All samples were freeze
dried, weighed, shaken 2 hr in a 4% Calgon solution, and then washed with
deionized water through a 64-µm sieve; the coarse fraction was also dried at 50°C
and weighed. Average weight percentages of the >64-µm fraction were
generally low, averaging 6 wt% at Site 1014 and 1.5 wt% at Site 1020. Benthic
foraminifers were picked for isotopic analysis from the >150-µm fraction. At
Site 1014, specimens of Cibicidoides
wuellerstorfi were very rare, so other Cibicidoides
species were picked, including C.
pachyderma and C.
mckannai as well as Planulina
ariminensis. Separate species of benthic foraminifers were analyzed
at Site 1014 at 18 different levels to estimate possible interspecific 18O
and
13C
offsets. Interspecific
18O
differences were negligible, and no systematic
13C
offsets were observed between C.
wuellerstorfi, C.
pachyderma, C.
mckannai, and P.
ariminensis. It should be noted, however, that both C.
mckannai and C.
pachyderma
13C
values were typically ~0.1
-0.2
lighter than C.
wuellerstorfi and P.
ariminensis, but the data density was insufficient to reliably
quantify systematic interspecific
13C
offsets. Specimens of C.
wuellerstorfi were common at Site 1020, and these were exclusively
picked for isotopic analysis at this site. An average of 12 specimens was picked
for analysis for each sample, although some samples yielded as few as 3-5
specimens, which were also analyzed.
Samples from Site 1014
were analyzed on the Woods Hole Oceanographic Institution Finnegan/MAT 252 mass
spectrometer with the Kiel automated carbonate preparation device. Samples were
not roasted before analysis. The external precision of the isotopic analyses was
±0.03 for
13C
and ±0.07
for
18O,
based on more than 1200 measurements of NBS-19 standard. Samples from Site 1020
were analyzed on the new Lamont-Doherty Earth Observatory (LDEO) VG Optima mass
spectrometer equipped with the automated multiprep carbonate preparation device
that, like the Kiel device, also acidifies samples individually. The external
precision for this instrument was ±0.05
for
13C
and ±0.06
for
18O,
based on numerous analyses of NBS-19.