Charline Giguet-Covex
Dados Biográficos
| ID | 2740596 |
|---|---|
| NOME | Charline Giguet-Covex |
| PRENOMES | Charline |
| SOBRENOME | Giguet-Covex |
| ASSINATURA | GIGUET-COVEX C |
| AFILIAÇÕES | Centre National de la Recherche Scientifique |
| ORCID | 0000-0002-5141-4815 |
| VERIFICADO | Sim |
| TOTAL DE OBRAS | 10 |
| TOTAL DE CITAÇÕES | 4 |
| TOTAL COMO AUTOR | 10 |
| TOTAL COMO EDITOR | 0 |
| PRIMEIRO ANO DE PUBLICAÇÃO | 2011 |
| ANO MAIS RECENTE DE PUBLICAÇÃO | 2025 |
| ÍNDICE H | 1 |
A 7,000 years trajectory of socio-ecosystems in the montane belt of the northern French Alps
Introduction This study, conducted on the Plateau des Glières, in the northern French Alps, investigates the evolution of vegetation composition over the past 7000 years. This site, within a montane ecosystem, offers a new opportunity to understand the human and landscape interactions under the influence of climate. To study these interactions as a whole and by integrating their complexity, we used two conceptual frameworks: the agroecosystem and…
Half of the soil erosion in the Alps during the Holocene is explained by transient erosion crises as a consequence of rapid human land clearing
Human land use changes have altered soil erosion for millennia with extensive consequences on terrestrial and aquatic ecosystems as well as on biogeochemical cycles along the land-ocean continuum. Despite their great importance, past erosion trends have high uncertainties limiting quantitative estimates of long-term erosion dynamics. Here, we applied a new approach combining well-dated paleo-records of soil erosion from lake sediments and a spati…
Bioarchaeological approaches to understanding the long-term development of mountain societies
Archaeologists do not always differentiate between human activities, practices and techniques within landscape archaeology. This problem is reflected in some research into the development of pastoralism in the Alps. Here, we develop a framework within a "position paper" that engages with these different processes by assessing recent developments in bioarchaeological and palaeoenvironmental methods. Over the last two decades, alpine research has m…
Reconstructing Paleoflood Occurrence and Magnitude from Lake Sediments
Lake sediments are a valuable archive to document past flood occurrence and magnitude, and their evolution over centuries to millennia. This information has the potential to greatly improve current flood design and risk assessment approaches, which are hampered by the shortness and scarcity of gauge records. For this reason, paleoflood hydrology from lake sediments received fast-growing attention over the last decade. This allowed an extensive de…
Lake Sedimentary DNA Research on Past Terrestrial and Aquatic Biodiversity
The use of lake sedimentary DNA to track the long-term changes in both terrestrial and aquatic biota is a rapidly advancing field in paleoecological research. Although largely applied nowadays, knowledge gaps remain in this field and there is therefore still research to be conducted to ensure the reliability of the sedimentary DNA signal. Building on the most recent literature and seven original case studies, we synthesize the state-of-the-art an…
Paravani, a puzzling lake in the South Caucasus
Frequency and intensity of high-altitude floods over the last 3.5 ka in northwestern French Alps (Lake Anterne)
In central Western Europe, several studies have shown that colder Holocene periods, such as the Little Ice Age, also correspond to wet periods. However, in mountain areas which are highly sensitive to erosion processes and where precipitation events can be localized, past evolution of hydrological activity might be more complicated. To assess these past hydrological changes, a paleolimnological approach was applied on a 13.4-m-long sediment core …
High-resolution record of Holocene erosion patterns in a high altitude lake (Lake Anterne, NW French Alps)
Recent ecological state evolution of four high altitude lakes (French Alps)
Changes in erosion patterns during the Holocene in a currently treeless subalpine catchment inferred from lake sediment geochemistry (Lake Anterne, 2063 m a.s.l., NW French Alps)
A high-resolution sedimentological and geochemical study was performed on a 20 m long core from the alpine Lake Anterne (2063 m a.s.l., NW French Alps) spanning the last 10 ka. Sedimentation is mainly of minerogenic origin. The organic matter quantity (TOC%) as well as its quality (hydrogen (HI) and oxygen (OI) indices) both indicate the progressive onset and subsequent stabilization of vegetation cover in the catchment from 9950 to 5550 cal. BP.…
Bioarchaeological approaches to understanding the long-term development of mountain societies
Archaeologists do not always differentiate between human activities, practices and techniques within landscape archaeology. This problem is reflected in some research into the development of pastoralism in the Alps. Here, we develop a framework within a "position paper" that engages with these different processes by assessing recent developments in bioarchaeological and palaeoenvironmental methods. Over the last two decades, alpine research has m…
Changes in erosion patterns during the Holocene in a currently treeless subalpine catchment inferred from lake sediment geochemistry (Lake Anterne, 2063 m a.s.l., NW French Alps)
A high-resolution sedimentological and geochemical study was performed on a 20 m long core from the alpine Lake Anterne (2063 m a.s.l., NW French Alps) spanning the last 10 ka. Sedimentation is mainly of minerogenic origin. The organic matter quantity (TOC%) as well as its quality (hydrogen (HI) and oxygen (OI) indices) both indicate the progressive onset and subsequent stabilization of vegetation cover in the catchment from 9950 to 5550 cal. BP.…
Frequency and intensity of high-altitude floods over the last 3.5 ka in northwestern French Alps (Lake Anterne)
In central Western Europe, several studies have shown that colder Holocene periods, such as the Little Ice Age, also correspond to wet periods. However, in mountain areas which are highly sensitive to erosion processes and where precipitation events can be localized, past evolution of hydrological activity might be more complicated. To assess these past hydrological changes, a paleolimnological approach was applied on a 13.4-m-long sediment core …
High-resolution record of Holocene erosion patterns in a high altitude lake (Lake Anterne, NW French Alps)
Recent ecological state evolution of four high altitude lakes (French Alps)
Lake Sedimentary DNA Research on Past Terrestrial and Aquatic Biodiversity
The use of lake sedimentary DNA to track the long-term changes in both terrestrial and aquatic biota is a rapidly advancing field in paleoecological research. Although largely applied nowadays, knowledge gaps remain in this field and there is therefore still research to be conducted to ensure the reliability of the sedimentary DNA signal. Building on the most recent literature and seven original case studies, we synthesize the state-of-the-art an…
Paravani, a puzzling lake in the South Caucasus
Reconstructing Paleoflood Occurrence and Magnitude from Lake Sediments
Lake sediments are a valuable archive to document past flood occurrence and magnitude, and their evolution over centuries to millennia. This information has the potential to greatly improve current flood design and risk assessment approaches, which are hampered by the shortness and scarcity of gauge records. For this reason, paleoflood hydrology from lake sediments received fast-growing attention over the last decade. This allowed an extensive de…
Bioarchaeological approaches to understanding the long-term development of mountain societies
Archaeologists do not always differentiate between human activities, practices and techniques within landscape archaeology. This problem is reflected in some research into the development of pastoralism in the Alps. Here, we develop a framework within a "position paper" that engages with these different processes by assessing recent developments in bioarchaeological and palaeoenvironmental methods. Over the last two decades, alpine research has m…
Half of the soil erosion in the Alps during the Holocene is explained by transient erosion crises as a consequence of rapid human land clearing
Human land use changes have altered soil erosion for millennia with extensive consequences on terrestrial and aquatic ecosystems as well as on biogeochemical cycles along the land-ocean continuum. Despite their great importance, past erosion trends have high uncertainties limiting quantitative estimates of long-term erosion dynamics. Here, we applied a new approach combining well-dated paleo-records of soil erosion from lake sediments and a spati…
A 7,000 years trajectory of socio-ecosystems in the montane belt of the northern French Alps
Introduction This study, conducted on the Plateau des Glières, in the northern French Alps, investigates the evolution of vegetation composition over the past 7000 years. This site, within a montane ecosystem, offers a new opportunity to understand the human and landscape interactions under the influence of climate. To study these interactions as a whole and by integrating their complexity, we used two conceptual frameworks: the agroecosystem and…
Geography (9 obras) · Geology and Paleoclimatology Research (8 obras) · Geology (7 obras) · Physical geography (7 obras) · Holocene (6 obras) · Ecology (5 obras) · Erosion (5 obras) · Oceanography (5 obras) · Archaeology (4 obras) · Geological formations and processes (4 obras)