Additional file 1: of A record of the upper Olduvai geomagnetic polarity transition from a sediment core in southern Yokohama City, Pacific side of central Japan

Table A1. Results from Core M. Natural remanent magnetizations (NRM), characteristic remanent magnetization (ChRM) declinations and inclinations, maximum angular dispersions (MAD), relative paleointensities (NRM20–40 mT/ARM20–40 mT), volume magnetic susceptibilities (κ), and anhysteretic remanent magnetization susceptibilities (κARM). (XLSX 61 kb)