Scott Mensing
Datos Biográficos
| ID | 343198 |
|---|---|
| NOMBRE | Scott Mensing |
| NOMBRES | Scott |
| APELLIDO | Mensing |
| FIRMA | MENSING S |
| AFILIACIONES | University of Nevada, Reno |
| ORCID | 0000-0003-4302-112X |
| VERIFICADO | Sí |
| TOTAL DE OBRAS | 23 |
| TOTAL DE CITAS | 77 |
| TOTAL COMO AUTOR | 23 |
| TOTAL COMO EDITOR | 0 |
| PRIMER AÑO DE PUBLICACIÓN | 1999 |
| AÑO MÁS RECIENTE DE PUBLICACIÓN | 2025 |
| ÍNDICE H | 5 |
Reconstruction of climatic and socio-economic impacts on the landscape of northern Tuscany (Italy) over the last 2000 years based on palaeoecological and historical evidence
Great Basin Survivance (USA)
The Late Holocene Dry Period (LHDP) was a one-plus millennial megadrought (3100-1800 cal BP) that delivered challenges and windfalls to Indigenous communities of the central Great Basin (United States). New pollen and sedimentation rate studies, combined with existing tree-ring data, submerged stump ages, and lake-level evidence, demonstrate that the LHDP was the driest Great Basin climate within the last 6,000 years-more extreme than the well-kn…
Identifying a Pre-Columbian Anthropocene in California
The beginning of the Anthropocene, a proposed geological epoch denoting human-caused changes to Earth’s systems, and what metrics signify its onset is currently under debate. Proposed initiation points range from the beginning of the Atomic Age to the Industrial Revolution to the adoption of agriculture in the early Holocene. Most of the debate centers on the effects of modern industrially oriented technological and economic development. The effe…
Reliability of the Artemisia /Chenopodiaceae pollen ratio in differentiating vegetation and reflecting moisture in arid and semi-arid China
The reliability of the ratio between Artemisia and Chenopodiaceae pollen percentage (i.e. A/ C) in differentiating vegetation and reflecting moisture conditions in arid and semi-arid regions has been disputed and this hindered its potential application in palaeoclimate reconstructions. In this paper, we investigated the A/ C ratios of lake-centre surface sediment from 45 lakes in the Inner Mongolia Plateau and the Qaidam Basin in arid and semi-ar…
Tyrrhenian central Italy
This paper compares changes in vegetation structure and composition (using synthetic fossil pollen data) with proxy data for population levels (including settlements and radiocarbon dates) over the course of the last 10 millennia in Tyrrhenian central Italy. These data show generalised patterns of clearance of woodland in response both to early agriculturalists and urbanism, as well as the specific adoption of tree crops and variations in stock g…
Using Paleolandscape Modeling to Investigate the Impact of Native American-Set Fires on Pre-Columbian Forests in the Southern Sierra Nevada, California, USA
Ethnographic accounts document widespread use of low-intensity surface fires by California's Native Americans to manage terrestrial resources, yet the effects of such practices on forest composition and structure remain largely unknown. Although numerous paleoenvironmental studies debate whether proxy interpretations indicate climatic or anthropogenic drivers of landscape change, available data sources (e.g., pollen, charcoal) are generally insuf…
Land Use and the Human Impact on the Environment in Medieval Italy
Modern narratives about changes in the Italian landscape during the early Middle Ages have often been based on assumptions about changing demography; the loss and replacement of complex Roman economic, political and agricultural systems; and broader changes in climate. Using fossil pollen taken from lake cores in the Rieti basin to reconstruct local ecological conditions, close examinations of two discreet periods offer new insights into the chan…
The value of non-pollen palynomorphs in interpreting paleoecological change in the Great Basin (Nevada, USA)
Non-pollen palynomorphs (NPPs) are identifiable microfossils that survive chemical digestion during pollen extraction and appear in pollen slides. They represent important proxies and indicators of environmental change that can be integrated with pollen studies of landscape history. NPPs have been widely studied in Europe since the 1970s and regularly included in paleoecological studies, whereas in the United States only the most common NPPs have…
Multi-disciplinary approach to identifying Native American impacts on Late Holocene forest dynamics in the southern Sierra Nevada range, California, USA
Human and climatically induced environmental change in the Mediterranean during the Medieval Climate Anomaly and Little Ice Age
The late Holocene drought
Late Holocene fire and vegetation reconstruction from the western Klamath Mountains, California, USA
The influence of Native American land-use practices on vegetation composition and structure has long been a subject of significant debate. This is particularly true in portions of the western United States where tribal hunter-gatherers did not use agriculture to meet subsistence and other cultural needs. Climate has been viewed as the dominant determinant of vegetation structure and composition change over time, but ethnographic and anthropologic…
High-precision AMS 14C chronology for Gatecliff Shelter, Nevada
A 9700-year multi-proxy reconstruction of hydrologic and vegetation history from a low-elevation spring-fed meadow, east central Nevada
A 15,000 year record of vegetation and climate change from a treeline lake in the Rocky Mountains, Wyoming, USA
Future climate projections predict warming at high elevations that will impact treeline species, but complex topographic relief in mountains complicates ecologic response, and we have a limited number of long-term studies examining vegetation change related to climate. In this study, pollen and conifer stomata were analyzed from a 2.3 m sediment core extending to 15,330 cal. yr BP recovered from a treeline lake in the Rocky Mountains of Wyoming. …
Changes in fire regimes since the Last Glacial Maximum
Extended drought in the Great Basin of western North America in the last two millennia reconstructed from pollen records
Radiocarbon Analysis Confirms the Annual Nature of Sagebrush Growth Rings
In the Great Basin of North America, big sagebrush ( Artemisia tridentata Nutt.) growth rings can be used to reconstruct environmental changes with annual resolution in areas where there is otherwise little such information available. We tested the annual nature of big sagebrush wood layers using accelerator mass spectrometry (AMS) radiocarbon dating. Four cross-sections from 3 sagebrush plants were collected near Ely, Nevada, USA, and analyzed u…
A Holocene pollen record of persistent droughts from Pyramid Lake, Nevada, USA
Pollen and algae microfossils preserved in sediments from Pyramid Lake, Nevada, provide evidence for periods of persistent drought during the Holocene age. We analyzed one hundred nineteen 1-cm-thick samples for pollen and algae from a set of cores that span the past 7630 years. The early middle Holocene, 7600 to 6300 cal yr B.P., was found to be the driest period, although it included one short but intense wet phase. We suggest that Lake Tahoe w…
Influence of the Pacific Decadal Oscillation on the climate of the Sierra Nevada, California and Nevada
Mono Lake sediments have recorded five major oscillations in the hydrologic balance between A.D. 1700 and 1941. These oscillations can be correlated with tree-ring-based oscillations in Sierra Nevada snowpack. Comparison of a tree-ring-based reconstruction of the Pacific Decadal Oscillation (PDO) index (D’Arrigo et al., 2001) with a coral-based reconstruction of Subtropical South Pacific sea-surface temperature (Linsley et al., 2000) indicates a …
Late-Glacial and Early Holocene Vegetation and Climate Change near Owens Lake, Eastern California
Pollen and algae from Owens Lake in eastern California provide evidence for a series of climatic oscillations late in the last glaciation. Juniper woodland, which dominated the Owens Valley from 16,200 to 15,500 cal yr B.P., suggests much wetter conditions than today. Although still wetter and cooler than today, the area then became fairly warm and dry, with woodland being replaced by shrubs (mainly sagebrush) from 15,500 to 13,100 cal yr B.P. Ne…
Land of Chamise and Pines
In marked contrast to California's landscape of urban sprawl, expansive agriculture, and wildlands altered by protectionist management systems, many landscapes in neighboring Baja California would still be recognizable to the first European explorers. This book shows that the vegetation of present-day Baja California is remarkably similar to that observed in the 18th and 19th centuries, and that historical fire and grazing management has done lit…
A 560-Year Record of Santa Ana Fires Reconstructed from Charcoal Deposited in the Santa Barbara Basin, California
Microscopic charcoal from varved Santa Barbara Basin sediments was used to reconstruct a 560-yr record (A.D. 1425 to 1985) of Santa Ana fires. Comparison of large (>3750 μm 2 ) charcoal with documented fire records in the Santa Barbara Ranger District shows that high accumulations correspond to large fires (>20,000 ha) that occurred during Santa Ana conditions. The charcoal record reconstructed a minimum of 20 large fires in the Santa Barbara reg…
High-precision AMS 14C chronology for Gatecliff Shelter, Nevada
Tyrrhenian central Italy
This paper compares changes in vegetation structure and composition (using synthetic fossil pollen data) with proxy data for population levels (including settlements and radiocarbon dates) over the course of the last 10 millennia in Tyrrhenian central Italy. These data show generalised patterns of clearance of woodland in response both to early agriculturalists and urbanism, as well as the specific adoption of tree crops and variations in stock g…
Human and climatically induced environmental change in the Mediterranean during the Medieval Climate Anomaly and Little Ice Age
Radiocarbon Analysis Confirms the Annual Nature of Sagebrush Growth Rings
In the Great Basin of North America, big sagebrush ( Artemisia tridentata Nutt.) growth rings can be used to reconstruct environmental changes with annual resolution in areas where there is otherwise little such information available. We tested the annual nature of big sagebrush wood layers using accelerator mass spectrometry (AMS) radiocarbon dating. Four cross-sections from 3 sagebrush plants were collected near Ely, Nevada, USA, and analyzed u…
Land of Chamise and Pines
In marked contrast to California's landscape of urban sprawl, expansive agriculture, and wildlands altered by protectionist management systems, many landscapes in neighboring Baja California would still be recognizable to the first European explorers. This book shows that the vegetation of present-day Baja California is remarkably similar to that observed in the 18th and 19th centuries, and that historical fire and grazing management has done lit…
Late Holocene fire and vegetation reconstruction from the western Klamath Mountains, California, USA
The influence of Native American land-use practices on vegetation composition and structure has long been a subject of significant debate. This is particularly true in portions of the western United States where tribal hunter-gatherers did not use agriculture to meet subsistence and other cultural needs. Climate has been viewed as the dominant determinant of vegetation structure and composition change over time, but ethnographic and anthropologic…
Using Paleolandscape Modeling to Investigate the Impact of Native American-Set Fires on Pre-Columbian Forests in the Southern Sierra Nevada, California, USA
Ethnographic accounts document widespread use of low-intensity surface fires by California's Native Americans to manage terrestrial resources, yet the effects of such practices on forest composition and structure remain largely unknown. Although numerous paleoenvironmental studies debate whether proxy interpretations indicate climatic or anthropogenic drivers of landscape change, available data sources (e.g., pollen, charcoal) are generally insuf…
Land Use and the Human Impact on the Environment in Medieval Italy
Modern narratives about changes in the Italian landscape during the early Middle Ages have often been based on assumptions about changing demography; the loss and replacement of complex Roman economic, political and agricultural systems; and broader changes in climate. Using fossil pollen taken from lake cores in the Rieti basin to reconstruct local ecological conditions, close examinations of two discreet periods offer new insights into the chan…
A 15,000 year record of vegetation and climate change from a treeline lake in the Rocky Mountains, Wyoming, USA
Future climate projections predict warming at high elevations that will impact treeline species, but complex topographic relief in mountains complicates ecologic response, and we have a limited number of long-term studies examining vegetation change related to climate. In this study, pollen and conifer stomata were analyzed from a 2.3 m sediment core extending to 15,330 cal. yr BP recovered from a treeline lake in the Rocky Mountains of Wyoming. …
Multi-disciplinary approach to identifying Native American impacts on Late Holocene forest dynamics in the southern Sierra Nevada range, California, USA
Great Basin Survivance (USA)
The Late Holocene Dry Period (LHDP) was a one-plus millennial megadrought (3100-1800 cal BP) that delivered challenges and windfalls to Indigenous communities of the central Great Basin (United States). New pollen and sedimentation rate studies, combined with existing tree-ring data, submerged stump ages, and lake-level evidence, demonstrate that the LHDP was the driest Great Basin climate within the last 6,000 years-more extreme than the well-kn…
A 560-Year Record of Santa Ana Fires Reconstructed from Charcoal Deposited in the Santa Barbara Basin, California
Microscopic charcoal from varved Santa Barbara Basin sediments was used to reconstruct a 560-yr record (A.D. 1425 to 1985) of Santa Ana fires. Comparison of large (>3750 μm 2 ) charcoal with documented fire records in the Santa Barbara Ranger District shows that high accumulations correspond to large fires (>20,000 ha) that occurred during Santa Ana conditions. The charcoal record reconstructed a minimum of 20 large fires in the Santa Barbara reg…
Land of Chamise and Pines
In marked contrast to California's landscape of urban sprawl, expansive agriculture, and wildlands altered by protectionist management systems, many landscapes in neighboring Baja California would still be recognizable to the first European explorers. This book shows that the vegetation of present-day Baja California is remarkably similar to that observed in the 18th and 19th centuries, and that historical fire and grazing management has done lit…
Late-Glacial and Early Holocene Vegetation and Climate Change near Owens Lake, Eastern California
Pollen and algae from Owens Lake in eastern California provide evidence for a series of climatic oscillations late in the last glaciation. Juniper woodland, which dominated the Owens Valley from 16,200 to 15,500 cal yr B.P., suggests much wetter conditions than today. Although still wetter and cooler than today, the area then became fairly warm and dry, with woodland being replaced by shrubs (mainly sagebrush) from 15,500 to 13,100 cal yr B.P. Ne…
Influence of the Pacific Decadal Oscillation on the climate of the Sierra Nevada, California and Nevada
Mono Lake sediments have recorded five major oscillations in the hydrologic balance between A.D. 1700 and 1941. These oscillations can be correlated with tree-ring-based oscillations in Sierra Nevada snowpack. Comparison of a tree-ring-based reconstruction of the Pacific Decadal Oscillation (PDO) index (D’Arrigo et al., 2001) with a coral-based reconstruction of Subtropical South Pacific sea-surface temperature (Linsley et al., 2000) indicates a …
A Holocene pollen record of persistent droughts from Pyramid Lake, Nevada, USA
Pollen and algae microfossils preserved in sediments from Pyramid Lake, Nevada, provide evidence for periods of persistent drought during the Holocene age. We analyzed one hundred nineteen 1-cm-thick samples for pollen and algae from a set of cores that span the past 7630 years. The early middle Holocene, 7600 to 6300 cal yr B.P., was found to be the driest period, although it included one short but intense wet phase. We suggest that Lake Tahoe w…
Radiocarbon Analysis Confirms the Annual Nature of Sagebrush Growth Rings
In the Great Basin of North America, big sagebrush ( Artemisia tridentata Nutt.) growth rings can be used to reconstruct environmental changes with annual resolution in areas where there is otherwise little such information available. We tested the annual nature of big sagebrush wood layers using accelerator mass spectrometry (AMS) radiocarbon dating. Four cross-sections from 3 sagebrush plants were collected near Ely, Nevada, USA, and analyzed u…
Changes in fire regimes since the Last Glacial Maximum
Extended drought in the Great Basin of western North America in the last two millennia reconstructed from pollen records
A 15,000 year record of vegetation and climate change from a treeline lake in the Rocky Mountains, Wyoming, USA
Future climate projections predict warming at high elevations that will impact treeline species, but complex topographic relief in mountains complicates ecologic response, and we have a limited number of long-term studies examining vegetation change related to climate. In this study, pollen and conifer stomata were analyzed from a 2.3 m sediment core extending to 15,330 cal. yr BP recovered from a treeline lake in the Rocky Mountains of Wyoming. …
A 9700-year multi-proxy reconstruction of hydrologic and vegetation history from a low-elevation spring-fed meadow, east central Nevada
High-precision AMS 14C chronology for Gatecliff Shelter, Nevada
The late Holocene drought
Late Holocene fire and vegetation reconstruction from the western Klamath Mountains, California, USA
The influence of Native American land-use practices on vegetation composition and structure has long been a subject of significant debate. This is particularly true in portions of the western United States where tribal hunter-gatherers did not use agriculture to meet subsistence and other cultural needs. Climate has been viewed as the dominant determinant of vegetation structure and composition change over time, but ethnographic and anthropologic…
Multi-disciplinary approach to identifying Native American impacts on Late Holocene forest dynamics in the southern Sierra Nevada range, California, USA
Human and climatically induced environmental change in the Mediterranean during the Medieval Climate Anomaly and Little Ice Age
The value of non-pollen palynomorphs in interpreting paleoecological change in the Great Basin (Nevada, USA)
Non-pollen palynomorphs (NPPs) are identifiable microfossils that survive chemical digestion during pollen extraction and appear in pollen slides. They represent important proxies and indicators of environmental change that can be integrated with pollen studies of landscape history. NPPs have been widely studied in Europe since the 1970s and regularly included in paleoecological studies, whereas in the United States only the most common NPPs have…
Using Paleolandscape Modeling to Investigate the Impact of Native American-Set Fires on Pre-Columbian Forests in the Southern Sierra Nevada, California, USA
Ethnographic accounts document widespread use of low-intensity surface fires by California's Native Americans to manage terrestrial resources, yet the effects of such practices on forest composition and structure remain largely unknown. Although numerous paleoenvironmental studies debate whether proxy interpretations indicate climatic or anthropogenic drivers of landscape change, available data sources (e.g., pollen, charcoal) are generally insuf…
Land Use and the Human Impact on the Environment in Medieval Italy
Modern narratives about changes in the Italian landscape during the early Middle Ages have often been based on assumptions about changing demography; the loss and replacement of complex Roman economic, political and agricultural systems; and broader changes in climate. Using fossil pollen taken from lake cores in the Rieti basin to reconstruct local ecological conditions, close examinations of two discreet periods offer new insights into the chan…
Tyrrhenian central Italy
This paper compares changes in vegetation structure and composition (using synthetic fossil pollen data) with proxy data for population levels (including settlements and radiocarbon dates) over the course of the last 10 millennia in Tyrrhenian central Italy. These data show generalised patterns of clearance of woodland in response both to early agriculturalists and urbanism, as well as the specific adoption of tree crops and variations in stock g…
Reliability of the Artemisia /Chenopodiaceae pollen ratio in differentiating vegetation and reflecting moisture in arid and semi-arid China
The reliability of the ratio between Artemisia and Chenopodiaceae pollen percentage (i.e. A/ C) in differentiating vegetation and reflecting moisture conditions in arid and semi-arid regions has been disputed and this hindered its potential application in palaeoclimate reconstructions. In this paper, we investigated the A/ C ratios of lake-centre surface sediment from 45 lakes in the Inner Mongolia Plateau and the Qaidam Basin in arid and semi-ar…
Identifying a Pre-Columbian Anthropocene in California
The beginning of the Anthropocene, a proposed geological epoch denoting human-caused changes to Earth’s systems, and what metrics signify its onset is currently under debate. Proposed initiation points range from the beginning of the Atomic Age to the Industrial Revolution to the adoption of agriculture in the early Holocene. Most of the debate centers on the effects of modern industrially oriented technological and economic development. The effe…
Great Basin Survivance (USA)
The Late Holocene Dry Period (LHDP) was a one-plus millennial megadrought (3100-1800 cal BP) that delivered challenges and windfalls to Indigenous communities of the central Great Basin (United States). New pollen and sedimentation rate studies, combined with existing tree-ring data, submerged stump ages, and lake-level evidence, demonstrate that the LHDP was the driest Great Basin climate within the last 6,000 years-more extreme than the well-kn…
Reconstruction of climatic and socio-economic impacts on the landscape of northern Tuscany (Italy) over the last 2000 years based on palaeoecological and historical evidence
Geography (20 obras) · Geology and Paleoclimatology Research (19 obras) · Physical geography (19 obras) · Archaeology (13 obras) · Climate change (12 obras) · Geology (12 obras) · Tree-ring climate responses (12 obras) · Ecology (10 obras) · Holocene (9 obras) · Structural basin (9 obras)