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Journal articles on the topic 'Diablo Range'

Author: Grafiati

Published: 28 July 2024

Last updated: 31 July 2025

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1

Verdone, Chris J., and Boris C. Kondratieff. "Malenka Diablo, A New Species Of Stonefly From The Diablo Range Of California, U.S.A. (Plecoptera: Nemouridae)." Illiesia 14, no. 6 (2018): 126–34. https://doi.org/10.5281/zenodo.4758021.

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Verdone, Chris J., Kondratieff, Boris C. (2018): Malenka Diablo, A New Species Of Stonefly From The Diablo Range Of California, U.S.A. (Plecoptera: Nemouridae). Illiesia 14 (6): 126-134, DOI: http://doi.org/10.5281/zenodo.4758021

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2

Pluta, Agnieszka, Agata Wrzesien-Kus, Barbara Cebula, et al. "The Prognostic Role of Smac/DIABLO Protein Expression in Acute Myeloid Leukemia." Blood 114, no. 22 (2009): 2626. http://dx.doi.org/10.1182/blood.v114.22.2626.2626.

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Abstract Abstract 2626 Poster Board II-602 Background: Smac/DIABLO (second mitochondrial derived activator of caspase/direct IAP binding protein with low pI), an antagonist of inhibitor of apoptosis proteins (IAP) family, was shown to trigger both external and internal apoptosis pathways in acute leukemia cell lines. The role, pathway of action and prognostic significance of Smac/DIABLO protein is not clearly determined in acute myeloid leukemia (AML) patients. Aims: The main objective of this study was to verify whether expression of Smac/DIABLO protein has a prognostic impact on response to

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3

Wasson, John T., and Xinwei Ouyang. "Compositional range in the Canyon Diablo meteoroid." Geochimica et Cosmochimica Acta 54, no. 11 (1990): 3175–83. http://dx.doi.org/10.1016/0016-7037(90)90132-5.

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4

ERNST, W. G. "Metamorphism of Franciscan tectonostratigraphic assemblage, Pacheco Pass area, east-central Diablo Range, California Coast Ranges." Geological Society of America Bulletin 105, no. 5 (1993): 618–36. http://dx.doi.org/10.1130/0016-7606(1993)105<0618:moftap>2.3.co;2.

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5

Pluta, Agnieszka, Agata Wrzesien-Kus, Barbara Cebula-Obrzut, et al. "The Role of Inhibitor of Apoptosis Proteins Family Expression In Acute Myeloid Leukemia Patients." Blood 116, no. 21 (2010): 2728. http://dx.doi.org/10.1182/blood.v116.21.2728.2728.

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Abstract Abstract 2728 Background: IAPs (Inhibitor of Apoptosis Proteins) family acts as an inhibitor of both external and internal apoptosis pathways by binding to specific caspases. These proteins also participate in intracellular signal transduction. Seven human IAPs have been identified: XIAP, cIAP-1, cIAP-2, survivin, livin, NAIP and BRUCE/Apollon. IAPs family can be inhibited by Smac/DIABLO (second mitochondrial derived activator of caspase/direct IAP binding protein with low pI) protein. The role, pathway of action and prognostic significance of IAPs family is not clearly determined in

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6

Jacobson, Hayden L., Danica L. Roth, Gabriel Walton, Margaret Zimmer, and Kerri Johnson. "Post-fire evolution of ravel transport regimes in the Diablo Range, CA." Earth Surface Dynamics 12, no. 6 (2024): 1415–46. https://doi.org/10.5194/esurf-12-1415-2024.

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Abstract. Post-fire changes to the transport regime of dry ravel, which describes the gravity-driven transport of individual particles downslope, are poorly constrained but critical to understand as ravel may contribute to elevated sediment fluxes and associated debris flow activity observed post-fire in the western United States. In this study, we evaluated post-fire variability in dry ravel travel distance exceedance probabilities and disentrainment rates in the Diablo Range of central coastal California following the Santa Clara Unit Lightning Complex fire of August 2020. Between March 2021

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7

PATRICK, B. E., and H. W. DAY. "Controls on the first appearance of jadeitic pyroxene, northern Diablo Range, California." Journal of Metamorphic Geology 7, no. 6 (1989): 629–39. http://dx.doi.org/10.1111/j.1525-1314.1989.tb00623.x.

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8

Fry, Danny L. "Prescribed Fire Effects on Deciduous Oak Woodland Stand Structure, Northern Diablo Range, California." Rangeland Ecology & Management 61, no. 3 (2008): 294–301. http://dx.doi.org/10.2111/07-113.1.

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9

Harms, T. A., A. S. Jayko, and M. C. Blake. "Kinematic evidence for extensional unroofing of the Franciscan Complex along the Coast Range Fault, Northern Diablo Range, California." Tectonics 11, no. 2 (1992): 228–41. http://dx.doi.org/10.1029/91tc01880.

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10

Baldwin, Bruce G. "Lagophylla diabolensis(Compositae–Madiinae), a New Hare-Leaf from the Southern Diablo Range, California." Madroño 60, no. 3 (2013): 249–54. http://dx.doi.org/10.3120/0024-9637-60.3.249.

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11

Tembayashi, M., S. Maruyama, and J. G. Liou. "Thermobaric Structure of the Franciscan Complex in the Pacheco Pass Region, Diablo Range, California." Journal of Geology 104, no. 5 (1996): 617–36. http://dx.doi.org/10.1086/629855.

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12

Erskine, Bradley G., and Mark Bailey. "Characterization of asbestiform glaucophane-winchite in the Franciscan Complex blueschist, northern Diablo Range, California." Toxicology and Applied Pharmacology 361 (December 2018): 3–13. http://dx.doi.org/10.1016/j.taap.2018.09.020.

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13

Kim, Daeyeong, Ikuo Katayama, Katsuyoshi Michibayashi, and Tatsuki Tsujimori. "Rheological contrast between glaucophane and lawsonite in naturally deformed blueschist from Diablo Range, California." Island Arc 22, no. 1 (2012): 63–73. http://dx.doi.org/10.1111/iar.12003.

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14

BROTHERS, R. N., and R. H. GRAPES. "Clastic lawsonite, glaucophane, and jadeitic pyroxene in Franciscan metagraywackes from the Diablo Range, California." Geological Society of America Bulletin 101, no. 1 (1989): 14–26. http://dx.doi.org/10.1130/0016-7606(1989)101<0014:clgajp>2.3.co;2.

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15

Hohn, Rachel A., Khalil P. Abusaba, Erin N. Bray, et al. "Ongoing mercury contamination downstream from the former New Idria Mercury Mine: Southern diablo range of the California coast ranges." PLOS Water 4, no. 6 (2025): e0000328. https://doi.org/10.1371/journal.pwat.0000328.

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California’s mining legacy continues to threaten water quality and ecosystem health throughout the state. This study focuses on mercury (Hg) releases from the former New Idria Mercury Mine, which was the second largest historic Hg producer in North America. San Carlos Creek, which flows adjacent to the mine, is impacted by acid mine drainage (AMD) as well as mining waste piles that sit at a high angle of repose over the channel. We documented total mercury (HgT) concentrations exceeding California’s 50 ng L-1 water quality objective for almost 10 km, from New Idria to a ~ 0.25 km2 perennial we

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16

Dalla Torre, Michael, Kenneth J. T. Livi, and Martin Frey. "Chlorite textures and compositions from high-pressure/low-temperature metashales and metagraywackes, Franciscan Complex, Diablo Range, California, USA." European Journal of Mineralogy 8, no. 4 (1996): 825–46. http://dx.doi.org/10.1127/ejm/8/4/0825.

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17

Hagstrum, Jonathan T., and David L. Jones. "Paleomagnetism, paleogeographic origins, and uplift history of the Coast Range ophiolite at Mount Diablo, California." Journal of Geophysical Research: Solid Earth 103, B1 (1998): 597–603. http://dx.doi.org/10.1029/97jb02785.

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18

Raymond, Loren A. "Origin of Mélanges of the Franciscan Complex, Diablo Range and Northern California: An Analysis and Review." Geosciences 9, no. 8 (2019): 338. http://dx.doi.org/10.3390/geosciences9080338.

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The Franciscan Complex of California is characterized in part by the presence of mélanges. In general, mélange origins are attributed to sedimentary, tectonic, or diapiric processes—or a combination of these. Published reviews list the main features of mélanges characteristic of each type of origin. In this review, particular diagnostic features typical of sedimentary, tectonic, and diapiric mélanges are used to assess 15 specific mélanges, which in some cases have been interpreted in contrasting ways in the literature. The data do not support the view that most Franciscan mélanges were formed

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19

RAYMOND, LOREN A. "Clastic lawsonite, glaucophane, and jadeitic pyroxene in Franciscan metagraywackes from the Diablo Range, California: Alternative interpretation." Geological Society of America Bulletin 103, no. 7 (1991): 970–72. http://dx.doi.org/10.1130/0016-7606(1991)103<0970:clgajp>2.3.co;2.

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20

Ortega-Ramírez, Jose R., Alfonso Valiente-Banuet, Jaime Urrutia-Fucugauchi, Carlos A. Mortera-Gutiérrez, and Guillermo Alvarado-Valdez. "Paleoclimatic changes during the Late Pleistocene - Holocene in Laguna Babícora, near the Chihuahuan Desert, México." Canadian Journal of Earth Sciences 35, no. 10 (1998): 1168–79. http://dx.doi.org/10.1139/e98-060.

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The paleoclimatic variability of northern Mexico since the Late Wisconsinan is determined from sedimentological, geochemical, and stratigraphic studies of the lacustrine sequence of Laguna Babícora (29.4°N, 107.7°W; elevation 2100 m asl). Chronological control is based on 13 radiocarbon dates (6 from this study and 7 previously reported) from four stratigraphic profiles that cover a range from 16 342 to 2800 BP. Two major periods of increased humidity are recognized by lake-level variation during the Late Wisconsinan and early Holocene. The Late Wisconsinan humid period may be related to jet s

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21

Torre, M. Dalla, Kenneth J. T. Livi, David R. Veblen, and M. Frey. "White K-mica evolution from phengite to muscovite in shales and shale matrix melange, Diablo Range, California." Contributions to Mineralogy and Petrology 123, no. 4 (1996): 390–405. http://dx.doi.org/10.1007/s004100050164.

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22

Dalla Torre, M., C. De Capitani, M. Frey, M. B. Underwood, J. Mullis, and R. Cox. "Very low-temperature metamorphism of shales from the Diablo Range, Franciscan Complex, California: New constraints on the exhumation path." Geological Society of America Bulletin 108, no. 5 (1996): 578. http://dx.doi.org/10.1130/0016-7606(1996)108<0578:vltmos>2.3.co;2.

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23

Nereson, Alexander L., and Noah J. Finnegan. "Drivers of earthflow motion revealed by an 80 yr record of displacement from Oak Ridge earthflow, Diablo Range, California, USA." GSA Bulletin 131, no. 3-4 (2018): 389–402. http://dx.doi.org/10.1130/b32020.1.

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24

Ernst, W. G., and Shohei Banno. "Neoblastic jadeitic pyroxene in Franciscan metagreywackes from Pacheco Pass, central Diablo Range, California, and implications for the inferred metamorphic P‐T trajectory." New Zealand Journal of Geology and Geophysics 34, no. 3 (1991): 285–92. http://dx.doi.org/10.1080/00288306.1991.9514466.

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25

Grapes, R. H., and W. G. Ernst. "Neoblastic jadeitic pyroxene in Franciscan metagreywackes from Pacheco Pass, central Diablo Range, California, and implications for the inferred metamorphic P‐T trajectory." New Zealand Journal of Geology and Geophysics 35, no. 3 (1992): 381–87. http://dx.doi.org/10.1080/00288306.1992.9514532.

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26

Moleski, Nicholas, Anthony Boxleiter, and Joyashish Thakurta. "Sulfur Isotope Ratios from VMS Deposits in the Penokean Volcanic Belt, Great Lakes Region, USA: Constraints on the Source of Sulfur in a Paleoproterozoic Intra-Arc Rift." Minerals 9, no. 1 (2018): 6. http://dx.doi.org/10.3390/min9010006.

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The Paleoproterozoic (~1.8 Ga) Penokean Volcanic Belt (PVB) in the Great Lakes Region of North America hosts several polymetallic volcanogenic massive sulfide (VMS) deposits. These deposits were formed by back-arc extensional volcanism during the accretion of island-arc terranes along the southern margin of the Archean Superior Craton. This study reports δ34S values obtained from sulfide minerals collected from eight VMS deposits in the PVB: Back Forty, Bend, Eisenbrey, Flambeau, Horseshoe, Lynne, Reef, and Schoolhouse. The average δ34S values from most of these deposits lie within the mantle-

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27

Kelly, Thomas S., and J. D. Stewart. "New records of Middle and Late Miocene perissodactyla and artiodactyla from the western border of the San Joaquin valley Diablo Range, Fresno county, California." Contributions in science 516 (November 7, 2008): 1–29. http://dx.doi.org/10.5962/p.226784.

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28

Kelly, Thomas S., and J. D. Stewart. "New records of Middle and Late Miocene perissodactyla and artiodactyla from the western border of the San Joaquin valley Diablo Range, Fresno county, California." Contributions in science 516 (November 7, 2008): 1–29. http://dx.doi.org/10.5962/p.226784.

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29

Turbin, V., Yu Dementev, and I. Kenyo. "Production peculiarities of Brussels sprouts in Crime for conveyor delivery of its heads to the retail chain." E3S Web of Conferences 176 (2020): 03006. http://dx.doi.org/10.1051/e3sconf/202017603006.

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The results of a long-term study on the theoretical foundation of the adaptation capabilities of Brussels sprouts of the Franklin F1 and Diablo F1 hybrids to growing in the natural and climatic conditions of Crimea are figured. Recommended terms of outdoor transplanting of seedlings, substantiated the acceptance of the cultivation Brussels sprouts in winter culture, shows the duration of the phases of laying, growth, development and maturation of Brussels sprouts. The proposed elements of growing technology permit to wide the range of vegetables consumed by the population of Crimea, prolong th

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30

Maruyama, S., J. G. Liou, and Y. Sasakura. "Low-temperature recrystallization of Franciscan greywackes from Pacheco Pass, California." Mineralogical Magazine 49, no. 352 (1985): 345–55. http://dx.doi.org/10.1180/minmag.1985.049.352.05.

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AbstractLow-temperature metamorphism of the Franciscan complex at Pacheco Pass occurs at P-T conditions near the so-called jadeite isograd. Along Highway 152 in the Diablo Range, from west to east, four distinct prograde metamorphic zones are defined: (I) albite-quartz zone, (II) albite-rich, albite-quartz-clinopyroxene assemblage, (III) clinopyroxene-rich, albite-quartz-clinopyroxene assemblage, and (IV) clinopyroxene zone. Metamorphic pyroxenes are restricted to zones II, III, and IV in metagreywackes, but metabasites contain augite-rich pyroxenes even in zone I. With increasing grade, the c

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31

Huber, M. V., and A. V. Mokrushin. "Sulfur isotope signatures of sulfides from the Khibina and Lovozero massifs (Kola Alkaline Province, Fennoscandian Shield)." Vestnik MGTU 24, no. 1 (2021): 80–87. http://dx.doi.org/10.21443/1560-9278-2021-24-1-80-87.

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The sulfur isotope geochemistry of the Khibina and Lovozero agpaitic massifs provides an opportunity to understand the role of plume-lithosphere interaction processes responsible for the Paleozoic alkaline igneous activity in the north-eastern part of the Fennoscandian Shield. The stable sulfur isotope δS analysis using triple collector isotope ratio mass spectrometer (IRMS) has been carried out on the pentlandite, chalcopyrite and pyrite from nepheline syenites. The δS values for pentlandite from Khibina rocks range from +0.69 to +2.06 ‰ relative to the Vienna Canyon Diablo Troillite standard

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32

Hunt, Julie A., Tim Baker, James Cleverley, Garry J. Davidson, Anthony E. Fallick, and Derek J. Thorkelson. "Fluid inclusion and stable isotope constraints on the origin of Wernecke Breccia and associated iron oxide – copper – gold mineralization, Yukon." Canadian Journal of Earth Sciences 48, no. 10 (2011): 1425–45. http://dx.doi.org/10.1139/e11-044.

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Iron oxide – Cu ± Au ± U ± Co (IOCG) mineralization is associated with numerous Proterozoic breccia bodies, collectively known as Wernecke Breccia, in Yukon Territory, Canada. Multiphase breccia zones occur in areas underlain by Paleoproterozoic Wernecke Supergroup metasedimentary rocks and are associated with widespread sodic, potassic, and carbonate alteration assemblages. Fluid inclusion data indicate syn-breccia fluids were hot (185–350 °C) saline (24–42 wt.% NaCl equivalent) NaCl–CaCl2–H2O brines. Estimates of fluid pressure vary from 0.4 to 2.4 kbar (1 kbar = 100 MPa). Carbon and oxygen

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33

Liu, Lijuan, Jeremy P. Richards, Robert A. Creaser, S. Andrew DuFrane, Karlis Muehlenbachs, and Peter B. Larson. "Geology and age of the Morrison porphyry Cu–Au–Mo deposit, Babine Lake area, British Columbia." Canadian Journal of Earth Sciences 53, no. 9 (2016): 950–78. http://dx.doi.org/10.1139/cjes-2015-0231.

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The Morrison porphyry Cu–Au–Mo deposit is genetically and spatially related to Eocene plagioclase–hornblende–biotite porphyry intrusions. One porphyry intrusion yielded a U–Pb age of 52.54 ± 1.05 Ma. Mineralization occurs in three stages: (1) vein-type and disseminated chalcopyrite and minor bornite (associated with potassic alteration and gold mineralization); (2) vein-type molybdenite (associated with weak phyllic alteration); and (3) polymetallic sulfide–carbonate veins (dolomite ± quartz–sphalerite–galena–arsenopyrite–chalcopyrite, associated with weak sericite–carbonate alteration). Re–Os

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34

KVASNYTSYA, V. M. "The Size and Shape of Diamond Crystals of Different Origin." Mineralogical Journal 44, no. 1 (2022): 32–40. http://dx.doi.org/10.15407/mineraljournal.44.01.032.

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The size and shape of diamond crystals of different origin are analyzed. Diamonds with a size of less than about 0.5 mm are classified as microcrystals. Diamonds found in meteorites typically show non-faceted anhedral crystals of various sizes. Only the Canyon Diablo iron meteorite has cubic microcrystals of unclear crystallogenesis. Nano, micro- and macro-sized crystals of diamond in meteorites are usually aggregate in nature. The release of diamond polyhedra in meteorites is limited by the too small size of its crystals in chondrites and by its solid-phase transformation from very fine-grain

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35

Hewton, M. L., D. D. Marshall, L. Ootes, L. E. Loughrey, and R. A. Creaser. "Colombian-style emerald mineralization in the northern Canadian Cordillera: integration into a regional Paleozoic fluid flow regime." Canadian Journal of Earth Sciences 50, no. 8 (2013): 857–71. http://dx.doi.org/10.1139/cjes-2012-0128.

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Emerald in the Mackenzie Mountains is hosted in extensional quartz–carbonate veins cutting organic-poor Neoproterozoic sandstones and siltstones within the hanging wall of a thrust fault that emplaced these strata above Paleozoic rocks. Isotopic compositions of water extracted from emerald are typical of evolved sedimentary sulphate brines. Fluid inclusion studies indicate two saline fluid populations: a CO2–N2-bearing, high-salinity brine (20.4–25.8 wt.% NaCl equivalent), and a gas-free, saline brine (7.6–15.3 wt.% NaCl equivalent). Both populations display evidence of post-entrapment volume

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36

Drake, Henrik, Nick M. W. Roberts, and Martin J. Whitehouse. "Geochronology and Stable Isotope Analysis of Fracture-Fill and Karst Mineralization Reveal Sub-Surface Paleo-Fluid Flow and Microbial Activity of the COSC-1 Borehole, Scandinavian Caledonides." Geosciences 10, no. 2 (2020): 56. http://dx.doi.org/10.3390/geosciences10020056.

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The deep biosphere hosted in fractured rocks within the upper continental crust is one of the least understood and studied ecological realms on Earth. Scarce knowledge of ancient life and paleo-fluid flow within this realm is owing to the lack of deep drilling into the crust. Here we apply microscale high spatial-resolution analytical techniques to fine-grained secondary minerals in a deep borehole (COSC-1) drilled into the Silurian-Devonian Scandinavian Caledonide mountain range in central Sweden. The aim is to detect and date signs of ancient microbial activity and low-temperature fluid circ

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37

Gafsi, Saddam, Farhan Bin Tarik, Cody T. Nelson, and Judson D. Ryckman. "Optically resonant all-dielectric diabolo nanodisks." Applied Physics Letters 120, no. 26 (2022): 261702. http://dx.doi.org/10.1063/5.0089007.

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Optically resonant all-dielectric nanostructures attractively exhibit reduced losses compared to their plasmonic counterparts; however, achieving strong field enhancements at the nanoscale, especially within solid-state media, has remained a significant challenge. In this work, we demonstrate how subwavelength modifications to a conventional silicon nanodisk enable strong sub-diffractive and polarization dependent field enhancements in devices supporting Mie resonances, including anapole-like modes. We examine the electromagnetic properties of both individual and arrayed “diabolo nanodisks,” w

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38

Carpenter, Chris. "2D Restorations and Basin Modeling Provide Insight Into Formation Maturation." Journal of Petroleum Technology 75, no. 02 (2023): 84–86. http://dx.doi.org/10.2118/0223-0084-jpt.

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_ This article, written by JPT Technology Editor Chris Carpenter, contains highlights of paper URTeC 2021-5434, “Delaware Basin Wolfcamp Formation Maturation and Post-Permian Basin Evolution Based on 2D Restorations and Basin Modeling,” by Rachel Hoar, Mauro Becker, and Alan Yu, Texas A&M University. The paper has not been peer reviewed. _ The Permian Delaware Basin is a complex system in which the maturation of organic matter is affected by events not evident in the post-Permian available data. In this study, the authors aim to identify the effect of various geologic controls on hydrocarb

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Alsayed, Yazan, Michael Timm, Alexey Leontovich, et al. "Proteomic Analysis of Waldenstrom Macroglobulinemia (WM) Using Nanoscale Protein Micorarray Techniques." Blood 106, no. 11 (2005): 504. http://dx.doi.org/10.1182/blood.v106.11.504.504.

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Abstract The objective of this study was to determine the molecular alterations that occur at the protein level in patients with WM in order to identify novel targets of therapy, determine new markers of prognosis, and begin to delineate the pathogenesis of WM. Five bone marrow samples were obtained after informed consent from patients with symptomatic WM. Two bone marrow samples were obtained from age-matched controls and were pooled. All samples were purified with anti-CD19+ beads with over 90% purity. Protein quantification was performed and 1ug of protein was obtained for each sample and c

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40

Deckert, Mikołaj, and Anna Cichosz. "A reception perspective on client-agent interactions in the DiaBiz corpus of spoken Polish." Ibérica, no. 48 (December 19, 2024): 43–69. https://doi.org/10.17398/2340-2784.48.43.

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This paper introduces the DiaBiz corpus (Pęzik et al., 2022) – a spoken corpus of call-centre dialogues in Polish – and discusses the findings of a reception experiment (N=100) exploring some of the characteristics of the language data in the corpus. Given that the conversations were recorded specifically for the corpus rather than being authentic exchanges extracted from real-life business contexts, we first offer evidence on how the DiaBiz dialogues are experienced and evaluated by language users along a range of reception parameters: cognitive load, absorption, comprehension as well as natu

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41

Jennings, J. W., and W. B. Ward. "Geostatistical Analysis of Permeability Data and Modeling of Fluid-Flow Effects in Carbonate Outcrops." SPE Reservoir Evaluation & Engineering 3, no. 04 (2000): 292–303. http://dx.doi.org/10.2118/65370-pa.

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Summary Permeability data from Permian dolomitized shallow-water platform carbonate outcrops in west Texas and New Mexico exhibit two to five orders of magnitude variability, most of which occurs within distances of a few feet [1 to 2 m] within single rock-fabric units. A variety of longer-range features are also observed, including vertical interbed average-permeability contrasts, 140- to 180-ft [42- to 54-m] lateral periodicities, and up to 2,700-ft [810-m] lateral trends. The short-range heterogeneities can be modeled with K-Bessel semivariograms having asymptotic power-law behavior at the

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42

Kilminster, Kieryn, and Ian Cartwright. "A sulfur-stable-isotope-based screening tool for assessing impact of acid sulfate soils on waterways." Marine and Freshwater Research 62, no. 2 (2011): 152. http://dx.doi.org/10.1071/mf10190.

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Early warning indicators for waterways affected by acid sulfate soils (ASS) are valuable tools for water management organisations. Oxidised ASS may discharge high concentrations of metals, acid and sulfur to surrounding water. The origin of sulfate may be determined by δ34S values. δ34S values of dissolved sulfate in ~300 samples of fresh, brackish and estuarine surface water from south-west Western Australia ranged from –6.6 to 31.4‰ (Cañon Diablo Troilite). An indicator was developed based on [SO42–], [Cl–] and δ34S that categorised samples into groups with similar isotopic influences (iso-g

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Liu, X., P. Coulibaly, and N. Evora. "Comparison of data-driven methods for downscaling ensemble weather forecasts." Hydrology and Earth System Sciences Discussions 4, no. 1 (2007): 189–210. http://dx.doi.org/10.5194/hessd-4-189-2007.

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Abstract. This study investigates dynamically different data-driven methods, specifically a statistical downscaling model (SDSM), a time lagged feedforward neural network (TLFN), and an evolutionary polynomial regression (EPR) technique for downscaling numerical weather ensemble forecasts generated by a medium range forecast (MRF) model. Given the coarse resolution (about 200-km grid spacing) of the MRF model, an optimal use of the weather forecasts at the local or watershed scale, requires appropriate downscaling techniques. The selected methods are applied for downscaling ensemble daily prec

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Coulibaly, P., and N. Evora. "Comparison of data-driven methods for downscaling ensemble weather forecasts." Hydrology and Earth System Sciences 12, no. 2 (2008): 615–24. http://dx.doi.org/10.5194/hess-12-615-2008.

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Abstract. This study investigates dynamically different data-driven methods, specifically a statistical downscaling model (SDSM), a time lagged feedforward neural network (TLFN), and an evolutionary polynomial regression (EPR) technique for downscaling numerical weather ensemble forecasts generated by a medium range forecast (MRF) model. Given the coarse resolution (about 200-km grid spacing) of the MRF model, an optimal use of the weather forecasts at the local or watershed scale, requires appropriate downscaling techniques. The selected methods are applied for downscaling ensemble daily prec

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Rosa Lara, Rogéria Inês, Nelson Wanderley Perioto, and Caleb Califre Martins. "Osmylidae (Insecta: Neuroptera) from Atlantic rainforest in southeastern Brazil and new records for Gumilla adspersus Navás, 1912." REVISTA CHILENA DE ENTOMOLOGÍA 50, no. 1 (2024): 41–50. http://dx.doi.org/10.35249/rche.50.1.24.06.

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Between October 2009 and December 2011, five Malaise traps/area were used to survey of the lance lacewings (Neuroptera: Osmylidae) in five areas of the Atlantic rainforest in São Paulo state, Brazil. Were obtained 73 specimens of Isostenosmylus pulverulentus (Gerstaecker, 1894) (96.1% of the total collected), two of Gumilla adspersus Navás, 1912 (2.6%), and one of Isostenosmylus sp. (1.3%). The osmylids were more frequently observed in the Parque Estadual da Serra do Mar / Núcleo Santa Virgínia (59.2% of the total collected), Parque Estadual Intervales (30.3%) and Parque Estadual Morro do Diab

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Stowers, J. M., H. W. Sutherland, and D. F. Kerridge. "Long-Range Implications for the Mother: The Aberdeen Experience." Diabetes 34, Supplement_2 (1985): 106–10. http://dx.doi.org/10.2337/diab.34.2.s106.

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Pérez, Mijail, and Marlon Sotelo. "Species richness of continental gastropod mollusks from a coffee plantation in Jinotega, northern Nicaragua: a first approach." UNED Research Journal 5, no. 1 (2013): 17–23. http://dx.doi.org/10.22458/urj.v5i1.215.

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Continental mollusks of some parts of Nicaragua, such as the Pacific region and the central-north of the country have been relatively well studied, including recently contributions on community ecology for these areas. This paper presents the results of a study on the structure of communities in a coffee farm in the northern zone of the country and at a protected area adjacent to it. The results show a total inventory of 21 species, more or less common values in communities of this group. Species richness at the coffee farm considering all stations (18 species) is higher than species richness

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Montfort, Nick. "Rap beyond the Afterfuture." Global Hip Hop Studies 6, no. 1 (2025): 113–21. https://doi.org/10.1386/ghhs_00107_7.

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A comparison of two visions of the future from the year 2000: Deltron 3030 by the trio of the same name and Welcome to the Afterfuture by Mike Ladd. Many aspects of these albums are considered, including production and even the cover art, although the focus is on the lyrics. Del the Funky Homosapien draws on The Matrix, Ghost in the Shell and Akira and is broadly concerned with the plight of humanity and the downtrodden, while Ladd riffs on Star Trek, Star Wars and Blade Runner and foregrounds racial concerns. The sound and range of references on Afterfuture take the idea of a syncretic future

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Jensen, I., V. Kruse, and U. D. Larsen. "Scintigraphic Studies in Rats: Kinetics of Insulin Analogues Covering Wide Range of Receptor Affinities." Diabetes 40, no. 5 (1991): 628–32. http://dx.doi.org/10.2337/diab.40.5.628.

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Miranda, Marcel Sabino, Flávio Dias Passos, and Alan Rodrigo Batistão. "New occurrences of Mirinaba unidentata (G.B. Sowerby II, 1825) from southeastern Brazil, with comments on the distribution of M. planidens (Michelin, 1831) (Gastropoda: Eupulmonata: Strophocheilidae)." Journal of Conchology 45, no. 2 (2024): 195–200. http://dx.doi.org/10.61733/jconch/4518.

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Here, we report new occurrences of Mirinaba unidentata (G.B. Sowerby II, 1825) and review of the occurrence records M. unidentata and M. planidens (Michelin, 1831). A single shell of M. unidentata was collected in the Parque Estadual Caverna do Diabo, southern São Paulo state, Brazil. Moreover, material of both species deposited at the Museum of Zoology of University of São Paulo were observed. These two seem to have allopatric distributions, and not overlapping. Mirinaba planidens occurs in the mountain ranges shared by São Paulo, Rio de Janeiro, and Minas Gerais in southeastern Brazil, where

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