiance conditions. The Si(OH)4 replete (> 5 mmol/m**3) region south of the APF, on the contrary, was dominated by microphytoplankton (diatoms and dinoflagellates) with lower ratios of (DD+DT)/TChl-a, despite having been exposed to higher levels of irradiance. The significant correlation between nanophytoplankton and (DD+DT)/TChl-a indicates that differences in taxon-specific response to light are also influencing TChl-a concentration in the APF during summer. Our results reveal that provided mixing is deep and Si(OH)4 is replete, TChl-a concentrations higher than 0.6 mg/m**3 are achievable in the iron-limited APF waters during summer.