Desiccation cracks provide evidence of lake drying on Mars, Sutton Island member, Murray formation, Gale Crater

N. Stein; J. P. Grotzinger; J. Schieber; N. Mangold; B. Hallet; H. Newsom; K. M. Stack; J. A. Berger; L. Thompson; K. L. Siebach; A. Cousin; S. Le Mouélic; M. Minitti; D. Y. Sumner; C. Fedo; C. H. House; S. Gupta; A. R. Vasavada; R. Gellert; R. C. Wiens; J. Frydenvang; O. Forni; P. Y. Meslin; V. Payré; E. Dehouck

doi:10.1130/G40005.1

Desiccation cracks provide evidence of lake drying on Mars, Sutton Island member, Murray formation, Gale Crater

N. Stein, J. P. Grotzinger, J. Schieber, N. Mangold, B. Hallet, H. Newsom, K. M. Stack, J. A. Berger, L. Thompson, K. L. Siebach, A. Cousin, S. Le Mouélic, M. Minitti, D. Y. Sumner, C. Fedo, C. H. House, S. Gupta, A. R. Vasavada, R. Gellert, R. C. WiensJ. Frydenvang, O. Forni, P. Y. Meslin, V. Payré, E. Dehouck

Research output: Contribution to journal › Article

21 Scopus citations

Abstract

Mars Science Laboratory (MSL) Curiosity rover data are used to describe the morphology of desiccation cracks observed in ancient lacustrine strata at Gale crater, Mars, and to interpret their paleoenvironmental setting. The desiccation cracks indicate subaerial exposure of lacustrine facies in the Sutton Island member of the Murray formation. In association with ripple cross-stratification and possible eolian cross-bedding, these facies indicate a transition from longer-lived perennial lakes recorded by older strata to younger lakes characterized by intermittent exposure. The transition from perennial to episodically exposed lacustrine environments provides evidence for local to regional climate change that can help constrain Mars climate models.

Original language	English (US)
Pages (from-to)	515-518
Number of pages	4
Journal	Geology
Volume	46
Issue number	6
DOIs	https://doi.org/10.1130/G40005.1
State	Published - Jun 1 2018

All Science Journal Classification (ASJC) codes

Geology

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10.1130/G40005.1

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Stein, N., Grotzinger, J. P., Schieber, J., Mangold, N., Hallet, B., Newsom, H., Stack, K. M., Berger, J. A., Thompson, L., Siebach, K. L., Cousin, A., Le Mouélic, S., Minitti, M., Sumner, D. Y., Fedo, C., House, C. H., Gupta, S., Vasavada, A. R., Gellert, R., ... Dehouck, E. (2018). Desiccation cracks provide evidence of lake drying on Mars, Sutton Island member, Murray formation, Gale Crater. Geology, 46(6), 515-518. https://doi.org/10.1130/G40005.1

Stein, N. ; Grotzinger, J. P. ; Schieber, J. ; Mangold, N. ; Hallet, B. ; Newsom, H. ; Stack, K. M. ; Berger, J. A. ; Thompson, L. ; Siebach, K. L. ; Cousin, A. ; Le Mouélic, S. ; Minitti, M. ; Sumner, D. Y. ; Fedo, C. ; House, C. H. ; Gupta, S. ; Vasavada, A. R. ; Gellert, R. ; Wiens, R. C. ; Frydenvang, J. ; Forni, O. ; Meslin, P. Y. ; Payré, V. ; Dehouck, E. / Desiccation cracks provide evidence of lake drying on Mars, Sutton Island member, Murray formation, Gale Crater. In: Geology. 2018 ; Vol. 46, No. 6. pp. 515-518.

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title = "Desiccation cracks provide evidence of lake drying on Mars, Sutton Island member, Murray formation, Gale Crater",

abstract = "Mars Science Laboratory (MSL) Curiosity rover data are used to describe the morphology of desiccation cracks observed in ancient lacustrine strata at Gale crater, Mars, and to interpret their paleoenvironmental setting. The desiccation cracks indicate subaerial exposure of lacustrine facies in the Sutton Island member of the Murray formation. In association with ripple cross-stratification and possible eolian cross-bedding, these facies indicate a transition from longer-lived perennial lakes recorded by older strata to younger lakes characterized by intermittent exposure. The transition from perennial to episodically exposed lacustrine environments provides evidence for local to regional climate change that can help constrain Mars climate models.",

author = "N. Stein and Grotzinger, {J. P.} and J. Schieber and N. Mangold and B. Hallet and H. Newsom and Stack, {K. M.} and Berger, {J. A.} and L. Thompson and Siebach, {K. L.} and A. Cousin and {Le Mou{\'e}lic}, S. and M. Minitti and Sumner, {D. Y.} and C. Fedo and House, {C. H.} and S. Gupta and Vasavada, {A. R.} and R. Gellert and Wiens, {R. C.} and J. Frydenvang and O. Forni and Meslin, {P. Y.} and V. Payr{\'e} and E. Dehouck",

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doi = "10.1130/G40005.1",

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Stein, N, Grotzinger, JP, Schieber, J, Mangold, N, Hallet, B, Newsom, H, Stack, KM, Berger, JA, Thompson, L, Siebach, KL, Cousin, A, Le Mouélic, S, Minitti, M, Sumner, DY, Fedo, C, House, CH, Gupta, S, Vasavada, AR, Gellert, R, Wiens, RC, Frydenvang, J, Forni, O, Meslin, PY, Payré, V & Dehouck, E 2018, 'Desiccation cracks provide evidence of lake drying on Mars, Sutton Island member, Murray formation, Gale Crater', Geology, vol. 46, no. 6, pp. 515-518. https://doi.org/10.1130/G40005.1

Desiccation cracks provide evidence of lake drying on Mars, Sutton Island member, Murray formation, Gale Crater. / Stein, N.; Grotzinger, J. P.; Schieber, J.; Mangold, N.; Hallet, B.; Newsom, H.; Stack, K. M.; Berger, J. A.; Thompson, L.; Siebach, K. L.; Cousin, A.; Le Mouélic, S.; Minitti, M.; Sumner, D. Y.; Fedo, C.; House, C. H.; Gupta, S.; Vasavada, A. R.; Gellert, R.; Wiens, R. C.; Frydenvang, J.; Forni, O.; Meslin, P. Y.; Payré, V.; Dehouck, E.

In: Geology, Vol. 46, No. 6, 01.06.2018, p. 515-518.

Research output: Contribution to journal › Article

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AU - Stein, N.

AU - Grotzinger, J. P.

AU - Schieber, J.

AU - Mangold, N.

AU - Hallet, B.

AU - Newsom, H.

AU - Stack, K. M.

AU - Berger, J. A.

AU - Thompson, L.

AU - Siebach, K. L.

AU - Cousin, A.

AU - Le Mouélic, S.

AU - Minitti, M.

AU - Sumner, D. Y.

AU - Fedo, C.

AU - House, C. H.

AU - Gupta, S.

AU - Vasavada, A. R.

AU - Gellert, R.

AU - Wiens, R. C.

AU - Frydenvang, J.

AU - Forni, O.

AU - Meslin, P. Y.

AU - Payré, V.

AU - Dehouck, E.

PY - 2018/6/1

Y1 - 2018/6/1

N2 - Mars Science Laboratory (MSL) Curiosity rover data are used to describe the morphology of desiccation cracks observed in ancient lacustrine strata at Gale crater, Mars, and to interpret their paleoenvironmental setting. The desiccation cracks indicate subaerial exposure of lacustrine facies in the Sutton Island member of the Murray formation. In association with ripple cross-stratification and possible eolian cross-bedding, these facies indicate a transition from longer-lived perennial lakes recorded by older strata to younger lakes characterized by intermittent exposure. The transition from perennial to episodically exposed lacustrine environments provides evidence for local to regional climate change that can help constrain Mars climate models.

AB - Mars Science Laboratory (MSL) Curiosity rover data are used to describe the morphology of desiccation cracks observed in ancient lacustrine strata at Gale crater, Mars, and to interpret their paleoenvironmental setting. The desiccation cracks indicate subaerial exposure of lacustrine facies in the Sutton Island member of the Murray formation. In association with ripple cross-stratification and possible eolian cross-bedding, these facies indicate a transition from longer-lived perennial lakes recorded by older strata to younger lakes characterized by intermittent exposure. The transition from perennial to episodically exposed lacustrine environments provides evidence for local to regional climate change that can help constrain Mars climate models.

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