Evidence from the Pacific troposphere for large global sources of oxygenated organic compounds

Oxygen isotope evidence for the formatio

Oxygen isotope evidence for the formation of andesitic–dacitic magmas from the fast-spreading Pacific–Antarctic Rise by assimilation–fractional crystallisation

✍ Freund, Sarah; Beier, Christoph; Krumm, Stefan; Haase, Karsten M. 📂 Article 📅 2013 🏛 Elsevier Science 🌐 English ⚖ 999 KB

Biogenic volatile organic compounds as p

Biogenic volatile organic compounds as potential carbon sources for microbial communities in soil from the rhizosphere of Populus tremula

✍ Susan M. Owen; Stuart Clark; Matevz Pompe; Kirk T. Semple 📂 Article 📅 2007 🏛 John Wiley and Sons 🌐 English ⚖ 101 KB

SPME-GC-MS analysis of volatile organic

SPME-GC-MS analysis of volatile organic compounds in honey from Basilicata. Evidence for the presence of pollutants from anthropogenic activities

✍ Giovanni Bentivenga; Maurizio D'Auria; Pietro Fedeli; Giacomo Mauriello; Rocco R 📂 Article 📅 2004 🏛 John Wiley and Sons 🌐 English ⚖ 104 KB

Structure of Horseradish Perosidase Comp

Structure of Horseradish Perosidase Compound I : Kinetic Evidence for the Incorporation of One Oxygen Atom from the Oxidizing Substrate into the Enzyme

✍ Suara A. ADEDIRAN; H. Brian DUNFORD 📂 Article 📅 1983 🏛 John Wiley and Sons 🌐 English ⚖ 363 KB

The global network of plate boundaries c

The global network of plate boundaries can be divided into two discrete subnetworks containing the spreading and subduction boundaries, respectively. We advocate that this division is a stable pattern that derives from consistency rules in rigid-plate rotations. Subduction is distributed along a single, long subnetwork, hence organizing the mantle convection as a single, long downwelling wall and two lower mantle upwelling columns, at the Pacific and African sides of the Earth, respectively. The columns should merge upward between Antarctica and Australia to reach the single, long spreading subnetwork. The flow encircles two toric volumes that escape convectional mixing and are the likely sources of the two, Atlantic–Indian and Pacific, hot spot domains.

✍ L.-E. Ricou 📂 Article 📅 1998 🏛 John Wiley and Sons 🌐 English ⚖ 197 KB

The global network of plate boundaries can be divided into two discrete subnetworks containing the spreading and subduction boundaries, respectively. We advocate that this division is a stable pattern that derives from consistency rules in rigid‐plate rotations. Subduction is distributed along a sin