Arid
DOI10.1016/j.jsames.2020.102959
Rock varnish in La Proveedora/Sonora in the context of desert geobiological processes and landscape evolution
Martinez-Pabello, Pavel U.; Sedov, Sergey; Solleiro-Rebolledo, Elizabeth; Sole, Jesus; Pi-Puig, Teresa; Alcantara-Hernandez, Rocio J.; Lebedeva, Marina; Shishkov, Vasily; Villalobos, Cesar
通讯作者Martinez-Pabello, PU (corresponding author), Univ Nacl Autonoma Mexico, Inst Geol, Mexico City, DF, Mexico.
来源期刊JOURNAL OF SOUTH AMERICAN EARTH SCIENCES
ISSN0895-9811
EISSN1873-0647
出版年2021
卷号105
英文摘要Desert varnish is a dark microlayer that forms on rocky surfaces that is usually associated with arid and desert environments. It consists mainly of clay minerals (60%), while the rest are Fe and Mn oxides. Growth rates are very slow and vary from <1 to 40 mu m/ky. Although different proposals exist to explain their formation mechanisms, these processes are still unknown. Around the world, various groups and human communities have created petroglyphs with different meanings in desert varnish. In the Sonoran Desert, the archaeological site La Proveedora is known for having many petroglyphs made in granite rock varnishes. It is believed that people groups occupied the area during the mid-Holocene (ca 5000-3000 BC). The research was carried out by analyzing and looking for possible signals and contributions from past environments and current processes that are preserved in the varnish layers. The X-ray diffraction, laser breakdown spectra and scanning electron microscopy with energy dispersive spectroscopy analyses in varnish samples, showed that the distribution and concentrations of Fe and Mn exhibit an alternating behavior on a depth scale from the surface until contact with granite. The DNA analysis showed a major presence of the Proteobacteria and Actinobacteria groups. Notably, some of these microorganisms can incorporate Fe and Mn into their metabolic processes and mobilize them through the varnish for its formation. The C-14 radiocarbon dating (370 +/- 54 cal BP) indicates a very young age associated primarily with recent microorganisms. However, a first approximation was obtained for the minimum age (50001000 yr BP). The comparison between the areas of varnish and the surfaces within the petroglyphs suggests that the varnish formation occurred under conditions in the past when the humidity was higher, and that it is probably a very slow, intermittent or uncoated formation mechanism today.
英文关键词Desert varnish Sonoran desert Petroglyph Fe and Mn oxides
类型Article
语种英语
收录类别SCI-E
WOS记录号WOS:000606797300005
WOS关键词NEGEV DESERT ; BACTERIAL COMMUNITIES ; MOJAVE DESERT ; NW SONORA ; SOIL ; MASS ; MEXICO ; DUST ; SPECTROSCOPY ; PLEISTOCENE
WOS类目Geosciences, Multidisciplinary
WOS研究方向Geology
来源机构Universidad Nacional Autónoma de México
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/348040
作者单位[Martinez-Pabello, Pavel U.; Sedov, Sergey; Solleiro-Rebolledo, Elizabeth; Alcantara-Hernandez, Rocio J.] Univ Nacl Autonoma Mexico, Inst Geol, Mexico City, DF, Mexico; [Sole, Jesus; Pi-Puig, Teresa] Univ Nacl Autonoma Mexico, Natl Lab Geochem & Minerol, Mexico City, DF, Mexico; [Lebedeva, Marina] VV Dokuchaev Soil Sci Inst, Pyzhevski Lane 7, Moscow 109017, Russia; [Shishkov, Vasily] Russian Acad Sci, Inst Geog, Starornonetnyi Per 29, Moscow 109017, Russia; [Villalobos, Cesar] Univ Nacl Autonoma Mexico, Inst Anthropol Res, Mexico City, DF, Mexico
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Martinez-Pabello, Pavel U.,Sedov, Sergey,Solleiro-Rebolledo, Elizabeth,et al. Rock varnish in La Proveedora/Sonora in the context of desert geobiological processes and landscape evolution[J]. Universidad Nacional Autónoma de México,2021,105.
APA Martinez-Pabello, Pavel U..,Sedov, Sergey.,Solleiro-Rebolledo, Elizabeth.,Sole, Jesus.,Pi-Puig, Teresa.,...&Villalobos, Cesar.(2021).Rock varnish in La Proveedora/Sonora in the context of desert geobiological processes and landscape evolution.JOURNAL OF SOUTH AMERICAN EARTH SCIENCES,105.
MLA Martinez-Pabello, Pavel U.,et al."Rock varnish in La Proveedora/Sonora in the context of desert geobiological processes and landscape evolution".JOURNAL OF SOUTH AMERICAN EARTH SCIENCES 105(2021).
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