Primordial condensation of meteorite components — Experimental evidence of the state of the source medium     

G. Arrhenius  J. L. McCrumb  N. Friedman 《Astrophysics and Space Science》1979,65(2):297-307

Mineral grains and grain aggregates in meteorites carry potential information on the conditions in the environment where they formed. To avoid model-dependent interpretations it is necessary to develop experimental criteria that uniquely reflect the environmental parameters of interest. These parameters include the various temperatures of the source medium and the temperature of grains at growth, all of which are observed to be highly differentiated in the space medium in accordance with the radiation laws.Independent tests are also necessary to establish the chemical composition of the source medium which appears from the meteorite record to have been variable. Another important variable is the number density which is observed to span over more than twelve orders of magnitude in the domains in space where dust is being modified by condensation or evaporation.Metal diffusion couples in the interior of refractory mineral grains (melilite and spinel) indicate that these couples and their refractory host grains may have existed up to a year at 780 K. They could have supported temperatures lower than 900 K more than a day but cannot have formed at grain temperatures of the order of 1700 K as is assumed in some theories.The temperature parameters of the source medium are more difficult to determine from the record in meteorite minerals; assessments, in order to be realistic, have to be made within the bounds of the observed properties of the space medium. Kinetic isotope effects, imprinted together with nuclear effects on meteorite solids, provide a promising source of information on fractionation processes and on the state of excitation in the source medium. Theoretical and experimental verification of the isotope fractionation mechanisms, which may be responsible for the observed effects, are thus of importance.Invited contribution to the Proceedings of a Workshop onThermodynamics and Kinetics of Dust Formation in the Space Medium held at the Lunar and Planetary Institute, Houston, 6–8 September, 1978.  相似文献   

Use of composite data sets for source-tracking enterococci in the water column and shoreline interstitial waters on Pensacola Beach, Florida     

Genthner FJ  James JB  Yates DF  Friedman SD 《Marine pollution bulletin》2005,50(7):724-732

Sources of Enterococcus faecalis isolates from Pensacola Beach, FL. were identified using a library-based approach by applying the statistical method of average similarity to single and composite data sets generated from separate analyses. Data sets included antibiotic resistance analysis (ARA), rep-fingerprints, and fatty acid methyl ester (FAME) profiles. Use of a composite data set composed of ARA and rep-fingerprints, added to the confidence of the identifications. The addition of FAME data to composite data sets did not add to the confidence of identifications. Source identification was performed to better understand risk associated with higher densities of enterococci found in swash zone interstitial water (SZIW) as compared to adjacent bathing water on Pensacola Beach, FL. The "swash zone" is that area of the beach continually washed over by waves. As the potential sources of enterococci were limited in this environment, only two library units, sea gull and human, were constructed. Identification of the beach isolates using a composite data set indicated a sea gull origin. The clonality of the beach isolates suggested that the beach environment selects certain subspecies of E. faecalis.  相似文献   

Book reviews     

M. Friedman  H. Körner  L. Müller  A. Watznauer  G. Beurle 《Rock Mechanics and Rock Engineering》1970,2(3):177-180

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Early carbonate diagenesis in slope sequences and at their boundaries, Cenozoic, offshore New Jersey (ODP Leg 150): comment     

G. M. Friedman 《International Journal of Earth Sciences》1999,88(1):163-164

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Statistical techniques for the classification of chromites in diamond exploration samples     

W.L. Griffin  N.I. Fisher  J.H. Friedman  C.G. Ryan 《Journal of Geochemical Exploration》1997,59(3):233-249

A database of 1267 quality-screened major- and trace-element analyses of chromites (s.l.) from kimberlites, lamproites, ultramafic lamprophyres (UMLs) and crustal sources (‘greenstones’, including ophiolites, gabbros, basalts and komatiites) has been subjected to statistical analysis, in order to derive discriminants for use in diamond exploration. The techniques used included nearest-neighbour analysis, CART (classification and regression trees) and MARS (multivariate adaptive regression splines). The results show that both CART and MARS approaches can correctly discriminate kimberlite/lamproite chromites from UML/‘greenstone’ chromites at levels near 90%. Discrimination into the four classes separately is achieved at levels of ca. 80% by MARS and > 70% by CART; much of the misclassification is between the kimberlite and lamproite classes. These results probably represent the maximum probable level of discrimination on chemical criteria, given that ascending magmas may sample both mantle and crustal rocks. The CART approach produces a classification tree that requires no further computation to classify a given grain; the MARS approach requires the use of a simple software package. Tests on known samples illustrate the high level of accuracy of the methods in an exploration context, as well as the useful petrogenetic conclusions that can be drawn from some ‘misclassifications’.  相似文献   

GhostNet marine debris survey in the Gulf of Alaska--satellite guidance and aircraft observations     

Pichel WG  Veenstra TS  Churnside JH  Arabini E  Friedman KS  Foley DG  Brainard RE  Kiefer D  Ogle S  Clemente-Colón P  Li X 《Marine pollution bulletin》2012,65(1-3):28-41

Marine debris, particularly debris that is composed of lost or abandoned fishing gear, is recognized as a serious threat to marine life, vessels, and coral reefs. The goal of the GhostNet project is the detection of derelict nets at sea through the use of weather and ocean models, drifting buoys and satellite imagery to locate convergent areas where nets are likely to collect, followed by airborne surveys with trained observers and remote sensing instruments to spot individual derelict nets. These components of GhostNet were first tested together in the field during a 14-day marine debris survey of the Gulf of Alaska in July and August 2003. Model, buoy, and satellite data were used in flight planning. A manned aircraft survey with visible and IR cameras and a LIDAR instrument located debris in the targeted locations, including 102 individual pieces of debris of anthropogenic or terrestrial origin.  相似文献   

Metasomatized lithospheric mantle beneath Turkana depression in southern Ethiopia (the East Africa Rift): geochemical and Sr–Nd–Pb isotopic characteristics     

Daniel Meshesha  Ryuichi Shinjo  Risa Matsumura  Takele Chekol 《Contributions to Mineralogy and Petrology》2011,162(5):889-907

Mantle xenoliths entrained in Quaternary alkaline basalts from the Turkana Depression in southern Ethiopia (the East Africa Rift) were studied for their geochemical and Sr–Nd–Pb isotopic compositions to constrain the evolution of the lithosphere. The investigated mantle xenoliths are spinel lherzolites in composition with a protogranular texture. They can be classified into two types: anhydrous and hydrous spinel lherzolites; the latter group characterized by the occurrences of pargasite and phlogopite. The compositions of whole-rock basaltic component (CaO = 3.8–5.6 wt%, Al₂O₃ = 2.5–4.1 wt%, and MgO = 34.7–38.1 wt%), spinel (Cr# = 0.062–0.117, Al₂O₃ = 59.0–64.4 wt%) and clinopyroxene (Mg# = 88.4–91.7, Al₂O₃ = 5.2–6.7 wt%) indicate that the lherzolites are fertile and have not experienced significant partial melting. Both types are characterized by depleted ⁸⁷Sr/⁸⁶Sr (0.70180–0.70295) and high ¹⁴³Nd/¹⁴⁴Nd (0.51299–0.51348) with wide ranges of ²⁰⁶Pb/²⁰⁴Pb (17.86–19.68) isotopic compositions. The variations of geochemical and isotopic compositions can be explained by silicate metasomatism induced by different degree of magma infiltrations from ascending mantle plume. The thermobarometric estimations suggest that the spinel lherzolites were derived from depths of 50–70 km (15.6–22.2 kb) and entrained in the alkaline magma at 847–1,052°C. Most of the spinel lherzolites from this study record an elevated geotherm (60–90 mW/m²) that is related to the presence of rising mantle plume in an active tectonic setting. Sm–Nd isotopic systematic gives a mean T_DM model age of 0.95 Ga, interpreted as the minimum depletion age of the subcontinental lithosphere beneath the region.  相似文献   

Response of a phytoplankton community to nutrient addition under different CO2 and pH conditions     

Takeo Hama  Tomoki Inoue  Risa Suzuki  Hiroto Kashiwazaki  Shigeki Wada  Daisuke Sasano  Naohiro Kosugi  Masao Ishii 《Journal of Oceanography》2016,72(2):207-223

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Evaluation of mussel immune responses as indicators of contamination in San Francisco Bay     

Luengen AC  Friedman CS  Raimondi PT  Flegal AR 《Marine environmental research》2004,57(3):197-212

Several immune parameters were evaluated in two species of mussels (Mytilus californianus and M. galloprovincialis/M. trossulus) as bioindicators of contaminant effects. The mussels were deployed in San Francisco Bay Estuary and a control site at Bodega Marine Laboratory. Assays for phagocytosis and phagocytic index (average number of particles engulfed per hemocyte) were conducted with hemocytes in their own hemolymph-the "Serum" method. The responses were compared with contaminant concentrations in those mussels. For both species, the contaminated South Bay Dumbarton Bridge and Redwood Creek sites had elevated phagocytosis relative to the Bodega control site, indicating contaminant stress. The results also showed that M. californianus had higher percentages of phagocytosis (74%) and a higher phagocytic index (4.6 particles per cell) than those of M. galloprovincialis/M. trossulus (60% phagocytosis and 3.5 particles per cell). As there is a difference in immune response to contaminants, it is suggested that future San Francisco Estuary monitoring should be conducted with endemic M. galloprovincialis/M. trossulus rather than with the currently utilized M. californianus, which is not found in the estuary.  相似文献   

Marine debris collects within the North Pacific Subtropical Convergence Zone   总被引：1，自引：0，他引：1  

Pichel WG  Churnside JH  Veenstra TS  Foley DG  Friedman KS  Brainard RE  Nicoll JB  Zheng Q  Clemente-Colón P 《Marine pollution bulletin》2007,54(8):1207-1211

Floating marine debris, particularly derelict fishing gear, is a hazard to fish, marine mammals, turtles, sea birds, coral reefs, and even human activities. To ameliorate the economic and environmental impact of marine debris, we need to efficiently locate and retrieve dangerous debris at sea. Guided by satellite-derived information, we made four flights north of Hawaii in March and April 2005. During these aerial surveys, we observed over 1800 individual pieces of debris, including 122 derelict fishing nets. The largest debris concentrations were found just north of the North Pacific Transition Zone Chlorophyll Front (TZCF) within the North Pacific Subtropical Convergence Zone (STCZ). Debris densities were significantly correlated with sea-surface temperature (SST), chlorophyll-a concentration (Chla), and the gradient of Chla. A Debris Estimated Likelihood Index (DELI) was developed to predict where high concentrations of debris would be most likely in the North Pacific during spring and early summer.  相似文献