Magnetic mineral study of Holocene marine sediments from the Alfonso Basin, Gulf of California - implications for depositional environment and sediment sources
Results of a rock magnetic study of marine sediments from the Alfonso Basin, Bay of La Paz are used to investigate sediment sources and depositional environment in the southern Gulf of California during SPROUTED PROTEIN CHOC the Holocene.Radiocarbon dating provides stratigraphic control, with age for the core bottom sediments of 7597-7831 cal.yr B.