Implications for reconstruction

Bogaard, A., Heaton, T. H. E., Poulton P. and Merbach, I. (2007) The impact of manuring on nitrogen isotope ratios in cereals archaeological implications for reconstruction of diet and crop management practices. Journal of Archaeological Science 34, 335 343. 

GC of midchain dimethylalkane carbon skeleton alkylthiophenes, 475,477/ GC-MS procedure, 449-450 geological setting, 446-447 hydrocarbon biomarkers, 453-457 implications for reconstruction of palaeoenvironments, 478,480 lithology, 448/",452... 

Elderfield H., Cooper M., and Ganssen G. (2000) Sr/Ca in multiple species of planktonic foraminifera implications for reconstructions of seawater Sr/Ca. Geochem. Geophys. Geosys. 1, paper no. 1999GC00031. 

Rosenthal Y., Lohmann G. P., Lohmann K. C., and SherreU R. M. (2000) Incorporation and preservation of Mg in Globigerinoides sacculifer implications for reconstructing the temperature and of seawater. Paleoceanography... 

Globigerinoides sacculifer. implications for reconstructing the temperature and of seawater. Paleoceanography... 

Lemarchand D., Gaillardet J., Lewin E., and Allegre C. J. (2000) The influence of rivers on marine boron isotopes and implications for reconstructing past ocean pH. Nature 408(6815), 951-954. 

Eggins, S., De Deckker, P. Marshall, J. 2003. Mg/Ca variation in planktonic foraminifera tests implications for reconstructing palaeo-seawater temperature and habitat migration. Earth and Planetary Science Letters, 212, 291-306. 

Bickert, T., Wefer, G, 1999. South Atlantic and benthic foraminifer 8 C-deviations Implications for reconstructing the Late Quaternary deep-water circulation. Deep-Sea Research, 46 437-452. 

Feng, X., Epstein, S., 1995. Carbon isotopes of trees from arid environments and implications for reconstructing atmospheric CO2 concentration. Geochim. Cosmochim. Acta 59, 2599—2608. 

Dolphin, A.E., Goodman, A.H. (2009) Maternal diets, nutritional status, and zinc in contemporary Mexican infants teeth implications for reconstructing paleodiets. American Journal of Physical Anthropology, 140(3), 399-409. 

Burakov, B. E., Anderson, E. B., Galkin, B. Ya., Pazukhin, E. M., Shabalev, S. I. Study of Chernobyl hot" particles and fuel containing masses Implications for reconstructing the initial phase of the accident. Radiochim. Acta 65, 199-202 (1994)... 

Abouheif, E., Zardoya, R., and Meyer, A. (1998) Limitations of metazoan 18S rRNA sequence data implications for reconstructing a phylogeny of the animal kingdom and inferring the reality of the Cambrian explosion. Journal of Molecular Evolution, 47, 394—405. 

Abonyi, S. 1993 The Effects of Processing on Stable Isotope Levels and Mineral Concentration in Foods Implications for Paleodietary Reconstruction. Master s Thesis, Department of Archaeology, University of Calgary. 

Wang, Y. and Cerling, T.E. 1994 A model for fossil tooth and bone diagenesis implications for paleodiet reconstruction from stable isotopes. Palaeogeography, Palaeoclimatology, Palaeoecology 107 596-606. 

Jim, S., Ambrose, S. H. and Evershed, R. P. (2004) Stable carbon isotopic evidence for differences in the dietary origin of bone cholesterol, collagen and apatite implications for their use in palaeodietary reconstruction. Geochimica et Cosmochimica Acta 68, 61 72. 

J. M. Herbert and J. E. Harriman, Contraction relations for Grassman products of reduced density matrices and implications for density matrix reconstruction. Phys. Rev. A 65, 022511 (2002). 

Lean, J., J. Beer, and R. Bradley, Reconstruction of Solar Irradi-ance Since 1610 Implications for Climate Change, Geophys. Res. Lett, 22, 3195-3198 (1995a). 

Hancock, J.M. and Vogler, A.P. (2000) How slippage-derived sequences are incorporated into rRNA variable-region secondary structure implications for phylogeny reconstruction. Molecular Phylogenetics and Evolution 14, 366-374. 

Harkness RE, Berkas WR, Norbeck SW, Robinson SM (2000) Water Resources Data, North Dakota, Water Year 1999, Vol. 1 Surface Water. USGS Water Resources of North Dakota ND-99-1 Harrison TM, Copeland P, Kidd WSF, Yin A (1992) Raising Tibet. Science 255 1663-1670 Holmes JA, Chivas AR (2002) Ostracod shell chemistry - Overview. In The Ostracoda Applications in Quaternary Research. Holmes JA, Chivas AR (ed) AGU Geophysical Monograph 131 185-204 Hoppe KA (2006) Correlation between the oxygen isotope ratio of North American bison teeth and local waters Implications for paleoclimatic reconstructions. Earth Planet Sci Lett 244 408-417... 

Hoenger, A., Sack, S., Thormahlen, M., Marx, A., Muller, J., Gross, H., and Mandelkow, E. (1998). Image reconstructions of microtubules decorated with monomeric and dimeric kinesins Comparison with x-ray structure and implications for motility. /. CeU Biol. 141,419-430. 

The extensive surface reconstruction in the presence of N has implications for our discussion of the recombination process, since we must consider whether N2 forms from recombination on the unreconstructed Cu(l 1 1) surface or is formed by decomposition of copper nitride islands. In the latter case N recombination may either leave the local Cu atoms in a metastable (100) arrangement or else recombination might be associated with substantial motion of the Cu atoms as they relax from the nitride adsorption geometry. If N recombination occurs at nitride islands then the dynamics of recombinative desorption will sample a phase space which is completely different to that for dissociation on clean flat Cu terraces, making it impossible to relate these two processes by detailed balance. This is the behaviour of H recombination on Si where the large change in the Si equilibrium geometry induced by H adsorption ensures that the adsorption and desorption processes sample very different channels [13]. 

The oxides containing cations in octahedral coordination, such as MgO and TiOz, seem to suffer little or no reconstruction of the crystal structure at the surface, but there are major changes in electronic structure. These effects have important implications for surface reactivity, especially when oxygen vacancy defects are considered and particularly in transition-metal oxides. The example of TiOj was discussed above more complex behavior is shown by species such as TijOj and NiO (Henrich, 1987). The latter, like other transition metals, shows increasing [Pg.415]

Eased on two main lines of evidence, Niu et al. (1997) concluded that abyssal peridotites are the end products of melt extraction followed by variable amounts of olivine crystallization. First, in their set of reconstructed compositions they found that model fractional and batch melt extraction trends could not reproduce major and minor element variations in their data set. Most importantly, they found that melt extraction models failed to account for the strong positive correlation between FeO and MgO, as well as incompatible minor-element concentrations. Specifically, at a given Na20 or Ti02 content, abyssal peridotites are enriched in MgO relative to model melt extraction residues. Niu et al. (1997) showed that these compositional anomalies can be reconciled by a model of melt extraction followed by olivine crystallization, with more MgO-enriched samples having more accumulated olivine. If correct, this model has important implications for understanding melt extraction at oceanic ridges, and it has recently been the focus of re-evaluation. 

Dungan M. A., Wulff A., and Thompson R. (2001) Eruptive stratigraphy of the Tatara-San Pedro complex, 36°S, southern volcanic zone, Chilean Andes reconstruction method and implications for magma evolution at long-lived arc volcanic centers. J. Petrol, 555-626. 

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