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2002). To overcome this limitation, a novel combined U-Th ion microprobe crystal rim. 62 analysis and (U-Th)/He bulk cry

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Geology A VOLCANIC ERUPTION IN THE SALTON TROUGH (SOUTHERN CALIFORNIA) DURING HUMAN PRESENCE --Manuscript Draft-Manuscript Number: Full Title:

A VOLCANIC ERUPTION IN THE SALTON TROUGH (SOUTHERN CALIFORNIA) DURING HUMAN PRESENCE

Short Title:

Salton Trough eruption

Article Type:

Article

Keywords:

zircon; geochronology; obsidian; archaeometry; Lake Cahuilla

Corresponding Author:

Axel K Schmitt, Dr University of California, Los Angeles Los Angeles, CA UNITED STATES

Corresponding Author Secondary Information: Corresponding Author's Institution:

University of California, Los Angeles

Corresponding Author's Secondary Institution: First Author:

Axel K Schmitt, Dr

First Author Secondary Information: Order of Authors:

Axel K Schmitt, Dr Arturo Martin, PhD Daniel F Stockli, PhD Kenneth A Farley, PhD Oscar M Lovera, PhD

Order of Authors Secondary Information: Manuscript Region of Origin:

UNITED STATES

Abstract:

U-Th and (U-Th)/He zircon geochronology redefines the timing of volcanic activity in the Salton Trough (southern California), the subaerial extension of the incipiently oceanic Gulf of California. U-series disequilibrium corrected (U-Th)/He zircon analyses for a granophyre ejecta clast from Red Island indicate an eruption age of 2,480±470 a (between 0 and 940 BCE; error at 95% confidence). This eruption age is supported by U-Th zircon crystallization ages for two rhyolite domes: Red Island (the host for the granophyre) and Obsidian Butte, a prehistoric quarry for obsidian which is widely distributed in southern California and northern Mexico archaeological sites. Lavas and granophyre display overlapping zircon crystallization age distributions, supporting field and compositional evidence that they are cogenetic and contemporaneous. The (UTh)/He eruption age is younger and significantly more precise than previous ages for these volcanoes. These results are the first evidence for an eruption during human presence in the region. They also provide an alternative explanation for the absence of the Obsidian Butte lithic source among early prehistoric cultural artifacts which previously been has been attributed to submergence of the quarry location during hypothesized persistent flooding by ancient Lake Cahuilla.

Suggested Reviewers:

Kathleen Nicoll University of Utah [email protected] expert on geoarchaeology Peter Reiners University of Arizona

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[email protected] U-Th/He geochronology pioneer, especially for xenolith dating young volcanic samples. Joann Stock Caltech [email protected] Strong background in volcano-tectonic processes during rifting, PI for Salton Sea Seismic Imaging project Opposed Reviewers:

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Cover letter Click here to download Cover letter: Letter Wyld revision v2.doc

*Manuscript Click here to download Manuscript: Schmitt_etal_2012_GEOLOGY_revision_v3.doc

1 2

A VOLCANIC ERUPTION IN THE SALTON TROUGH (SOUTHERN CALIFORNIA) DURING HUMAN PRESENCE

3 4

Axel K. Schmitt

5

Department of Earth and Space Sciences, UCLA

6

Los Angeles CA 90095-1567, USA

7

Phone: +310-206-5760; Email: [email protected]

8 9

Arturo Martín

10

Departamento de Geología, CICESE

11

Km 107 Carr. Tijuana - Ensenada., Ensenada, B.C., México, C.P. 22800

12 13

Daniel F. Stockli

14

Department of Geological Sciences, University of Texas

15

Austin, TX 78712

16 17

Kenneth A. Farley

18

Division of Geological and Planetary Sciences, California Institute of Technology

19

Pasadena, CA 91125

20 21

Oscar M. Lovera

22

Department of Earth and Space Sciences, UCLA

23

Los Angeles CA 90095-1567, USA

24 1

25

Abstract

26

U-Th and (U-Th)/He zircon geochronology redefines the timing of volcanic activity in

27

the Salton Trough (southern California), the subaerial extension of the incipiently oceanic

28

Gulf of California. U-series disequilibrium corrected (U-Th)/He zircon analyses for a

29

granophyre ejecta clast from Red Island indicate an eruption age of 2,480±470 a

30

(between 0 and 940 BCE; error at 95% confidence). This eruption age is supported by U-

31

Th zircon crystallization ages for two rhyolite domes: Red Island (the host for the

32

granophyre) and Obsidian Butte, a prehistoric quarry for obsidian which is widely

33

distributed in southern California and northern Mexico archaeological sites. Lavas and

34

granophyre display overlapping zircon crystallization age distributions, supporting field

35

and compositional evidence that they are cogenetic and contemporaneous. The (U-

36

Th)/He eruption age is younger and significantly more precise than previous ages for

37

these volcanoes. These results are the first evidence for an eruption during human

38

presence in the region. They also provide an alternative explanation for the absence of the

39

Obsidian Butte lithic source among early prehistoric cultural artifacts which previously

40

been has been attributed to submergence of the quarry location during hypothesized

41

persistent flooding by ancient Lake Cahuilla.

42 43

Keywords: zircon; geochronology; obsidian; archaeometry; Lake Cahuilla

44

2

45

INTRODUCTION

46

Volcanic chronostratigraphy is essential in understanding the timing of human origins,

47

migration, and exchange. Radiometric dating of volcanic rocks down to the historical

48

realm is possible in favorable cases by K-Ar (40Ar/39Ar) geochronology (e.g., the 79 CE

49

eruption of Vesuvius; Renne et al., 1997; Lanphere et al., 2007), but often accuracy is

50

compromised by excess 40Ar, parent-daughter mobility, or diffusive fractionation of

51

40

52

Morgan et al., 2009; Flude et al., 2010).

Ar/36Ar (e.g., Cerling et al., 1985; Esser et al., 1997; McDougall and Harrison, 1999;

53

(U-Th)/He geochronology of zircon as one of the first radiometric dating

54

techniques (Strutt, 1908) has experienced a revival as a thermochronometer, but it is

55

equally suitable for rapidly cooled volcanic rocks without subsequent thermal disturbance

56

(e.g., Tagami et al., 2003; Davidson et al., 2004; Schmitt et al., 2006; Blondes et al.,

57

2007). Compared to K-Ar (40Ar/39Ar) geochronology, it offers the advantages of reduced

58

excess 4He due to rapid diffusion (Reiners, 2004), high daughter isotope production rates

59

(4He/40Ar >20 per parent nucleus), and negligible atmospheric contamination (air Ar/He

60

~2000). Its application, however, has been limited by U-series disequilibrium effects,

61

which, in the case of zircon, typically cause severe age underestimation (Farley et al.,

62

2002). To overcome this limitation, a novel combined U-Th ion microprobe crystal rim

63

analysis and (U-Th)/He bulk crystal degassing analysis technique has been developed1.

64

Here, we apply this technique to document an eruption in the Salton Trough (southern

65

California) as recently as 0 - 940 BCE, and age which overlaps with human occupation of

1

to equal extent at UCLA by AKS and OML, and University of Kansas by DFS

3

66

southern California and northern Baja California, and agrees with the onset of obsidian

67

use in these locations (e.g., Schaefer and Laylander, 2007).

68 69

VOLCANISM IN THE SALTON TROUGH

70

The Salton Buttes together with Cerro Prieto and Roca Consag are the

71

morphologically most pristine volcanoes in the northern Gulf of California and Salton

72

Trough rift zone (Fig. 1). They form an ~7 km long, NE-SW trending lineament of five

73

rhyolite domes (1500 1160 BCE 1700 >1450 >750 1400 1400 >1400 640 645 1020

n artifacts source

reference

1 2 1 5 6 1 2 1 1 1 1 1 1 1 7 2 3 3 2 1 2 1 1 1 2 1 3 4 1 1 2 16 2 12 1 5 1 debitage 2

Rick et al. (2001) Rick et al. (2001) Rick et al. (2001) Rick et al. (2001) Rick et al. (2001) Rick et al. (2001) Rick et al. (2001) Rick et al. (2001) Rick et al. (2001) Rick et al. (2001) Rick et al. (2001) Rick et al. (2001) Rick et al. (2001) Rick et al. (2001) Rick et al. (2001) Rick et al. (2001) Rick et al. (2001) Rick et al. (2001) Rick et al. (2001) Rick et al. (2001) Rick et al. (2001) Rick et al. (2001) Rick et al. (2001) Rick et al. (2001) Rick et al. (2001) Erlandson et al. (2011) McDonald (1992) McDonald (1992) McDonald (1992) McDonald (1992) McDonald (1992) McDonald (1992) McDonald (1992) McDonald (1992) McDonald (1992) McDonald (1992) Kyle (1996) Love and Dahdul (2002) Porcayo-Michelini (2006)

Coso Coso Coso Coso Coso Coso Coso Coso Coso Coso Coso Coso Other Coso Coso Coso Coso Coso Coso Coso Coso Coso Coso Obsidian Butte Obsidian Butte Coso Obsidian Butte Obsidian Butte Obsidian Butte unknown San Felipe San Felipe San Felipe (?) Obsidian Butte Obsidian Butte Obsidian Butte Obsidian Butte Coso Obsidian Butte

all sites with prefix CA except Zaragoza (Baja California, Mexico) all ages CE (unless indicated) with minimum and maximum ages at 2σ absolute ages reported in literature were recalcualted to calendric ages using OxCal v. 3.10 references: Erlandson, J.M., Rick, T.C., Braje, T.J., Casperson, M., Culleton, B., Fulfrost, B., Garcia, T., Guthrie, T.A., Jew, N., Kennett, D.J., M

Kyle, C.E., 1996, A 2,000 year old milling tool kit from CA-SDI-10148, San Diego, California: Pacific Coast Archaeological Society Love, B., and Dahdul, M., 2002, Desert chronologies and the Archaic period in the Coachella Valley. Pacific Coast Archaeologica McDonald, A.M., 1992, Indian Hill rockshelter and aboriginal cultural adaptation in Anza-Borrego State Park, southeastern Cali Porcayo-Michelini, A., 2006, Informe final para el consejo de arqueología de los trabajos arqueologícos realizados en el sitio Ig Rick, T.C., Skinner, C.E., Erlandson, J.M., and Vellanoweth, R.L., 2002, Obsidian Source Characterization and Human Exchange S

T.A., Jew, N., Kennett, D.J., Moss, M.L., Reeder, L., Skinner, C., Watts, J., Willis, L., 2011, Paleoindian Seafaring, Maritime Technologies, and

Coast Archaeological Society Quarterly, v. 32(4), p. 76-87. y. Pacific Coast Archaeological Society Quarterly, v. 38(2-3), p. 66-86. State Park, southeastern California [Ph.D. thesis]: Riverside, University of McDonald, A.M., 1992, Indian Hill rockshelter and aboriginal cult ogícos realizados en el sitio Ignacio Zaragoza. Archivo del Centro INAH, Baja California. ation and Human Exchange Systems on California’s Channel Islands: Pacific Coast Archaeological Society Quarterly, v. 37(3), p. 28-44.

ritime Technologies, and Coastal Foraging on California’s Channel Islands: Science, v. 331, p. 1181-1185.

helter and aboriginal cultural adaptation in Anza-Borrego State Park, southeastern California [Ph.D. thesis]: Riverside, University of Califor

y, v. 37(3), p. 28-44.

side, University of California, 429 p.

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