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.
How Does the Arctic Sea Ice Affect the Interannual Variability of Tropical Cyclone Activity Over the Western North Pacific?
