FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1978963419> ?p ?o ?g. }

• W1978963419 endingPage "159" @default.
• W1978963419 startingPage "139" @default.
• W1978963419 abstract "On the South Island of New Zealand, large piedmont glaciers descended from an ice cap on the Southern Alps onto the coastal plain of the West Coast during the late Pleistocene. The series of moraine belts and outwash plains left by the Taramakau glacier are used as a type section for interpreting the glacial geology and timing of major climatic events of New Zealand and also as a benchmark for comparison with the wider Southern Hemisphere. In this paper we review the chronology of advances by the Taramakau glacier during the last or Otira Glaciation using a combination of exposure dating using the cosmogenic nuclides 10Be and 36Cl, and tephrochronology. We document three distinct glacial maxima, represented by the Loopline, Larrikins and Moana Formations, separated by brief interstadials. We find that the Loopline Formation, originally attributed to Oxygen Isotope Chronozone 4, is much younger than previously thought, with an advance culminating around 24,900 ± 800 yr. The widespread late Pleistocene Kawakawa/Oruanui tephra stratigraphically lies immediately above it. This Formation has the same age previously attributed to the older part of the Larrikins Formation. Dating of the Larrikins Formation demonstrates there is no longer a basis for subdividing it into older and younger phases with an advance lasting about 1000 years between 20,800 ± 500 to 20,000 ± 400 yr. The Moana Formation represents the deposits of the last major advance of ice at 17,300 ± 500 yr and is younger than expected based on limited previous dating. The timing of major piedmont glaciation is restricted to between ∼25,000 and 17,000 yr and this interval corresponds to a time of regionally cold sea surface temperatures, expansion of grasslands at the expense of forest on South Island, and hemisphere wide glaciation." @default.
• W1978963419 created "2016-06-24" @default.
• W1978963419 creator A5007276196 @default.
• W1978963419 creator A5020295528 @default.
• W1978963419 creator A5020825692 @default.
• W1978963419 creator A5025431194 @default.
• W1978963419 creator A5071973994 @default.
• W1978963419 creator A5090269401 @default.
• W1978963419 date "2013-08-01" @default.
• W1978963419 modified "2023-10-14" @default.
• W1978963419 title "Late Pleistocene glacial stratigraphy of the Kumara-Moana region, West Coast of South Island, New Zealand" @default.
• W1978963419 cites W1927648166 @default.
• W1978963419 cites W195978946 @default.
• W1978963419 cites W1964602602 @default.
• W1978963419 cites W1965271222 @default.
• W1978963419 cites W1971568488 @default.
• W1978963419 cites W1972152903 @default.
• W1978963419 cites W1972930666 @default.
• W1978963419 cites W1975197770 @default.
• W1978963419 cites W1978308271 @default.
• W1978963419 cites W1978688609 @default.
• W1978963419 cites W1981464461 @default.
• W1978963419 cites W1987470663 @default.
• W1978963419 cites W1989570428 @default.
• W1978963419 cites W1992017740 @default.
• W1978963419 cites W1993783057 @default.
• W1978963419 cites W1994937022 @default.
• W1978963419 cites W1998298985 @default.
• W1978963419 cites W2000163063 @default.
• W1978963419 cites W2002473398 @default.
• W1978963419 cites W2005035365 @default.
• W1978963419 cites W2007539566 @default.
• W1978963419 cites W2007711314 @default.
• W1978963419 cites W2008290113 @default.
• W1978963419 cites W2009425598 @default.
• W1978963419 cites W2009575187 @default.
• W1978963419 cites W2017192340 @default.
• W1978963419 cites W2020669175 @default.
• W1978963419 cites W2023171383 @default.
• W1978963419 cites W2023401494 @default.
• W1978963419 cites W2035232595 @default.
• W1978963419 cites W2038265449 @default.
• W1978963419 cites W2041139567 @default.
• W1978963419 cites W2046804646 @default.
• W1978963419 cites W2048690726 @default.
• W1978963419 cites W2051603321 @default.
• W1978963419 cites W2055278228 @default.
• W1978963419 cites W2058199405 @default.
• W1978963419 cites W2061362847 @default.
• W1978963419 cites W2063155650 @default.
• W1978963419 cites W2063968713 @default.
• W1978963419 cites W2073473784 @default.
• W1978963419 cites W2073560038 @default.
• W1978963419 cites W2073715293 @default.
• W1978963419 cites W2076850342 @default.
• W1978963419 cites W2077230584 @default.
• W1978963419 cites W2078968364 @default.
• W1978963419 cites W2083418348 @default.
• W1978963419 cites W2086069100 @default.
• W1978963419 cites W2086697318 @default.
• W1978963419 cites W2092287133 @default.
• W1978963419 cites W2093330894 @default.
• W1978963419 cites W2104520911 @default.
• W1978963419 cites W2109459276 @default.
• W1978963419 cites W2117102444 @default.
• W1978963419 cites W2118684289 @default.
• W1978963419 cites W2119668780 @default.
• W1978963419 cites W2119721964 @default.
• W1978963419 cites W2131657919 @default.
• W1978963419 cites W2135883392 @default.
• W1978963419 cites W2136768862 @default.
• W1978963419 cites W2142727589 @default.
• W1978963419 cites W2154877554 @default.
• W1978963419 cites W2156226247 @default.
• W1978963419 cites W2159857285 @default.
• W1978963419 cites W2168925255 @default.
• W1978963419 cites W4211135859 @default.
• W1978963419 cites W4231051005 @default.
• W1978963419 cites W4248546378 @default.
• W1978963419 doi "https://doi.org/10.1016/j.quascirev.2013.04.010" @default.
• W1978963419 hasPublicationYear "2013" @default.
• W1978963419 type Work @default.
• W1978963419 sameAs 1978963419 @default.
• W1978963419 citedByCount "35" @default.
• W1978963419 countsByYear W19789634192013 @default.
• W1978963419 countsByYear W19789634192014 @default.
• W1978963419 countsByYear W19789634192015 @default.
• W1978963419 countsByYear W19789634192016 @default.
• W1978963419 countsByYear W19789634192017 @default.
• W1978963419 countsByYear W19789634192018 @default.
• W1978963419 countsByYear W19789634192019 @default.
• W1978963419 countsByYear W19789634192020 @default.
• W1978963419 countsByYear W19789634192021 @default.
• W1978963419 countsByYear W19789634192022 @default.
• W1978963419 countsByYear W19789634192023 @default.
• W1978963419 crossrefType "journal-article" @default.
• W1978963419 hasAuthorship W1978963419A5007276196 @default.
• W1978963419 hasAuthorship W1978963419A5020295528 @default.

• next