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Williams-Climate-change-refugia-for-terrestrial-biodiversity_0

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Group Short name Name Units Source citation Grids<br />

Regolith GEOLRGE Range in geological age<br />

168 <strong>Climate</strong> <strong>change</strong> <strong>refugia</strong> <strong>for</strong> <strong>terrestrial</strong> <strong>biodiversity</strong><br />

Millions of<br />

years BP<br />

Regolith FERT Inherent rock fertility Index<br />

Regolith PC1_20<br />

Regolith PC2_20<br />

Regolith PC3_20<br />

Regolith PC1_80<br />

Regolith PC2_80<br />

Regolith PC3_80<br />

Regolith ILL20<br />

Regolith KAO20<br />

Regolith SME20<br />

Regolith ILL80<br />

Regolith KAO80<br />

Regolith SME80<br />

Regolith CTIDEPTH<br />

Spectra of surficial topsoils 0-<br />

20cm – Principal component 1<br />

Spectra of surficial topsoils 0-<br />

20cm – Principal component 2<br />

Spectra of surficial topsoils 0-<br />

20cm – Principal component 3<br />

Spectra of surficial subsoils 60-<br />

80cm – Principal component 1<br />

Spectra of surficial subsoils 60-<br />

80cm – Principal component 2<br />

Spectra of surficial subsoils 60-<br />

80cm – Principal component 3<br />

relative abundance of illite clay<br />

minerals in surficial topsoil (0-<br />

20cm)<br />

relative abundance of kaolinite<br />

clay minerals in surficial topsoil<br />

(0-20cm)<br />

relative abundance of smectite<br />

clay minerals in surficial topsoil<br />

(0-20cm)<br />

relative abundance of illite clay<br />

minerals in surficial subsoil (60-<br />

80cm)<br />

relative abundance of kaolinite<br />

clay minerals in surficial subsoil<br />

(60-80cm)<br />

relative abundance of smectite<br />

clay minerals in surficial subsoil<br />

(60-80cm)<br />

Soil depth in metres derived<br />

from a topographic wetness<br />

index scaled by map unit soil<br />

depth range<br />

Index<br />

Index<br />

Index<br />

Index<br />

Index<br />

index<br />

Proportion<br />

Proportion<br />

proportion<br />

proportion<br />

proportion<br />

proportion<br />

Metres<br />

al., 2012)<br />

(Laurie et al.,<br />

2008, Raymond,<br />

2009, <strong>Williams</strong> et<br />

al., 2012)<br />

(De Vries, 2009,<br />

Raymond, 2009)<br />

Viscarra-Rossel<br />

and Chen (2011)<br />

Viscarra-Rossel<br />

and Chen (2011)<br />

Viscarra-Rossel<br />

and Chen (2011)<br />

Viscarra-Rossel<br />

and Chen (2011)<br />

(Viscarra-Rossel<br />

& Chen, 2011)<br />

(Viscarra-Rossel<br />

& Chen, 2011)<br />

Viscarra Rossel<br />

(2011)<br />

Viscarra Rossel<br />

(2011)<br />

Viscarra Rossel<br />

(2011)<br />

Viscarra Rossel<br />

(2011)<br />

Viscarra Rossel<br />

(2011)<br />

Viscarra Rossel<br />

(2011)<br />

KJW unpublished,<br />

Claridge et al.<br />

(2000), (Bureau of<br />

Rural Sciences,<br />

2000, McKenzie<br />

et al., 2000,<br />

Western &<br />

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