Shackleton

Fernandez ML, Higgins JS, Penfold J, Shackleton CS (1990) Polymer Commun 31 124... 

Fig. 18-1 Benthic foraminiferal oxygen isotope record from 3477 m water depth in the eastern tropical Pacific ocean from Ocean Drilling Program site 677 (Shackleton et al, 1990). ratios are expressed in the S...

Antarctica the West Antarctic ice sheet expanded significantly during the LGM (Denton et ai, 1989), while the East Antarctic ice sheet expanded modestly. Concurrent with the growth of major ice sheets was a drop in sea level, with a maximum sea level depression during the LGM of approximately 120 m (Shackleton, 1987). 

Fig. 18-22 The last 50 000 years of environmental history, recorded in central Greenland (GISP2 and GRIP ice cores), plus the CO2 record from Vostok, Antarctica, and global ice volume measured as sea level depression. (From top to bottom, references are Shackleton, 1987 Cuffey et ai, 1995 and Grootes et al, 1993 Cuffey and Clow, 1997 Chapellaz et al, 1990 Brook et al., 1996 Mayewski et al., 1997 Saltzman et al., 1997.)...

Shackleton, N. J. (1967). Oxygen isotope analyses and Pleistocene temperatures re-assessed. Nature 215, 15-17. 

Shackleton, N. J., Berger, A., and Peltier, W. R. (1990). An alternative astronomical calibration of the lower Pleistocene timescale based on ODP Site 677. Trans R. Soc. Edin. Earth Sci. 81,251-261. 

Shackleton, N.J. 1995 New data on the evolution of Pliocene climatic variability. /nVrba, E.S., Denton, G.H., Partridge, T.C. and Burckle, L.H., eds., Paleoclimate and Evolution. New Haven, CT, Yale University Press 242-248. 

The concept of COI was first developed by Rice (Rice 1966, 1967 Rice and Cooper 1967 Rice et al. 1985). It assumes that resources could be used for another purpose if a disease did not exist. Figure 1 demonstrates the basic concept of COI. Most health economic studies assessing the total costs of a disease use this methodology (e.g., Keith and Shackleton 2006 Welte et al. 2000 Leidl et al. 1999 Henke et al. 1997 Xie et al. 1996 Harwood et al. 1983 Hodgson and Meiners 1979). 

Whitesides TH, Shelly J (1975) Thermolysis and photolysis of (cyclopentadiene)iron tricarbonyl. Evidence for a radical mechanism involving iron(I). J Organomet Chem 92 215-226 Shackleton TA, Mackie SC, Fergusson SB, Johnston LJ, Baird MC (1990) The chemistry of (r -C5H5)Fe(CO)2H revisited. Organometallics 9 2248-2253... 

Legin AV, Vlasov YG, Rudnitskaya AM, Bychkov EA (1996) Cross-sensitivity of chalcogenide glass sensors in solutions of heavy metal ions. Sens Actuators B 34 456 61 De Marco R, Shackleton J (1999) Cahbration of the Hg chalcogenide glass membrane ion-selective electrode in seawater media. Talanta 49 385-391... 

Fig. 4.1. Isotopic paleotemperature analyses of planktonic and benthic foraminifera from the sub-Antarctic Pacific indicating considerably warmer conditions in the Early Cenozoic (Shackleton and Kennett, 1975a).

Shackleton, N.J. (1986) Paleogene stable isotope events. Paleogeogr. Paleoclimatol. PaleoecoL, 57, 91-102. 

Shackleton, N.J. and Kennett, J.P. (1975a) Paleotemperature history of the Cenozoic and the initiation of Antarctic glaciation oxygen and carbon isotope analyses in DSDP Sites 277, 279, and 281. Initial Reports of the DSDP, 29, Washington, D.C. U.S. Gov. Printing Office, pp. 743-755. 

Shackleton NJ, Imbrie J, Hall MA (1983) Oxygen and carbon isotope record of East Pacific core V19-30 implications for the formation of deep water in the late Pleistocene Nodh Atlantic. Earth Planet Sci... 

Martinson DG, Pisias NG, Hays JD, Imbrie J, Moore TC, Shackleton NJ (1987) Age dating and the orbital theory of the Ice Ages Development of a high-resolution 0 to 300,000 yr chronostratigraphy. Qrrat Res 27 1-29... 

Duplessy JC, Shackleton NJ, Fairbanks RG, Labeyrie L, Oppo D, Kallel N (1988) Deepwater source variations during the last climatic cycle and their impact on the global deepwater circulation. Paleoceanography 3(3) 343-360... 

Imbrie J, Hays JD, Martinson DG, McIntyre A, Mix AC, Morley JJ, Pisias NG, Prell W L, Shackleton NJ (1984) The orbital theory of Pleistocene climate Support from a revised chronology of the marine record. In Milankovitch and Climate, Vol. 1. Berger A, Imbrie J, Hays J, Kukla G, Saltzman B (eds) D. Reidel, Boston p 269-305... 

Emiliani, C. and N. J. Shackleton (1974), The Brunhes epoch Isotopic paleotempera-tures and geochronology, Science 183, 511-514. 

Shackleton, N. J. (1970), Stable isotope study of the palaeoenvironment of the neolithic site of Nea Nikomedeia, Greece, Nature 227, 943-944. 

Shackleton, N. J. and N. D. Opdyke (1973), Oxygen isotope and palaeomagnetic stratigraphy of equatorial Pacific core V28-238, Quatem. Research 3, 39-55. 

Warton B, Mattiessen J N and Shackleton M A (2001), Glucosinolate content and isothiocyanate evolution-two measures of the biofumigation potential of plants , J Agric Food Chem, 49, 5244—5250. 

Much credit goes to the team of professionals at CRC Press/Taylor Francis Group who worked on this second edition. Especially important were Dr. Fiona Macdonald, Publisher, Chemistry Dr. Janice Shackleton, Input Supervisor Patrica Roberson, Project Coordinator Elise Oranges and Jay Margolis, Project Editors and Marcela Peres, Production Assistant. 

Shackleton Department of Anaesthetics, Southampton General Hospital, Southampton, UK... 

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