The
oxygen isotopic composition (δ18O) of diatom
frustules is potentially a quantitative paleoenvironmental proxy.
However, δ18O analysis has some uncertainties because
of difficulties in removing clay-mineral contamination and taxon-specific
separation due to the small size of diatom frustules. The clay-mineral
contamination seriously affects δ18O measurements,
and the δ18O of bulk diatoms contains a mixture of
information from diatoms living in various seasons and water depths.
To resolve such problems, we established a new method for purifying
the frustules of disc-shaped diatoms using a cell sorter and succeeded
in removing the clay-mineral contamination and restricting the number
of species for the δ18O analysis. We developed this
method using samples from a sediment core retrieved from the Conrad
Rise in the Indian Ocean sector of the Southern Ocean. First, the
disc-shaped diatoms were enriched and cleaned by sieving, elutriation,
and heavy-liquid separation. The samples were then further purified
by a cell sorter. Regardless of the diatom assemblage or the sediment
type in the core sample, this method generated samples consisting
of more than 95% disc-shaped diatoms, dominated by Thalassiosira lentiginosa (Janisch) Fryxell, which
occurs ubiquitously throughout the Southern Ocean. The δ18O profile for the sediment core obtained from purified disc-shaped
diatoms showed the last glacial cycle since ca. 40 ka, which can be
correlated with the LR04 benthic δ18O stack record
and the temperature record in the EPICA Dome C ice core, indicating
that this method can contribute to obtaining an accurate δ18O record of diatoms associated with glacial–interglacial
cycles.