FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2525109780> ?p ?o ?g. }

• W2525109780 endingPage "18" @default.
• W2525109780 startingPage "1" @default.
• W2525109780 abstract "We review the scientific efforts over the last decades to reconstruct erosion from continuous alpine lake sediment records. We focused both on methodological issues, showing the growing importance of non-destructive high resolution approaches (XRF core-scanner) as well as progresses in the understanding of processes leading to the creation of an “erosion signal” in lakes. We distinguish “continuous records” from “event-records”. Both provide complementary information but need to be studied with different approaches. Continuous regionally-relevant records proved to be particularly pertinent to document regional erosion patterns throughout the Holocene, in particular applying the source to sink approach. Event-based approaches demonstrated and took advantage of the strong non-linearity of sediment transport in high altitude catchment areas. This led to flood frequency and intensity reconstructions, highlighting the influence of climate change upon flood dynamics in the mountain. The combination of different record types, both in terms of location (high vs. low elevation), sedimentology (high vs. low terrigenous contribution) and significance (local vs. regional) is one of the main outputs of this paper. It allows the establishment of comprehensive histories of NW French Alps erosion, but also and consequently, soil dynamics and hydrological patterns throughout the Holocene. We also discuss the influence of glacier dynamics, one of the major agents of erosion in the Alps. A major feature is the growing human influence upon erosion at a local scale since at least the middle of the Bronze Age (3500 cal. BP). However and according to the regional record from Lake Bourget, only few periods of rising erosion at local scales generated a regional record that can be discriminated from wetter climatic periods. Among them, the period between 200 BCE and 400 AD appeared to be marked by a generalised rise in human-triggered erosion at local scales in the northern French Alps. This review highlights the importance of modern high-resolution and interdisciplinary studies of lake sediments, in order to better understand the complex relationships between humans, climate and the Earth system in general. We strongly argue that regional integration of data is now required to move a step further. Such an integration is easier with cost- and time-effective methods as well as after a better definition of approaches and their limits. This should lead to a stronger collaboration between paleo-data producers and modellers in the near future." @default.
• W2525109780 created "2016-10-07" @default.
• W2525109780 creator A5004556876 @default.
• W2525109780 creator A5004774480 @default.
• W2525109780 creator A5006228784 @default.
• W2525109780 creator A5011427084 @default.
• W2525109780 creator A5016629859 @default.
• W2525109780 creator A5017842655 @default.
• W2525109780 creator A5019947647 @default.
• W2525109780 creator A5026258068 @default.
• W2525109780 creator A5034508646 @default.
• W2525109780 creator A5039879273 @default.
• W2525109780 creator A5046411351 @default.
• W2525109780 creator A5061292285 @default.
• W2525109780 creator A5061845792 @default.
• W2525109780 creator A5062154198 @default.
• W2525109780 creator A5062312604 @default.
• W2525109780 creator A5076445271 @default.
• W2525109780 date "2016-11-01" @default.
• W2525109780 modified "2023-10-03" @default.
• W2525109780 title "Erosion under climate and human pressures: An alpine lake sediment perspective" @default.
• W2525109780 cites W1148218399 @default.
• W2525109780 cites W1606178640 @default.
• W2525109780 cites W1878944287 @default.
• W2525109780 cites W189294987 @default.
• W2525109780 cites W1970928310 @default.
• W2525109780 cites W1971787710 @default.
• W2525109780 cites W1974643559 @default.
• W2525109780 cites W1974905100 @default.
• W2525109780 cites W1976379518 @default.
• W2525109780 cites W1977133630 @default.
• W2525109780 cites W1978156774 @default.
• W2525109780 cites W1981374621 @default.
• W2525109780 cites W1986390233 @default.
• W2525109780 cites W1986538388 @default.
• W2525109780 cites W1987594750 @default.
• W2525109780 cites W1989133136 @default.
• W2525109780 cites W199778079 @default.
• W2525109780 cites W1999881354 @default.
• W2525109780 cites W2003951968 @default.
• W2525109780 cites W2004276248 @default.
• W2525109780 cites W2005307596 @default.
• W2525109780 cites W2006242401 @default.
• W2525109780 cites W2007520708 @default.
• W2525109780 cites W2011157936 @default.
• W2525109780 cites W2017411888 @default.
• W2525109780 cites W2017987119 @default.
• W2525109780 cites W2019879190 @default.
• W2525109780 cites W2021144947 @default.
• W2525109780 cites W2022831043 @default.
• W2525109780 cites W2024046719 @default.
• W2525109780 cites W2024556731 @default.
• W2525109780 cites W2025633481 @default.
• W2525109780 cites W2026708294 @default.
• W2525109780 cites W2026829506 @default.
• W2525109780 cites W2028556967 @default.
• W2525109780 cites W2029401070 @default.
• W2525109780 cites W2032452105 @default.
• W2525109780 cites W2032776094 @default.
• W2525109780 cites W2033021341 @default.
• W2525109780 cites W2037918186 @default.
• W2525109780 cites W2038407660 @default.
• W2525109780 cites W2042077545 @default.
• W2525109780 cites W2043842533 @default.
• W2525109780 cites W2047457932 @default.
• W2525109780 cites W2049039740 @default.
• W2525109780 cites W2049426453 @default.
• W2525109780 cites W2049468624 @default.
• W2525109780 cites W2055398859 @default.
• W2525109780 cites W2056026433 @default.
• W2525109780 cites W2056738992 @default.
• W2525109780 cites W2057490004 @default.
• W2525109780 cites W2060492247 @default.
• W2525109780 cites W2060616357 @default.
• W2525109780 cites W2061490208 @default.
• W2525109780 cites W2061756144 @default.
• W2525109780 cites W2062114723 @default.
• W2525109780 cites W2063197332 @default.
• W2525109780 cites W2063315385 @default.
• W2525109780 cites W2066041708 @default.
• W2525109780 cites W2066213566 @default.
• W2525109780 cites W2068681816 @default.
• W2525109780 cites W2070741120 @default.
• W2525109780 cites W2075191370 @default.
• W2525109780 cites W2075501958 @default.
• W2525109780 cites W2082127369 @default.
• W2525109780 cites W2083114381 @default.
• W2525109780 cites W2086922483 @default.
• W2525109780 cites W2087856222 @default.
• W2525109780 cites W2088483366 @default.
• W2525109780 cites W2089838027 @default.
• W2525109780 cites W2090164565 @default.
• W2525109780 cites W2090389358 @default.
• W2525109780 cites W2090435705 @default.
• W2525109780 cites W2090671389 @default.
• W2525109780 cites W2090736127 @default.
• W2525109780 cites W2094065994 @default.
• W2525109780 cites W2096196263 @default.

• next