Bauch: Planktic Foraminifera in Holocene Sediments from Lavtev Sea
607
Core IK9373·10
100
50 cJ!.
100
50 ~
0
T. clarkei
0
10
~ 0
5
G. tenella
0
I
_
- - - - r . . . , . . . . . . . . . . . ~~~ __ .,.......I_Lo' 0"
~ G glut:~~ A t/). l
" ' : o l - l - - . . . . . . . - - - - - r - ---.--~~~_ _ _ .
.
G. bulloides
I
i
,Q. , i
I
o
500
1000
1500
2000
2500
Age (y BP)
Figure 3: Variability of planktic foraminifera in core IK9373-1O from the Laptev Sea during the latc Holocene.
study at the continental slope of the Laptev Sea has yielded some specimens of C. ruher in
deglacial sediments (R.F. Spielhagen pers. com. 1997). Furthermore, ongoing investigations
in this region has confirmed the presence of C. ruber even in surface sediments (R. Volkmann
pefs. com. 1997) - it should be noted at this point that species such as C. ruher. C. tenella, and
607
Core IK9373·10
100
50 cJ!.
100
50 ~
0
T. clarkei
0
10
~ 0
5
G. tenella
0
I
_
- - - - r . . . , . . . . . . . . . . . ~~~ __ .,.......I_Lo' 0"
~ G glut:~~ A t/). l
" ' : o l - l - - . . . . . . . - - - - - r - ---.--~~~_ _ _ .
.
G. bulloides
I
i
,Q. , i
I
o
500
1000
1500
2000
2500
Age (y BP)
Figure 3: Variability of planktic foraminifera in core IK9373-1O from the Laptev Sea during the latc Holocene.
study at the continental slope of the Laptev Sea has yielded some specimens of C. ruher in
deglacial sediments (R.F. Spielhagen pers. com. 1997). Furthermore, ongoing investigations
in this region has confirmed the presence of C. ruber even in surface sediments (R. Volkmann
pefs. com. 1997) - it should be noted at this point that species such as C. ruher. C. tenella, and