FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2790733439> ?p ?o ?g. }

• W2790733439 endingPage "305" @default.
• W2790733439 startingPage "285" @default.
• W2790733439 abstract "Detailed microscopic investigations of horizons in a surface paleosol, part of a pedostratigraphic stack of tills at New Mountain, Antarctica, dated to the middle Miocene climatic optimum event (ca. 15 Ma), suggest not only that the paleoclimate history of the continent can be read from stratigraphic layers within paleosols but also that records of cosmic events may lie embedded in coatings on sand clasts resident in paleosols. Recent microscopic and chemical data from sands in the upper horizons of a surface paleosol (Ant-828), adjacent to the Taylor Glacier, contain Fe and Na coatings surfaced with cosmic signatures including welded and shock-melted grains, opaque carbon coatings, microfeature stack of cards, Fe spherules, solubilized grain surfaces with streams of melted skin, a grain carrying an Ir signature, rare earth elements elevated above crustal averages, and slightly elevated Pt/Pd ratios. The projected link to the probable black-mat event of 12.8 ka is reinforced by the presence of fresh opaque carbon and other cosmic signatures on grain surfaces that overlie well-weathered grain features, presumably weathering from middle Miocene time near today. Evidence of CO2 and NOx accumulations dated to 12.9 ka in the Taylor Ice Dome suggest that the black-mat impact/airburst of the same time line as the Younger Dryas boundary may have reached across South America and the Pacific Ocean to the Dry Valley Mountains of Antarctica." @default.
• W2790733439 created "2018-03-29" @default.
• W2790733439 creator A5041545020 @default.
• W2790733439 creator A5055270180 @default.
• W2790733439 creator A5067293477 @default.
• W2790733439 creator A5067447916 @default.
• W2790733439 creator A5083211055 @default.
• W2790733439 date "2018-05-01" @default.
• W2790733439 modified "2023-09-23" @default.
• W2790733439 title "Did the Black-Mat Impact/Airburst Reach the Antarctic? Evidence from New Mountain Near the Taylor Glacier in the Dry Valley Mountains" @default.
• W2790733439 cites W1586351031 @default.
• W2790733439 cites W1688376315 @default.
• W2790733439 cites W1904145318 @default.
• W2790733439 cites W1967572107 @default.
• W2790733439 cites W1968588309 @default.
• W2790733439 cites W1971816180 @default.
• W2790733439 cites W1973046453 @default.
• W2790733439 cites W1977902163 @default.
• W2790733439 cites W1981309347 @default.
• W2790733439 cites W1985575284 @default.
• W2790733439 cites W1986623813 @default.
• W2790733439 cites W1989568493 @default.
• W2790733439 cites W1994299916 @default.
• W2790733439 cites W1998639331 @default.
• W2790733439 cites W2002077961 @default.
• W2790733439 cites W2008101666 @default.
• W2790733439 cites W2011654501 @default.
• W2790733439 cites W2018307575 @default.
• W2790733439 cites W2028119033 @default.
• W2790733439 cites W2033443586 @default.
• W2790733439 cites W2034389451 @default.
• W2790733439 cites W2034989643 @default.
• W2790733439 cites W2041784109 @default.
• W2790733439 cites W2045497835 @default.
• W2790733439 cites W2048437887 @default.
• W2790733439 cites W2051652831 @default.
• W2790733439 cites W2063151544 @default.
• W2790733439 cites W2064821698 @default.
• W2790733439 cites W2065465833 @default.
• W2790733439 cites W2067434913 @default.
• W2790733439 cites W2076597914 @default.
• W2790733439 cites W2079354040 @default.
• W2790733439 cites W2081802593 @default.
• W2790733439 cites W2089819985 @default.
• W2790733439 cites W2097650396 @default.
• W2790733439 cites W2099149056 @default.
• W2790733439 cites W2101337753 @default.
• W2790733439 cites W2105178645 @default.
• W2790733439 cites W2112914804 @default.
• W2790733439 cites W2118075348 @default.
• W2790733439 cites W2125032954 @default.
• W2790733439 cites W2143147471 @default.
• W2790733439 cites W2150087475 @default.
• W2790733439 cites W2155645894 @default.
• W2790733439 cites W2156765302 @default.
• W2790733439 cites W2158914796 @default.
• W2790733439 cites W2163794040 @default.
• W2790733439 cites W2165953847 @default.
• W2790733439 cites W2170151876 @default.
• W2790733439 cites W2293299816 @default.
• W2790733439 cites W2294326086 @default.
• W2790733439 cites W2318482076 @default.
• W2790733439 cites W2319751507 @default.
• W2790733439 cites W2322200390 @default.
• W2790733439 cites W2328776012 @default.
• W2790733439 cites W2340650602 @default.
• W2790733439 cites W2587171877 @default.
• W2790733439 cites W2787250335 @default.
• W2790733439 cites W2787691836 @default.
• W2790733439 cites W4235536609 @default.
• W2790733439 doi "https://doi.org/10.1086/697248" @default.
• W2790733439 hasPublicationYear "2018" @default.
• W2790733439 type Work @default.
• W2790733439 sameAs 2790733439 @default.
• W2790733439 citedByCount "7" @default.
• W2790733439 countsByYear W27907334392019 @default.
• W2790733439 countsByYear W27907334392020 @default.
• W2790733439 countsByYear W27907334392021 @default.
• W2790733439 countsByYear W27907334392022 @default.
• W2790733439 countsByYear W27907334392023 @default.
• W2790733439 crossrefType "journal-article" @default.
• W2790733439 hasAuthorship W2790733439A5041545020 @default.
• W2790733439 hasAuthorship W2790733439A5055270180 @default.
• W2790733439 hasAuthorship W2790733439A5067293477 @default.
• W2790733439 hasAuthorship W2790733439A5067447916 @default.
• W2790733439 hasAuthorship W2790733439A5083211055 @default.
• W2790733439 hasConcept C100834320 @default.
• W2790733439 hasConcept C111368507 @default.
• W2790733439 hasConcept C114793014 @default.
• W2790733439 hasConcept C127313418 @default.
• W2790733439 hasConcept C132651083 @default.
• W2790733439 hasConcept C138170599 @default.
• W2790733439 hasConcept C151730666 @default.
• W2790733439 hasConcept C15785411 @default.
• W2790733439 hasConcept C17409809 @default.
• W2790733439 hasConcept C185515318 @default.
• W2790733439 hasConcept C205325660 @default.
• W2790733439 hasConcept C33683781 @default.

• next