A high-resolution Holocene ostracod record from the Sahel zone of Northeastern Nigeria

The ostracod record from Kajemarum Oasis in the Sahel zone of Northeastern Nigeria covers the last c. 4 000 cal, years of a 5 500 cal. year lake-sedim ent sequence. The first appearance of ostracods, around 4 000 cal. yr BP, r eflects the switch from a very dilute lake during the mid-Holocene, to slig htly oligosaline conditions that favoured the occurrence and preservation o f ostracods. Between 3 800 and 3 100 cal. yr BP, the lake remained permanen t and fresh or slightly oligosaline, with a Ca-Mg-HCO3 composition. A rise in salinity c. 3 100 cal. yr BP, accompanied by a change to more variable c onditions on a seasonal to interannual timescale, led to the influx of more -euryhaline taxa. Oligosaline conditions continued between 3 100 and 1 500 cal. yr BP Around 1 500 cal. yr BP, there was a sharp rise in salinity, pro bably accompanied by a shift to Na-CO3-type water, with marked seasonal and interannual variability. Salinity decreased after 900 cal. yr BP, although short-term variations were marked between 900 cal. yr BP and the top of th e sequence, 95 cal. yr BP. Changes in the species assemblages and ostracod abundance were a response to climate-driven variations in the seasonal and interannual stability of the lake, together with changes in its salinity an d solute composition, but there is no simple relationship between ostracod faunas and salinity. Within Kajemarum, there is no evidence of ostracod ass emblages typical of deep, fresh water, nor of hypersaline Na-Cl waters. The sediments associated with the freshest waters at Kajemarum did not favour ostracod preservation, and the driest climatic conditions were associated w ith oligosaline to mesosaline water of Na-CO3-type. The species-poor assemb lages reflect the short-term instability of the lake, coupled with the limi ted opportunities for the colonisation of this isolated basin.