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Abstract. The Mid-Brunhes Transition (MBT) saw an increase in the amplitude of glacial cycles expressed in ice core and deep ocean records from about 400 ka, but its influence on high-latitude climates is not fully understood. The Arctic Ocean is thought to have warmed and exhibited reduced sea ice, but little is known of sea ice marginal locations such as the Bering Sea. The Bering Sea is the link between the Arctic and Pacific Ocean and is an area of high productivity and CO2 ventilation; it hosts a pronounced oxygen minimum zone (OMZ) and is thought to be the location of Glacial North Pacific Intermediate Water (GNPIW) formation in the Pleistocene. To understand palaeoceanographic change in the region, we analysed benthic foraminiferal faunas from Bowers Ridge (Site U1342, 800 m of water depth) over the past 600 kyr, as they are uniquely well preserved and sensitive to changes in deep and surface ocean conditions. We identified and imaged 71 taxa and provide a full taxonomy. Foraminiferal preservation is markedly higher during glacials, indicating the presence of less corrosive GNPIW. The most abundant species are Bulimina exilis, Takayanagia delicata, Alabaminella weddellensis, Gyroidina sp. 2, Cassidulina laevigata, Islandiella norcrossi, and Uvigerina bifurcata, consistent with broadly high net primary production throughout the last 600 kyr. Correspondence analysis shows that the most significant Assemblage 1 comprises B. exilis, T. delicata, Bolivina spissa, and Brizalina, which occur sporadically within intervals of laminated, biogenic-rich sediment, mostly during glacials and also some deglacials, and are interpreted as indicating very high productivity. Other assemblages contain the phytodetritivore species A. weddellensis, I. norcrossi, and C. laevigata, indicative of seasonal phytoplankton blooms. Before the MBT, more numerous intervals of the very high-productivity Assemblage 1 and A. weddellensis occur, which we suggest reflect a time of more sea-ice-related seasonal stratification and ice edge blooms. Our inference of a decrease in sea ice meltwater stratification influence in the central Bering Sea after the MBT is consistent with records showing that the Arctic and Pacific Ocean warmed during glacials and suggests that high-latitude productivity and sea ice changes were an important feature of this climate event.

Water samples from River Owan located within the Benin-Owena River Basin, southwestern Nigeria, were investigated for irrigation suitability employing electrical conductivity (EC), Sodium Absorption Ratio (SAR), %Na, Residual Sodium Bicarbonate (RSBC), Potential Salinity (PS), Soluble Sodium Product (SSP), Magnesium absorption ratio (MAR), Kelly ratio (KR) and Wilcox plot. Estimated irrigation parameters revealed that SAR ranged from 0. RSBC; MAR; KR; while PS, SSP and %Na were from 0. 01 -3.12 (av. 0.56), 31.51 -70.33 (av. 55.99) and 19.93 -58.69 (av55.99) respectively. Furthermore, Wilcox plot revealed that all water samples from River Owan were in the excellent to good irrigation category. All estimated indices except MAR and KR indicated that River Owan water was suitable for irrigation. Wells at Owan were shallow and pruned to dryness during dry season. River Owan water that was moderately suitable for irrigation could serve as a buffer to farming activities especially during dry season.