Carbon geochemistry in serpentinites from and beneath the Lost City Hydrothermal Field

The carbon geochemistry of serpentinized peridotites and gabbroic rocks recovered at the Lost City Hydrothermal Field (LCHF) and drilled at IODP Hole 1309D at the central dome of the Atlantis Massif (Mid-Atlantic Ridge, 30°N) was examined to characterize carbon sources and speciation in oceanic basement rocks affected by long-lived hydrothermal alteration. Our study presents new data on the geochemistry of organic carbon in the oceanic lithosphere and provides constraints on the fate of dissolved organic carbon in seawater during serpentinization. The basement rocks of the Atlantis Massif are characterized by total carbon (TC) contents of 59 ppm to 1.6 wt% and 17863_TC values ranging from -28.7? to +2.3?. In contrast, total organic carbon (TOC) concentrations and isotopic compositions are relatively constant (d13C_TOC: -28.9? to -21.5?) and variations in d13CTC reflect mixing of organic carbon with carbonates of marine origin. Saturated hydrocarbons extracted from serpentinites beneath the LCHF consist of n-alkanes ranging from C15 to C30. Longer-chain hydrocarbons (up to C40) are observed in olivine-rich samples from the central dome (IODP Hole 1309D). Occurrences of isoprenoids (pristane, phytane and squalane), polycyclic compounds (hopanes and steranes) and higher relative abundances of n-C16 to n-C20 alkanes in the serpentinites of the southern wall suggest a marine organic input. The vent fluids are characterized by high concentrations of methane and hydrogen, with a putative abiotic origin of hydrocarbons; however, evidence for an inorganic source of n-alkanes in the basement rocks remains equivocal. We propose that high seawater fluxes in the southern part of the Atlantis Massif likely favor the transport and incorporation of marine dissolved organic carbon and overprints possible abiotic geochemical signatures. The presence of pristane, phytane and squalane biomarkers in olivine-rich samples associated with local faults at the central dome implies fracture-controlled seawater circulation deep into the gabbroic core of the massif. Thus, our study indicates that hydrocarbons account for an important proportion of the total carbon stored in the Atlantis Massif basement and suggests that serpentinites may represent an important (as yet unidentified) reservoir for dissolved organic carbon (DOC) from seawater.

Geochemistry of Atlantis Massif crust

The Atlantis Massif (Mid-Atlantic Ridge, 30°N) is an oceanic core complex marked by distinct variations in crustal architecture, deformation and metamorphism over distances of at least 5 km. We report Sr and Nd isotope data and Rare Earth Element (REE) concentrations of gabbroic and ultramafic rocks drilled at the central dome (IODP Hole 1309D) and recovered by submersible from the southern ridge of the massif that underlie the peridotite-hosted Lost City Hydrothermal Field. Systematic variations between the two areas document variations in seawater penetration and degree of fluid-rock interaction during uplift and emplacement of the massif and hydrothermal activity associated with the formation of Lost City. Homogeneous Sr and Nd isotope compositions of the gabbroic rocks from the two areas (87Sr/86Sr: 0.70261-0.70429 and epsilon-Nd: +9.1 to +12.1) indicate an origin from a depleted mantle. At the central dome, serpentinized peridotites are rare and show elevated seawater-like Sr isotope compositions related to serpentinization at shallow crustal levels, whereas unaltered mantle isotopic compositions preserved in the gabbroic rocks attest to limited seawater interaction at depth. This portion of the massif remained relatively unaffected by Lost City hydrothermal activity. In contrast, pervasive alteration and seawater-like Sr and Nd isotope compositions of serpentinites at the southern wall (87Sr/86Sr: 0.70885-0.70918; epsilon-Nd: -4.7 to +11.3) indicate very high fluid-rock ratios (~20 and up to 10**6) and enhanced fluid fluxes during hydrothermal circulation. Our studies show that Nd isotopes are most sensitive to high fluid fluxes and are thus an important geochemical tracer for quantification of water-rock ratios in hydrothermal systems. Our results suggest that high fluxes and long-lived serpentinization processes may be critical to the formation of Lost City-type systems and that normal faulting and mass wasting in the south facilitate seawater penetration necessary to sustain hydrothermal activity.

Sulphur mineralogy and geochemistry of serpentinites and gabbros from the Atlantis Massif

In-situ uplifted portions of oceanic crust at the central dome of the Atlantis Massif (Mid-Atlantic Ridge, 30°N) were drilled during Expeditions 304 and 305 of the Integrated Ocean Drilling Program (IODP) and a 1.4 km section of predominantly gabbroic rocks with minor intercalated ultramafic rocks were recovered. Here we characterize variations in sulfur mineralogy and geochemistry of selected samples of serpentinized peridotites, olivine-rich troctolites and diverse gabbroic rocks recovered from Hole 1309D. These data are used to constrain alteration processes and redox conditions and are compared with the basement rocks of the southern wall of the Atlantis Massif, which hosts the Lost City Hydrothermal Field, 5 km to the south. The oceanic crust at the central dome is characterized by Ni-rich sulfides reflecting reducing conditions and limited seawater circulation. During uplift and exhumation, seawater interaction in gabbroic-dominated domains was limited, as indicated by homogeneous mantle-like sulfur contents and isotope compositions of gabbroic rocks and olivine-rich troctolites. Local variations from mantle compositions are related to magmatic variability or to interaction with seawater-derived fluids channeled along fault zones. The concomitant occurrence of mackinawite in olivine-rich troctolites and an anhydrite vein in a gabbro provide temperature constraints of 150-200 °C for late circulating fluids along local brittle faults below 700 m depth. In contrast, the ultramafic lithologies at the central dome represent domains with higher seawater fluxes and higher degrees of alteration and show distinct changes in sulfur geochemistry. The serpentinites in the upper part of the hole are characterized by high total sulfide contents, high d34Ssulfide values and low d34Ssulfate values, which reflect a multistage history primarily controlled by seawater-gabbro interaction and subsequent serpentinization. The basement rocks at the central dome record lower oxygen fugacities and more limited fluid fluxes compared with the serpentinites and gabbros of the Lost City hydrothermal system. Our studies are consistent with previous results and indicate that sulfur speciation and sulfur isotope compositions of altered oceanic mantle sequences commonly evolve over time. Heterogeneities in sulfur geochemistry reflect the fact that serpentinites are highly sensitive to local variations in fluid fluxes, temperature, oxygen and sulfur fugacities, and microbial activity.

Nicklinson v Ministry of Justice [2012] 304 (QB) : further UK developments regarding a person's right to choose when and how to die : assisted termination of life

UK High Court decision - application for declarations legitimising third party assistance in voluntary termination of life - facts - moral, social and ethical issues - analysis.

A Curious Harpour in Helle : An Edition of the Commentary on the Orpheus Metre of De consolatione philosophiae in MS Thott 304,2

Tutkielmani on tekstieditio keskiaikaisesta kommentaarista, joka löytyy Kööpenhaminan Kuninkaallisen kirjaston käsikirjoituksesta Thott 304,2. Käsikirjoitus voidaan ajoittaa 1400-luvun ensimmäiselle neljännekselle ja se on kirjoitettu keskienglanniksi. Se sisältää John Waltonin runomuotoisen käännöksen Boethiuksen 500-luvun alussa latinaksi kirjoittamasta teoksesta De consolatione philosophiae (Filosofian lohdutus) sekä teosta kommentoivan proosamuotoisen kommentaarin. Käsikirjoitus on vaillinainen, mutta sen säilyneet foliot ovat enimmäkseen erittäin hyväkuntoisia. Itse käsikirjoitusta on tutkittu vain muutamissa artikkeleissa ja yhdessä tutkielmassa; kommentaarista ei ole toistaiseksi tehty kattavaa tutkimusta. Tavoitteeni onkin tuoda kommentaari keskiaikaisen filosofian, keskienglannin ja käsikirjoitusten tutkijoiden käytettäviin. Käsikirjoitus Thott 304,2 on esimerkki epätyypillisestä myöhäiskeskiaikaisesta maallikkomesenaattiudesta Englannissa. Tavanmukaisesti maallikkomesenaatit tukivat uskonnollisten tekstien tuottamista ja kääntämistä, kun taas Thott 304,2 sisältää käännöksen filosofisesta tekstistä. Sen lisäksi mesenaatti oli nainen, aatelistoon kuuluva Elizabeth Berkeley. Varsin harvinaiseksi käsikirjoituksen tekee sen painaminen kirjaksi 1500-luvun alussa. Kirjanpainajan käsikirjoituksen sivuille tekemistä merkinnöistä saadaan korvaamatonta tietoa varhaisesta painotekniikasta, sillä kirjanpainajien käyttämiä käsikirjoituskopioita ei ole säilynyt kovin runsaasti. Waltonin käännös on säilynyt yli kahdessakymmenessä käsikirjoituskopiossa, joista vain Thott 304,2 sisältää laajan kommentaarin. 1500-luvun painoksesta on jäljellä kolme kopiota, ja ne sisältävät saman kommentaarin kuin Thott 304,2. Valitsin editoitavaksi niin kutsuttua Orfeus-runoa kommentoivan osan kommentaarista, sillä se muodostaa ehjän kokonaisuuden ja sopii pituutensa puolesta Pro gradu -tutkielmaan. Orfeus-runo on myös yksi käsikirjoituksen kattavimmin kommentoiduista runoista. Editio on niin sanottu diplomaattinen transkriptio, jossa käsikirjoituksen piirteet on pyritty säilyttämään mahdollisimman tarkasti edition luettavuuden siitä kuitenkaan kärsimättä. Perinteisistä editioista poiketen tutkielmani sisältää myös kommentaarin ja Orfeus-runon transkriptiot, joissa rivijako, lyhenteet ja erikoismerkit on säilytetty. Näiden transkriptioiden toivon auttavan erityisesti käsikirjoituksessa esiintyvien lyhenteiden, erikoismerkkien ja kirjanpainajan merkintöjen tulkinnassa ja tutkimisessa. Editiota ja transkriptioita täydentävät nykyenglanniksi kirjoitettu lyhennelmä kommentaarista ja kuvat käsikirjoituksen sivuista, joilla editoimani kommentaari on. Tutkielmaan sisältyy alkuperäisen tekstin, käännöksen, kommentaarin ja käsikirjoituksen taustaa valottava osuus. Esittelen myös kaikki löytämäni lähteet, joissa käsikirjoitus on mainittu tai joissa sitä on tutkittu. Liitteeksi olen laatinut sanaston helpottamaan kommentaarin tulkitsemista.

Influence of cast versus wrought microstructure on the processing map for hot working of stainless steel type AISI 304

Processing maps for hot working of as-cast and wrought stainless steels of type AISI 304 have been developed in the temperature range 600 to 1250°C and strain rate range 0.001 to 100 s−1. The domain of dynamic recrystallization (DRX) in as-cast material occurs at higher temperatures (1250°C) and lower strain rates (0.001 s−1) than in the wrought steel (1100°C and 0.01 s−1). The effect is explained in terms of enhanced nucleation rate of DRX due to the carbide, ferrite particles, stable oxides/nitrides and second-phase intermetallics in the as-cast microstructure. The DRX domain is wider in the wrought material although the peak efficiency is less (32%) than in the as-cast case (40%). The flow instability regime is not significantly affected by the initial microstructure

Influence of strain rate and state-of-stress on the formation of ferrite in stainless steel type AISI 304 during hot working

The influence of strain rate and state-of-stress on the formation of ferrite in stainless steel type AISI 304L, 304 and 304 as-cast, during hot working has been studied. Compression and torsion tests were conducted in the temperature range 1100 to 1250 degrees C and strain rate range 0.001 to 100 s(-1) on these materials, Ferrite formation occurs during deformation at temperatures above 1150 degrees C and strain rates above 10 s(-1), in stainless steel type AISI 304L and 304. The tendency for the formation of ferrite is more in as-cast 304 than in wrought 304, In as-cast 304 the ferrite forms at lower temperatures and strain rates, The tendency for the ferrite formation is more in torsion than in compression.