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Holocene records of the significance of ENSO on vegetation and fire ...

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age (cal yr BP)<br />

-100<br />

0<br />

100<br />

200<br />

300<br />

400<br />

500<br />

600<br />

700<br />

800<br />

900<br />

1000<br />

1100<br />

1200<br />

1300<br />

1400<br />

1500<br />

1600<br />

1700<br />

1800<br />

1900<br />

2000<br />

2100<br />

2200<br />

2300<br />

2400<br />

2500<br />

2600<br />

2700<br />

2800<br />

2900<br />

3000<br />

Canelo Hills, AZ<br />

Winter Wet<br />

Artemisia S WW W<br />

Geraniaceae e H<br />

Brassicaceae ae H WW<br />

Amaranthace ceae H SW<br />

Asteraceae H H SW<br />

Summer Wet<br />

Ambrosia H SW S<br />

Cirsium H SW SW<br />

Chicory H SW SW<br />

Poaceae H SW S<br />

Euphorbiacea eae H SW<br />

Rosaceae SSW S S<br />

Cyperaceae WL W<br />

Aquatic<br />

total Pinaceae ae E<br />

herbs<br />

SUMS<br />

shrubs<br />

trees<br />

20 40 20 40 60 20 40 20 40 60 80 20 40 60 80 100 20<br />

The initiati<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> Canelo Hills cienega (or reactivati<strong>on</strong>) at ~3000 cal yr BP,<br />

<str<strong>on</strong>g>the</str<strong>on</strong>g> same time that it gets wet again at Cloverdale

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