Holocene records of the significance of ENSO on vegetation and fire ...
Holocene records of the significance of ENSO on vegetation and fire ...
Holocene records of the significance of ENSO on vegetation and fire ...
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RSBAA<br />
SBNWR<br />
Age (cal yrr<br />
B.P.)<br />
0<br />
500<br />
1000<br />
1500<br />
2000<br />
2500<br />
3000<br />
3500<br />
4000<br />
4500<br />
5000<br />
5500<br />
6000<br />
6500<br />
7000<br />
7500<br />
0.0<br />
CHAR Background Frequency<br />
Peaks Winter:Summer<br />
8000 0.0<br />
0.001<br />
10<br />
0.1<br />
00<br />
1.0<br />
00<br />
10. 000<br />
1000.000<br />
interbedded fluvial/wetl<strong>and</strong> sediments<br />
1000.000<br />
10. 000<br />
1.000<br />
0.100<br />
0.010<br />
01<br />
NAM <strong>on</strong><br />
<str<strong>on</strong>g>ENSO</str<strong>on</strong>g> <strong>on</strong><br />
↑ charcoal<br />
↑ winter taxa<br />
0 1 2 3 0 0.05 0.1<br />
particles/cm 2 /year <strong>fire</strong> episodes/100 years<br />
Less winter<br />
More winter<br />
SBC1<br />
SBC2<br />
SBC3<br />
SBC4<br />
SBC5<br />
NAM +/- / ??<br />
<str<strong>on</strong>g>ENSO</str<strong>on</strong>g> <str<strong>on</strong>g>of</str<strong>on</strong>g>f<br />
Little charcoal<br />
Summer taxa
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