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All Biocode files are based on field identifications to the best of the researcher’s ability at the time.
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In TJM2, changed to: Condea emoryi
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In TJM2, changed to: Condea emoryi
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In TJM2, changed to: Condea emoryi
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canyon bottom drainage course among volcanic hills with Vachellia, Stenocereus thurberi, Ambrosia, Ceiba acuminata, Iresine, Perityle leptoglossa
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canyon bottom drainage course among volcanic hills with Vachellia, Stenocereus thurberi, Ambrosia, Ceiba acuminata, Iresine, Perityle leptoglossa
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canyon bottom drainage course among volcanic hills with Vachellia, Stenocereus thurberi, Ambrosia, Ceiba acuminata, Iresine, Perityle leptoglossa
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canyon bottom drainage course among volcanic hills with Vachellia, Stenocereus thurberi, Ambrosia, Ceiba acuminata, Iresine, Perityle leptoglossa
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2017 California Academy of Sciences
CalPhotos
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2017 California Academy of Sciences
CalPhotos
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in thorn scrub thicket on coarse granitic soil of gently sloping coastal plain.
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in thorn scrub thicket on coarse granitic soil of gently sloping coastal plain.
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on narrow sandy drainage crossing flats behind beach dunes of Playa Las Tunas
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on narrow sandy drainage crossing flats behind beach dunes of Playa Las Tunas
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on narrow sandy drainage crossing flats behind beach dunes of Playa Las Tunas
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on narrow sandy drainage crossing flats behind beach dunes of Playa Las Tunas
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on narrow sandy drainage crossing flats behind beach dunes of Playa Las Tunas
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roadcut in volcanic rubble of steeply terraced mid-canyon slope. This and other pre-2013 collecting sites on this famous scenic descent into Barranca Batopilas are now largely buried by construction of new paved highway to Batopilas.
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in disturbed soils of alleyway adjacent to undeveloped area
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in disturbed soils of alleyway adjacent to undeveloped area
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in disturbed soils of alleyway adjacent to undeveloped area
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on steep, western facing, mid elevation slope of Barranca Batopilas, volcanic rhyolitic tuff substrate
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on steep, western facing, mid elevation slope of Barranca Batopilas, volcanic rhyolitic tuff substrate
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on steep, western facing, mid elevation slope of Barranca Batopilas, volcanic rhyolitic tuff substrate
