Elizabeth Solleiro-Rebolledo
Dados Biográficos
| ID | 4020811 |
|---|---|
| NOME | Elizabeth Solleiro-Rebolledo |
| PRENOMES | Elizabeth |
| SOBRENOME | Solleiro-Rebolledo |
| ASSINATURA | SOLLEIRO-REBOLLEDO E |
| AFILIAÇÕES | Universidad Nacional Autonoma de Mexico |
| ORCID | 0000-0001-7395-8429 |
| VERIFICADO | Sim |
| TOTAL DE OBRAS | 22 |
| TOTAL DE CITAÇÕES | 24 |
| TOTAL COMO AUTOR | 22 |
| TOTAL COMO EDITOR | 0 |
| PRIMEIRO ANO DE PUBLICAÇÃO | 2003 |
| ANO MAIS RECENTE DE PUBLICAÇÃO | 2023 |
| ÍNDICE H | 4 |
Magnetic properties as indicators of pedogenic and pyrogenic processes at the Upper Paleolithic site of Kostenki 14
In geoarchaeological studies, there is an issue with distinguishing between natural and anthropogenic signals in pedological paleoarchives. With the pedostratigraphy of the Upper Paleolithic site of Kostenki 14, this issue is reflected by problems with the determination of features of pedogenic and pyrogenic processes. This issue was addressed by means of a thorough analysis of the magnetic properties of paleosols accompanied by micromorphologica…
Evidence for stages of landscape evolution in Central Mexico during the late Quaternary from paleosol-pedosediment sequences
Paleosols interbedded with pyroclastic deposits have been proven to be an important paleoenvironmental proxy for the late Quaternary in Central Mexico. We studied a key upland section and several profiles on the slopes and lowlands of the Tlaxcala Block, assuming that the topographic variability of the soil-sedimentary mantle contains the complete record of the landscape history. The upland section included three paleosols separated by tepetates …
Late Quaternary paleosols and landscape evolution in dune systems of Veracruz at the Gulf of Mexico coast
Rock varnish as a natural canvas for rock art in La Proveedora, northwestern Sonoran Desert (Mexico)
Black clayey soil (Vertisol) in the Lerma valley, Michoacán, North‐Central Mexico
Catastrophic events (climatic, tectonic, volcanic, etc.) frequently cause geomorphological instability, which interrupts normal pedogenesis and switches the processes of surface erosion and/or sedimentation. These processes have an effect on the distribution of ancient settlements and can be the cause of the abandonment of cities. In the Lerma Valley, particularly in the Tres Mezquites area, surveys and extensive excavations have been conducted t…
Early Holocene charcoal accumulations in the Aktun Ha cenote
An integrative methodology, including controlled heating experiments, petrography, taphonomy, systematics of charcoal fragments, solid‐state 13 C nuclear magnetic resonance (NMR) spectroscopy, differential scanning calorimetry (DSC), and 14 C dating, are used to discriminate in situ (anthropogenic) versus transported charcoal accumulations in the Ancestors Chamber at the Aktun Ha cenote and its potential relationship with the initial settlement o…
The role of pedogenesis in palaeosols of Mexico basin and its implication in the paleoenvironmental reconstruction
Environmental setting of the early irrigation in Oasisamerica
Reworked volcaniclastic deposits from the Usumacinta river, Mexico
The origin and distribution of volcanic glass temper in Maya ceramics has attracted the attention of Mesoamerican archaeologists for the last 80 years. Several Quaternary volcanoes, particularly those in the Central American Volcanic Arc (CAVA), are proposed as the source of tephra in the Maya region, however, a continuous stratigraphic record of this tephra deposit is still lacking. A reworked volcaniclastic deposit (9 ± 2 ka) was located in the…
Mineral magnetic properties of an alluvial paleosol sequence in the Maya Lowlands
Guest editors preface
Soil development on a beach ridge chronosequence in the Gulf of Mexico coastal plain and its relation to the ancient land use
Spatial variability of Late Pleistocene–Early Holocene soil formation and its relation to early human paleoecology in Northwest Mexico
Phytoliths, stable carbon isotopes and micromorphology of a buried alluvial soil in Southern Mexico
Archaic settlement in El Tebernal, Veracruz
Population Dynamics and Its Relation to Ancient Landscapes in the Northwestern Maya Lowlands
In this article we present for discussion certain aspects of settlement and paleo-environmental data obtained over the last few years for the northwestern Maya lowlands. Accordingly, our goal is to identify a point of departure for future research by presenting a list of possible "environmental attractors" that might later be used for a better understanding of the seemingly divergent trajectories shown by ancient communities located in different …
Paleoenvironment and Human Occupation in the M aya Lowlands of the U sumacinta R iver, S outhern M exico
Paleosol sequences along the lowest terraces of the U sumacinta R iver in southern M exico were used to reconstruct H olocene environmental changes and examine human–environmental interactions. Study sections were correlated through paleosol morphology, radiocarbon dating, and artifact seriation of Formative, C lassic, and P ostclassic ceramics. The oldest paleosols have gleyic features. Although they contain hard carbonate concretions dating to …
The Black San Pablo Paleosol of the Teotihuacan Valley, Mexico
Although archaeologists have generally assumed that the ancient landscape in the Teotihuacan Valley was somewhat similar to the present day, recent research has documented large‐scale modification of the soil by accelerated human‐induced erosion–sedimentation processes from the pre‐Hispanic and Colonial periods up until the present. Consequently, the Formative and Classic period soil (approximately 400 B.C.–A.D. 650) is buried in most of the Teot…
The Deposition and Chronology of Cenote T ’isil
Cenotes (natural wells or sinkholes) comprise the most common landscape features in the northern M aya L owlands of the Y ucatán P eninsula, M éxico. Detailed study of dated soil‐sedimentary sequences, recovered from a cenote at the archaeological site T ’isil and nearby wetlands, allows a partial reconstruction of environmental variability at the site for the last 2000 years. Biogenic calcite sedimentation and C alcisol development occur during …
Adaptation Of Maya Homegardens By “Container Gardening” In Limestone Bedrock Cavities
The northern Maya Lowlands of the Yucatán Peninsula are often characterized by outside observers as a challenging environment for agriculturalists. The limestone bedrock appears to have only a patchy cover of thin soil, yet the Maya inhabitants, both ancient and modern, have managed to successfully cultivate this landscape through a variety innovative techniques and micro-scale adaptations. Homegardens have a long history in the region, and conti…
Spatial variability of environment change in the Teotihuacan Valley during the Late Quaternary
Mineral and organic components of the buried paleosols of the Nevado de Toluca, Central Mexico as indicators of paleoenvironments and soil evolution
The Black San Pablo Paleosol of the Teotihuacan Valley, Mexico
Although archaeologists have generally assumed that the ancient landscape in the Teotihuacan Valley was somewhat similar to the present day, recent research has documented large‐scale modification of the soil by accelerated human‐induced erosion–sedimentation processes from the pre‐Hispanic and Colonial periods up until the present. Consequently, the Formative and Classic period soil (approximately 400 B.C.–A.D. 650) is buried in most of the Teot…
Reworked volcaniclastic deposits from the Usumacinta river, Mexico
The origin and distribution of volcanic glass temper in Maya ceramics has attracted the attention of Mesoamerican archaeologists for the last 80 years. Several Quaternary volcanoes, particularly those in the Central American Volcanic Arc (CAVA), are proposed as the source of tephra in the Maya region, however, a continuous stratigraphic record of this tephra deposit is still lacking. A reworked volcaniclastic deposit (9 ± 2 ka) was located in the…
Paleoenvironment and Human Occupation in the M aya Lowlands of the U sumacinta R iver, S outhern M exico
Paleosol sequences along the lowest terraces of the U sumacinta R iver in southern M exico were used to reconstruct H olocene environmental changes and examine human–environmental interactions. Study sections were correlated through paleosol morphology, radiocarbon dating, and artifact seriation of Formative, C lassic, and P ostclassic ceramics. The oldest paleosols have gleyic features. Although they contain hard carbonate concretions dating to …
The Deposition and Chronology of Cenote T ’isil
Cenotes (natural wells or sinkholes) comprise the most common landscape features in the northern M aya L owlands of the Y ucatán P eninsula, M éxico. Detailed study of dated soil‐sedimentary sequences, recovered from a cenote at the archaeological site T ’isil and nearby wetlands, allows a partial reconstruction of environmental variability at the site for the last 2000 years. Biogenic calcite sedimentation and C alcisol development occur during …
Magnetic properties as indicators of pedogenic and pyrogenic processes at the Upper Paleolithic site of Kostenki 14
In geoarchaeological studies, there is an issue with distinguishing between natural and anthropogenic signals in pedological paleoarchives. With the pedostratigraphy of the Upper Paleolithic site of Kostenki 14, this issue is reflected by problems with the determination of features of pedogenic and pyrogenic processes. This issue was addressed by means of a thorough analysis of the magnetic properties of paleosols accompanied by micromorphologica…
Population Dynamics and Its Relation to Ancient Landscapes in the Northwestern Maya Lowlands
In this article we present for discussion certain aspects of settlement and paleo-environmental data obtained over the last few years for the northwestern Maya lowlands. Accordingly, our goal is to identify a point of departure for future research by presenting a list of possible "environmental attractors" that might later be used for a better understanding of the seemingly divergent trajectories shown by ancient communities located in different …
Mineral and organic components of the buried paleosols of the Nevado de Toluca, Central Mexico as indicators of paleoenvironments and soil evolution
Spatial variability of environment change in the Teotihuacan Valley during the Late Quaternary
Adaptation Of Maya Homegardens By “Container Gardening” In Limestone Bedrock Cavities
The northern Maya Lowlands of the Yucatán Peninsula are often characterized by outside observers as a challenging environment for agriculturalists. The limestone bedrock appears to have only a patchy cover of thin soil, yet the Maya inhabitants, both ancient and modern, have managed to successfully cultivate this landscape through a variety innovative techniques and micro-scale adaptations. Homegardens have a long history in the region, and conti…
The Deposition and Chronology of Cenote T ’isil
Cenotes (natural wells or sinkholes) comprise the most common landscape features in the northern M aya L owlands of the Y ucatán P eninsula, M éxico. Detailed study of dated soil‐sedimentary sequences, recovered from a cenote at the archaeological site T ’isil and nearby wetlands, allows a partial reconstruction of environmental variability at the site for the last 2000 years. Biogenic calcite sedimentation and C alcisol development occur during …
Paleoenvironment and Human Occupation in the M aya Lowlands of the U sumacinta R iver, S outhern M exico
Paleosol sequences along the lowest terraces of the U sumacinta R iver in southern M exico were used to reconstruct H olocene environmental changes and examine human–environmental interactions. Study sections were correlated through paleosol morphology, radiocarbon dating, and artifact seriation of Formative, C lassic, and P ostclassic ceramics. The oldest paleosols have gleyic features. Although they contain hard carbonate concretions dating to …
The Black San Pablo Paleosol of the Teotihuacan Valley, Mexico
Although archaeologists have generally assumed that the ancient landscape in the Teotihuacan Valley was somewhat similar to the present day, recent research has documented large‐scale modification of the soil by accelerated human‐induced erosion–sedimentation processes from the pre‐Hispanic and Colonial periods up until the present. Consequently, the Formative and Classic period soil (approximately 400 B.C.–A.D. 650) is buried in most of the Teot…
Archaic settlement in El Tebernal, Veracruz
Population Dynamics and Its Relation to Ancient Landscapes in the Northwestern Maya Lowlands
In this article we present for discussion certain aspects of settlement and paleo-environmental data obtained over the last few years for the northwestern Maya lowlands. Accordingly, our goal is to identify a point of departure for future research by presenting a list of possible "environmental attractors" that might later be used for a better understanding of the seemingly divergent trajectories shown by ancient communities located in different …
Spatial variability of Late Pleistocene–Early Holocene soil formation and its relation to early human paleoecology in Northwest Mexico
Phytoliths, stable carbon isotopes and micromorphology of a buried alluvial soil in Southern Mexico
Mineral magnetic properties of an alluvial paleosol sequence in the Maya Lowlands
Guest editors preface
Soil development on a beach ridge chronosequence in the Gulf of Mexico coastal plain and its relation to the ancient land use
Reworked volcaniclastic deposits from the Usumacinta river, Mexico
The origin and distribution of volcanic glass temper in Maya ceramics has attracted the attention of Mesoamerican archaeologists for the last 80 years. Several Quaternary volcanoes, particularly those in the Central American Volcanic Arc (CAVA), are proposed as the source of tephra in the Maya region, however, a continuous stratigraphic record of this tephra deposit is still lacking. A reworked volcaniclastic deposit (9 ± 2 ka) was located in the…
The role of pedogenesis in palaeosols of Mexico basin and its implication in the paleoenvironmental reconstruction
Environmental setting of the early irrigation in Oasisamerica
Early Holocene charcoal accumulations in the Aktun Ha cenote
An integrative methodology, including controlled heating experiments, petrography, taphonomy, systematics of charcoal fragments, solid‐state 13 C nuclear magnetic resonance (NMR) spectroscopy, differential scanning calorimetry (DSC), and 14 C dating, are used to discriminate in situ (anthropogenic) versus transported charcoal accumulations in the Ancestors Chamber at the Aktun Ha cenote and its potential relationship with the initial settlement o…
Rock varnish as a natural canvas for rock art in La Proveedora, northwestern Sonoran Desert (Mexico)
Black clayey soil (Vertisol) in the Lerma valley, Michoacán, North‐Central Mexico
Catastrophic events (climatic, tectonic, volcanic, etc.) frequently cause geomorphological instability, which interrupts normal pedogenesis and switches the processes of surface erosion and/or sedimentation. These processes have an effect on the distribution of ancient settlements and can be the cause of the abandonment of cities. In the Lerma Valley, particularly in the Tres Mezquites area, surveys and extensive excavations have been conducted t…
Evidence for stages of landscape evolution in Central Mexico during the late Quaternary from paleosol-pedosediment sequences
Paleosols interbedded with pyroclastic deposits have been proven to be an important paleoenvironmental proxy for the late Quaternary in Central Mexico. We studied a key upland section and several profiles on the slopes and lowlands of the Tlaxcala Block, assuming that the topographic variability of the soil-sedimentary mantle contains the complete record of the landscape history. The upland section included three paleosols separated by tepetates …
Late Quaternary paleosols and landscape evolution in dune systems of Veracruz at the Gulf of Mexico coast
Magnetic properties as indicators of pedogenic and pyrogenic processes at the Upper Paleolithic site of Kostenki 14
In geoarchaeological studies, there is an issue with distinguishing between natural and anthropogenic signals in pedological paleoarchives. With the pedostratigraphy of the Upper Paleolithic site of Kostenki 14, this issue is reflected by problems with the determination of features of pedogenic and pyrogenic processes. This issue was addressed by means of a thorough analysis of the magnetic properties of paleosols accompanied by micromorphologica…
Geology (20 obras) · Geology and Paleoclimatology Research (19 obras) · Paleontology (18 obras) · Geography (14 obras) · Paleosol (13 obras) · Soil Science (13 obras) · Soil water (13 obras) · Archaeology and ancient environmental studies (12 obras) · Geochemistry (12 obras) · Loess (11 obras)