FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2765241490> ?p ?o ?g. }

• W2765241490 endingPage "1638" @default.
• W2765241490 startingPage "1626" @default.
• W2765241490 abstract "Fjords and old-growth forests store large amounts of organic carbon. Yet the role of episodic disturbances, particularly volcanic eruptions, in mobilizing organic carbon in fjord landscapes covered by temperate rainforests remains poorly quantified. To this end, we estimated how much wood and soils were flushed to nearby fjords following the 2008 eruption of Chaitén volcano in south-central Chile, where pyroclastic sediments covered >12 km2 of pristine temperate rainforest. Field-based surveys of forest biomass, soil organic content, and dead wood transport reveal that the reworking of pyroclastic sediments delivered ~66,500 + 14,600/−14,500 tC of large wood to two rivers entering the nearby Patagonian fjords in less than a decade. A similar volume of wood remains in dead tree stands and buried beneath pyroclastic deposits (~79,900 + 21,100/−16,900 tC) or stored in active river channels (5,900–10,600 tC). We estimate that bank erosion mobilized ~132,300+21,700/−30,600 tC of floodplain forest soil. Eroded and reworked forest soils have been accreting on coastal river deltas at >5 mm yr−1 since the eruption. While much of the large wood is transported out of the fjord by long-shore drift, the finer fraction from eroded forest soils is likely to be buried in the fjords. We conclude that the organic carbon fluxes boosted by rivers adjusting to high pyroclastic sediment loads may remain elevated for up to a decade and that Patagonian temperate rainforests disturbed by excessive loads of pyroclastic debris can be episodic short-lived carbon sources." @default.
• W2765241490 created "2017-11-10" @default.
• W2765241490 creator A5013654589 @default.
• W2765241490 creator A5057151723 @default.
• W2765241490 creator A5060822280 @default.
• W2765241490 creator A5083393978 @default.
• W2765241490 date "2017-11-01" @default.
• W2765241490 modified "2023-10-17" @default.
• W2765241490 title "Pyroclastic Eruption Boosts Organic Carbon Fluxes Into Patagonian Fjords" @default.
• W2765241490 cites W1494431475 @default.
• W2765241490 cites W1500766476 @default.
• W2765241490 cites W1516902267 @default.
• W2765241490 cites W1521595634 @default.
• W2765241490 cites W1530495053 @default.
• W2765241490 cites W1536977965 @default.
• W2765241490 cites W1543619409 @default.
• W2765241490 cites W1668593943 @default.
• W2765241490 cites W1754490558 @default.
• W2765241490 cites W1823786200 @default.
• W2765241490 cites W1980000448 @default.
• W2765241490 cites W1981213426 @default.
• W2765241490 cites W1981827347 @default.
• W2765241490 cites W2001320907 @default.
• W2765241490 cites W2011433554 @default.
• W2765241490 cites W2022767712 @default.
• W2765241490 cites W2025018931 @default.
• W2765241490 cites W2028450370 @default.
• W2765241490 cites W2032735291 @default.
• W2765241490 cites W2037885538 @default.
• W2765241490 cites W2042376056 @default.
• W2765241490 cites W2044589526 @default.
• W2765241490 cites W2048126105 @default.
• W2765241490 cites W2049070397 @default.
• W2765241490 cites W2049321881 @default.
• W2765241490 cites W2059094503 @default.
• W2765241490 cites W2061461870 @default.
• W2765241490 cites W2064922284 @default.
• W2765241490 cites W2070420656 @default.
• W2765241490 cites W2079864021 @default.
• W2765241490 cites W2081377455 @default.
• W2765241490 cites W2089813380 @default.
• W2765241490 cites W2092926079 @default.
• W2765241490 cites W2093919674 @default.
• W2765241490 cites W2094105589 @default.
• W2765241490 cites W2100484010 @default.
• W2765241490 cites W2110235309 @default.
• W2765241490 cites W2121218279 @default.
• W2765241490 cites W2123040072 @default.
• W2765241490 cites W2126164335 @default.
• W2765241490 cites W2126544705 @default.
• W2765241490 cites W2144224158 @default.
• W2765241490 cites W2154073704 @default.
• W2765241490 cites W2154717657 @default.
• W2765241490 cites W2156513415 @default.
• W2765241490 cites W2162348455 @default.
• W2765241490 cites W2165079227 @default.
• W2765241490 cites W2166490975 @default.
• W2765241490 cites W2174069807 @default.
• W2765241490 cites W2314527272 @default.
• W2765241490 cites W2336514688 @default.
• W2765241490 cites W2340358307 @default.
• W2765241490 cites W2412609444 @default.
• W2765241490 cites W2491955056 @default.
• W2765241490 cites W2609261196 @default.
• W2765241490 cites W94049490 @default.
• W2765241490 doi "https://doi.org/10.1002/2017gb005647" @default.
• W2765241490 hasPublicationYear "2017" @default.
• W2765241490 type Work @default.
• W2765241490 sameAs 2765241490 @default.
• W2765241490 citedByCount "13" @default.
• W2765241490 countsByYear W27652414902019 @default.
• W2765241490 countsByYear W27652414902020 @default.
• W2765241490 countsByYear W27652414902021 @default.
• W2765241490 countsByYear W27652414902022 @default.
• W2765241490 countsByYear W27652414902023 @default.
• W2765241490 crossrefType "journal-article" @default.
• W2765241490 hasAuthorship W2765241490A5013654589 @default.
• W2765241490 hasAuthorship W2765241490A5057151723 @default.
• W2765241490 hasAuthorship W2765241490A5060822280 @default.
• W2765241490 hasAuthorship W2765241490A5083393978 @default.
• W2765241490 hasBestOaLocation W27652414901 @default.
• W2765241490 hasConcept C111368507 @default.
• W2765241490 hasConcept C114793014 @default.
• W2765241490 hasConcept C120806208 @default.
• W2765241490 hasConcept C127313418 @default.
• W2765241490 hasConcept C135310875 @default.
• W2765241490 hasConcept C146348940 @default.
• W2765241490 hasConcept C158787203 @default.
• W2765241490 hasConcept C159390177 @default.
• W2765241490 hasConcept C159750122 @default.
• W2765241490 hasConcept C17409809 @default.
• W2765241490 hasConcept C187320778 @default.
• W2765241490 hasConcept C18903297 @default.
• W2765241490 hasConcept C20113989 @default.
• W2765241490 hasConcept C2619416 @default.
• W2765241490 hasConcept C2816523 @default.
• W2765241490 hasConcept C39432304 @default.
• W2765241490 hasConcept C76886044 @default.

• next