A high-resolution Late Glacial to Holocene record of environmental change in the Mediterranean from Lake Ohrid (Macedonia/Albania)

Lacey, J. H., Francke, A., Leng, M. J., Vane, C. H. and Wagner, B.: A high-resolution Late Glacial to Holocene record of environmental change in the Mediterranean from Lake Ohrid (Macedonia/Albania), International Journal of Earth Sciences, 104(6), 1623–1638, doi:10.1007/s00531-014-1033-6, 2014.

d18O (LS15LAOH01a): interpretation3_scope: '' has been replaced by 'isotope'
d18O (LS15LAOH01a): interpretation4_scope: '' has been replaced by 'isotope'

Thermo Finnigan DeltaPlus IRMS linked to a Thermo Finnigan Gasbench II

Samples only used if TIC/TOC > 0.3; samples with very enriched d13C values assumed to have formed diagenetically; SEM-screened to exclude a detrital origin of carbonates

Carbonate record consists of ikaite-derived calcite; Negative correlation between amount of precipitation and west wind intensity (Mayr et al., 2007; Garreaud et al., 2013)

Hydrologically closed lake (Talbot 1990; Leng & Marshall 2004)

Oehlerich, M. , Mayr, C. , Gussone, N. , Hahn, A. , Holzl, S. , Lucke, A. , Ohlendorf, C. , Rummel, S. , Teichert, B.M.A. , Zolitschka, B.

Lateglacial and Holocene climatic changes in south-eastern Patagonia inferred from carbonate isotope records of Laguna Potrok Aike (Argentina)

Oehlerich, M., Mayr, C., Gussone, N., Hahn, A., Hoelzl, S., Luecke, A., Ohlendorf, C., Rummel, S., Teichert, B. M. A. and Zolitschka, B.: Lateglacial and Holocene climatic changes in south-eastern Patagonia inferred from carbonate isotope records of Laguna Potrok Aike (Argentina), Quaternary Science Reviews, 114, 189–202, doi:10.1016/j.quascirev.2015.02.006, 2015.

d18O (LS15OEPO01a): interpretation4_scope: '' has been replaced by 'isotope'

GC coupled to Delta V IRMS via pyrolysis interface operated at 1430 degrees C

Located in southern Ghana, the climate of Lake Bosumtwi is heavily influenced by the West African monsoon, which draws moisture onshore from the Gulf of Guineaduring the months of April-October as the monsoon trough migrates northward with the sun (Fig. S2). In winter the winds reverse, and the climate of southern Ghana is influenced by hot, dry northeasterly monsoon winds, which inhibit precipitation over much of North Africa.