FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2111843934> ?p ?o ?g. }

• W2111843934 endingPage "1452" @default.
• W2111843934 startingPage "1439" @default.
• W2111843934 abstract "The Marboré Cirque, which is located in the southern Central Pyrenees on the north face of the Monte Perdido Peak (42°40′0″N; 0.5°0″W; 3355 m), contains a wide variety of Holocene glacial and periglacial deposits, and those from the ‘Little Ice Age’ (‘LIA’) are particularly well developed. Based on geomorphological mapping, cosmogenic exposure dating and previous studies of lacustrine sediment cores, the different deposits were dated and a sequence of geomorphological and paleoenvironmental events was established as follows: (1) The Marboré Cirque was at least partially deglaciated before 12.7 kyr BP. (2) Some ice masses are likely to have persisted in the Early Holocene, although their moraines were destroyed by the advance of glaciers during the Mid Holocene and ‘LIA’. (3) A glacial expansion occurred during the Mid Holocene (5.1 ± 0.1 kyr), represented by a large push moraine that enclosed a unique ice mass at the foot of the Monte Perdido Massif. (4) A melting phase occurred at approximately 3.4 ± 0.2 and 2.5 ± 0.1 kyr (Bronze/Iron Ages) after one of the most important glacial advances of the Neoglacial period. (5) Another glacial expansion occurred during the Dark Age Cold Period (1.4–1.2 kyr), followed by a melting period during the Medieval Climate Anomaly. (6) The ‘LIA’ represented a clear stage of glacial expansion within the Marboré Cirque. Two different pulses of glaciation were detected, separated by a short retraction. The first pulse occurred most likely during the late 17th century or early 18th century (Maunder Minimum), whereas the second occurred between 1790 and ad 1830 (Dalton Minimum). A strong deglaciation process has affected the Marboré Cirque glaciers since the middle of the 19th century. (7) A large rock avalanche occurred during the Mid Holocene, leaving a chaotic deposit that was previously considered to be a Late Glacial moraine." @default.
• W2111843934 created "2016-06-24" @default.
• W2111843934 creator A5013792700 @default.
• W2111843934 creator A5018862525 @default.
• W2111843934 creator A5026527064 @default.
• W2111843934 creator A5035815902 @default.
• W2111843934 creator A5063511748 @default.
• W2111843934 creator A5082160598 @default.
• W2111843934 date "2014-08-12" @default.
• W2111843934 modified "2023-10-02" @default.
• W2111843934 title "Holocene and ‘Little Ice Age’ glacial activity in the Marboré Cirque, Monte Perdido Massif, Central Spanish Pyrenees" @default.
• W2111843934 cites W1481885754 @default.
• W2111843934 cites W1496922909 @default.
• W2111843934 cites W157310239 @default.
• W2111843934 cites W1585899189 @default.
• W2111843934 cites W1772990943 @default.
• W2111843934 cites W1964332098 @default.
• W2111843934 cites W1966442470 @default.
• W2111843934 cites W1974755922 @default.
• W2111843934 cites W1974957281 @default.
• W2111843934 cites W1975183126 @default.
• W2111843934 cites W1975350041 @default.
• W2111843934 cites W1976819442 @default.
• W2111843934 cites W1978754311 @default.
• W2111843934 cites W1979436104 @default.
• W2111843934 cites W1979479398 @default.
• W2111843934 cites W1981999632 @default.
• W2111843934 cites W1982502727 @default.
• W2111843934 cites W1987865635 @default.
• W2111843934 cites W1988123755 @default.
• W2111843934 cites W1988331452 @default.
• W2111843934 cites W1996855210 @default.
• W2111843934 cites W2002473398 @default.
• W2111843934 cites W2003051332 @default.
• W2111843934 cites W2010955985 @default.
• W2111843934 cites W2014460114 @default.
• W2111843934 cites W2014961122 @default.
• W2111843934 cites W2016651782 @default.
• W2111843934 cites W2017241772 @default.
• W2111843934 cites W2032621606 @default.
• W2111843934 cites W2032819288 @default.
• W2111843934 cites W2041139567 @default.
• W2111843934 cites W2042246112 @default.
• W2111843934 cites W2044438318 @default.
• W2111843934 cites W2046088904 @default.
• W2111843934 cites W2049068688 @default.
• W2111843934 cites W2059175769 @default.
• W2111843934 cites W2065231029 @default.
• W2111843934 cites W2071173487 @default.
• W2111843934 cites W2071634360 @default.
• W2111843934 cites W2073473784 @default.
• W2111843934 cites W2075394653 @default.
• W2111843934 cites W2079479246 @default.
• W2111843934 cites W2079548035 @default.
• W2111843934 cites W2080210901 @default.
• W2111843934 cites W2089755791 @default.
• W2111843934 cites W2089998748 @default.
• W2111843934 cites W2092519422 @default.
• W2111843934 cites W2100054721 @default.
• W2111843934 cites W2103737089 @default.
• W2111843934 cites W2105437508 @default.
• W2111843934 cites W2107648631 @default.
• W2111843934 cites W2111308404 @default.
• W2111843934 cites W2111892553 @default.
• W2111843934 cites W2114448181 @default.
• W2111843934 cites W2118407115 @default.
• W2111843934 cites W2120637384 @default.
• W2111843934 cites W2129096709 @default.
• W2111843934 cites W2129622504 @default.
• W2111843934 cites W2136246993 @default.
• W2111843934 cites W2143451212 @default.
• W2111843934 cites W2147458491 @default.
• W2111843934 cites W2154787858 @default.
• W2111843934 cites W2166493077 @default.
• W2111843934 cites W2170559393 @default.
• W2111843934 cites W2172259751 @default.
• W2111843934 cites W2297299121 @default.
• W2111843934 cites W2297811765 @default.
• W2111843934 cites W2300342679 @default.
• W2111843934 cites W2306359893 @default.
• W2111843934 cites W2413896038 @default.
• W2111843934 cites W2527582552 @default.
• W2111843934 doi "https://doi.org/10.1177/0959683614544053" @default.
• W2111843934 hasPublicationYear "2014" @default.
• W2111843934 type Work @default.
• W2111843934 sameAs 2111843934 @default.
• W2111843934 citedByCount "62" @default.
• W2111843934 countsByYear W21118439342015 @default.
• W2111843934 countsByYear W21118439342016 @default.
• W2111843934 countsByYear W21118439342017 @default.
• W2111843934 countsByYear W21118439342018 @default.
• W2111843934 countsByYear W21118439342019 @default.
• W2111843934 countsByYear W21118439342020 @default.
• W2111843934 countsByYear W21118439342021 @default.
• W2111843934 countsByYear W21118439342022 @default.
• W2111843934 countsByYear W21118439342023 @default.
• W2111843934 crossrefType "journal-article" @default.
• W2111843934 hasAuthorship W2111843934A5013792700 @default.

• next