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West Mojave Plan FEIR/S - Desert Managers Group

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MYACENOZOICEPOCHTable 3-65Paleontological Resources OverviewMAMMALASSEMBLAGES0Rancholabrean Rancho La Brea, Carpinteria Faunas (56).1 PLEISTOCENE Irvingtonian Manix, Bautista Faunas (Savage & Downs 1954:56).2 Coso Mt., San Timoteo FaunasPLIOCENE Blancan (Savage & Downs 1954:52).5Hemphillian Mt. Eden, Kern R. Fauna (Savage & Downs 1954:52).10 Clarendonian Ricardo, Avawatz, Tejon Hills, Mint Canyon Faunas(Savage & Downs 1954:52).15 MIOCENE Barstovian Barstow Fauna (Savage & Downs 1954:49).Tick Canyon Fauna (Savage & Downs 1954:49).20 Hemingfordian25 Arikareean Tecuya Fauna (Savage & Downs 1954:49).30 OLIGOCENE Whitneyan-Orellan Kew Quarry Fauna (Savage & Downs 1954:47).35 Chadronian Titus Canyon Fauna (Savage & Downs 1954:47).40 Duchesnean Pearson Ranch Fauna (Savage & Downs 1954:47).45 EOCENE Uintan Poway Fauna (Savage & Downs 1954:47).50 BridgerianWasatchian55 ClarkforkianTiffanian60 PALEOCENE Torrejonian65 Dragonian-Puercan70(Woodburne 1978:26)Tecopa Lake Beds consist of lacustrine siltstone and mudstone interbedded with layers oftufa and ash that range from 100 feet to 200 feet thick. Multiple vertebrate fossils have beenrecovered from exposures east of Tecopa Hot Springs, though numerous finds occur west andnorth. This area is one of only two placed that provide good examples of small Irvingtonian-agemammals. Additionally, it has yielded remains of a unique camel-like animal unknownelsewhere (Woodburne 1978:37).The Avawatz Formation occurs in the rugged canyon land exposures on the south andsouthwestern flank of Avawatz Peak as well as along slivers of the Garlock and Death ValleyFault Zones. These deposits consist of coarse-grained conglomerate overlain by interbeddedclaystone, sandstone, and coarse- to fine-grained conglomerate. Coarse-grained breccia overliesthe claystone section and is capped by arenaceous clastic sediments and some tuff with coarsegrainedsandstone at the top. Faunal remains occur in the upper Clarendonian age unit(Woodburne 1978:49).Pleistocene-age fossil bones have been reported in the lake sediments of Salt Spring HillsPlaya, but not collected (Woodburne 1978:51).Chapter 3 3-289

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