Outputs (48)

Red Sea Palaeoclimate: Stable Isotope and Element-Ratio Analysis of Marine Mollusc Shells (2018)
Book Chapter
Hausmann, N., Kokkinaki, O., & Leng, M. J. (2019). Red Sea Palaeoclimate: Stable Isotope and Element-Ratio Analysis of Marine Mollusc Shells. In N. M. Rasullan, & C. F. Stewart (Eds.), Geological Setting, Palaeoenvironment and Archaeology of the Red Sea (725-740). Springer. https://doi.org/10.1007/978-3-319-99408-6_33

The southern Red Sea coast is the location of more than 4,200 archaeological shell midden sites. These shell middens preserve archaeological and climatic archives of unprecedented resolution and scale. By using shells from these contexts, it is possi... Read More about Red Sea Palaeoclimate: Stable Isotope and Element-Ratio Analysis of Marine Mollusc Shells.

Middle-late quaternary palaeoclimate variability from lake and wetland deposits in the Nefud Desert, Northern Arabia (2018)
Journal Article
Parton, A., Clark-Balzan, L., Parker, A. G., Preston, G. W., Sung, W. W., Breeze, P. S., …Petraglia, M. D. (2018). Middle-late quaternary palaeoclimate variability from lake and wetland deposits in the Nefud Desert, Northern Arabia. Quaternary Science Reviews, https://doi.org/10.1016/j.quascirev.2018.10.010

Records of former lake and wetland development in present day arid/hyper-arid environments provide an important source of information for palaeoclimatic and palaeoenvironmental studies. In Arabia, such records are typically confined to eccentricity-m... Read More about Middle-late quaternary palaeoclimate variability from lake and wetland deposits in the Nefud Desert, Northern Arabia.

Effects of cleaning methods upon preservation of stable isotopes and trace elements in shells of Cyprideis torosa (Crustacea, Ostracoda): implications for palaeoenvironmental reconstruction (2018)
Journal Article
Roberts, L., Holmes, J., Leng, M. J., Sloane, H., & Horne, D. (2018). Effects of cleaning methods upon preservation of stable isotopes and trace elements in shells of Cyprideis torosa (Crustacea, Ostracoda): implications for palaeoenvironmental reconstruction. Quaternary Science Reviews, 189, https://doi.org/10.1016/j.quascirev.2018.03.030

The trace element (Sr/Ca and Mg/Ca) and stable isotope (δ¹⁸O and δ¹³C) geochemistry of fossil ostracod valves provide valuable information, particularly in lacustrine settings, on palaeo-water composition and palaeotemperature. The removal of sedimen... Read More about Effects of cleaning methods upon preservation of stable isotopes and trace elements in shells of Cyprideis torosa (Crustacea, Ostracoda): implications for palaeoenvironmental reconstruction.

Holocene-aged human footprints from the Cuatrociénegas Basin, NE Mexico (2013)
Journal Article
Felstead, N. J., Gonzalez, S., Huddart, D., Noble, S. R., Hoffmann, D. L., Metcalfe, S. E., …Jimenez-Lopez, J. C. (2014). Holocene-aged human footprints from the Cuatrociénegas Basin, NE Mexico. Journal of Archaeological Science, 42, 250-259. https://doi.org/10.1016/j.jas.2013.11.010

Two sets of well-preserved human footprints have been found in tufa sediments in the Cuatrociénegas Basin, NE Mexico, and here we present their U-series dates of 10.55±0.03ka and 7.24±0.13ka. The former are the oldest known footprints in Mexico, alth... Read More about Holocene-aged human footprints from the Cuatrociénegas Basin, NE Mexico.

Influence of the ratio of planktonic to benthic diatoms on lacustrine organic matter δ 13 C from Erlongwan maar lake, northeast China (2012)
Journal Article
Wang, L., Mackay, A. W., Leng, M. J., Rioual, P., Panizzo, V. N., Lu, H., …Kendrick, C. P. (2013). Influence of the ratio of planktonic to benthic diatoms on lacustrine organic matter δ 13 C from Erlongwan maar lake, northeast China. Organic Geochemistry, 54, 62-68. https://doi.org/10.1016/j.orggeochem.2012.09.010

Carbon isotope ratio (δ 13 C org ) values of organic matter in lake sediments are commonly used to reconstruct environmental change, but the factors which influence change are varied and complex. Here we report δ 13 C values for sediments from Erlong... Read More about Influence of the ratio of planktonic to benthic diatoms on lacustrine organic matter δ 13 C from Erlongwan maar lake, northeast China.

Evidence of past environmental conditions during the evolution of a calcretised Wadi System in Southern Jordan using stable isotopes (2012)
Journal Article
McLaren, S. J., Leng, M. J., Knowles, T., & Bradley, A. V. (2012). Evidence of past environmental conditions during the evolution of a calcretised Wadi System in Southern Jordan using stable isotopes. Palaeogeography, Palaeoclimatology, Palaeoecology, 348-349, 1-12. https://doi.org/10.1016/j.palaeo.2012.05.010

A stratigraphically and temporally ordered sequence of channel calcretes preserved along the Wadi Dana, Southern Jordan, records the Quaternary evolution of the formation and infilling of rock-cut channels and their subsequent incision in a tectonica... Read More about Evidence of past environmental conditions during the evolution of a calcretised Wadi System in Southern Jordan using stable isotopes.

A multiproxy palaeolimnological investigation of Holocene environmental change, between c. 10 700 and 7200 years BP, at Holebudalen, southern Norway (2008)
Journal Article
Panizzo, V. N., Jones, V. J., Birks, H. J., Boyle, J. F., Brooks, S. J., & Leng, M. J. (2008). A multiproxy palaeolimnological investigation of Holocene environmental change, between c. 10 700 and 7200 years BP, at Holebudalen, southern Norway. Holocene, 18(5), 805-817. https://doi.org/10.1177/0959683608089217

Geochemical analyses (x-ray fluorescence, δ13C and C/N ratios) were used to reconstruct early Holocene environments (between 10685 and 7260 cal. yr BP) at a small lake near Holebudalen, southern Norway. Results show a period of increasing stability,... Read More about A multiproxy palaeolimnological investigation of Holocene environmental change, between c. 10 700 and 7200 years BP, at Holebudalen, southern Norway.

Reconstructing hydrological variability in Lake Baikal during MIS 11: An application of oxygen isotope analysis of diatom silica (2008)
Presentation / Conference Contribution
Mackay, A. W., Karabanov, E., Leng, M. J., Sloane, H. J., Morley, D. W., Panizzo, V. N., Khursevich, G., & Williams, D. (2007, April). Reconstructing hydrological variability in Lake Baikal during MIS 11: An application of oxygen isotope analysis of diatom silica. Presented at Isotopes in Biogenic Silica (IBiS), Nottingham, UK

In this paper we reconstruct hydrological variability in Lake Baikal during Marine Isotope Stage 11 (MIS 11) (427-362 ka BP) from oxygen isotope analysis of diatom silica. Highest δ18Odiatom values are found during MIS 11.3, highlighting the dominanc... Read More about Reconstructing hydrological variability in Lake Baikal during MIS 11: An application of oxygen isotope analysis of diatom silica.