10.1594/PANGAEA.968796Montade, VincentVincentMontade0000-0002-8518-2610Behling, HermannHermannBehling0000-0002-5843-8342Bremond, LaurentLaurentBremondRouland, SylvieSylvieRoulandDaut, GerhardGerhardDaut0000-0001-7414-1103Kasper, ThomasThomasKasper0000-0002-9675-1241Favier, CharlyCharlyFavier0000-0002-1126-6950PANGAEA2024isotopeLake sedimentmacroscopic charcoalMadagascarMagnetic susceptibilitySediment coreδ13C analysisDEPTH, sediment/rockAGEδ13CCoresee description in data abstractDataset10.1098/rsos.23093024 data pointstext/tab-separated-valuesCreative Commons Attribution 4.0 InternationalThe datasets provided here correspond to sedimentary charcoal counts, magnetic susceptibility measurements, and δ13C isotopic measurements obtained from a lacustrine sediment core recovered from Lake Maharasika in Montagne d'Ambre (northern Madagascar, 1,073 m asl). Fieldwork has been carried out in August 2018. The sediment core LMAHA-18 was taken from the central and deepest part of the lake (7 m water depth; 12.53509S, 49.17701E). Core LMAHA-18 was sampled with a Livingstone piston sediment corer operated from a small platform settled on two rubber boats. Using sampling tubes of ca. 5 cm diameter and 120 cm length, a total of 6 sections of about 100 cm sediment length were sampled with overlaps of 10-50 cm length. Preserved in aluminium tubes for transport to the laboratory, sediment was extruded from each aluminium tube and split into two sister cores, LMAHA-18a and LMAHA-18b. Each sister core was stored under cool (4°C) and dark conditions at the laboratory facilities (LMAHA-18a at the Friedrich-Schiller-University Jena and LMAHA-18b at the University of Goettingen, Germany).
Bulk organic δ13C was measured against certified standards (L-Prolin, EDTA and USG65) and reported in standard δ notation (‰) against Vienna Pee Dee Belemnite (VPDB) and Air, respectively. Relative errors based on triplicate measurements are 0.05 ‰ for δ13C.49.17701-12.53509MadagascarDeutsche Forschungsgemeinschaft, Bonnhttps://doi.org/10.13039/501100001659BE 2116/30Demographic fluctuations in dynamic landscapes: the integration of molecular and paleoecological evidence in a primate model opens a validated window into the past