FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3033221037> ?p ?o ?g. }

• W3033221037 endingPage "109821" @default.
• W3033221037 startingPage "109821" @default.
• W3033221037 abstract "We evaluate whether outer shelf/upper slope settings preserve a record of astronomical forcing using gamma ray logs from the upper Oligocene (upper Chattian) Tikorangi Formation, onshore Taranaki Basin, North Island, New Zealand. The formation is a siliciclastic‑carbonate succession deposited in outer neritic to upper bathyal depths at paleolatitudes of c. 45oS. Gamma ray and sonic logs calibrated to core indicate four lithofacies based on percent carbonate. These are calcareous siliciclastic mudrock (highest gamma ray values), highly calcareous siltstones (high gamma ray values), very fine to fine siliciclastic muddy packstones (intermediate gamma), and winnowed very fine to medium grain-dominated packstones and grainstones (low gamma). Detrended gamma ray logs were tuned using minimal tuning methods (405 kyr long eccentricity cycle or, where this was poorly developed, the ~100 kyr short eccentricity cycle) with sedimentation rates tested statistically against astronomical forcing. The tuned data show well developed long- and short-term eccentricity, obliquity, and a weak precessional forcing. Obliquity modulation is observed at the 1.2 Myr scale (one well) and 175 kyr scale (two wells). The floating time scale was tied to the absolute time scale via published biostratigraphy, the La2004 eccentricity solution, the Atlantic ODP site 1264 δ18O record, and the Mi-1 isotope event at c.23 Ma. Sea-level fluctuations typically were moderate (20 to 40 m) estimated from the δ18O record. The high gamma siliciclastic-prone units formed during warmer and wetter phases (and possibly slightly higher sea levels), whereas the cleaner carbonates with abundant inner-shelf-derived fine carbonate developed during cooler, drier phases (and possibly slightly lower sea levels). Gamma ray logs from outer shelf/upper slope settings provide valuable data sets for documenting the effects of astronomical forcing on the sedimentary record. The study supports climate models for New Zealand which predict generally increased precipitation with warming over the next 100 years. The study appears to be the first to record astronomical forcing in the Oligocene marine record of New Zealand." @default.
• W3033221037 created "2020-06-12" @default.
• W3033221037 creator A5001753624 @default.
• W3033221037 creator A5009185493 @default.
• W3033221037 creator A5027374040 @default.
• W3033221037 creator A5035298412 @default.
• W3033221037 creator A5039271608 @default.
• W3033221037 date "2020-10-01" @default.
• W3033221037 modified "2023-10-17" @default.
• W3033221037 title "Testing for astronomical forcing of cycles and gamma ray signals in outer shelf/upper slope, mixed siliciclastic-carbonates: Upper Oligocene, New Zealand" @default.
• W3033221037 cites W1969160941 @default.
• W3033221037 cites W1972628868 @default.
• W3033221037 cites W1974628456 @default.
• W3033221037 cites W1978157185 @default.
• W3033221037 cites W1983657072 @default.
• W3033221037 cites W1985350839 @default.
• W3033221037 cites W1986138270 @default.
• W3033221037 cites W1995395219 @default.
• W3033221037 cites W1996952258 @default.
• W3033221037 cites W2007685092 @default.
• W3033221037 cites W2012180822 @default.
• W3033221037 cites W2017255149 @default.
• W3033221037 cites W2018958695 @default.
• W3033221037 cites W2022366414 @default.
• W3033221037 cites W2031018785 @default.
• W3033221037 cites W2033816018 @default.
• W3033221037 cites W2034868239 @default.
• W3033221037 cites W2047674868 @default.
• W3033221037 cites W2051315776 @default.
• W3033221037 cites W2054410655 @default.
• W3033221037 cites W2061161672 @default.
• W3033221037 cites W2065752436 @default.
• W3033221037 cites W2066834407 @default.
• W3033221037 cites W2075538259 @default.
• W3033221037 cites W2078275838 @default.
• W3033221037 cites W2086655067 @default.
• W3033221037 cites W2090999126 @default.
• W3033221037 cites W2115575384 @default.
• W3033221037 cites W2126150865 @default.
• W3033221037 cites W2133226116 @default.
• W3033221037 cites W2140137179 @default.
• W3033221037 cites W2140477756 @default.
• W3033221037 cites W2151368777 @default.
• W3033221037 cites W2155706641 @default.
• W3033221037 cites W2155724780 @default.
• W3033221037 cites W2170575926 @default.
• W3033221037 cites W2234931695 @default.
• W3033221037 cites W2270990278 @default.
• W3033221037 cites W2473855155 @default.
• W3033221037 cites W2730053617 @default.
• W3033221037 cites W2789494427 @default.
• W3033221037 cites W2802184660 @default.
• W3033221037 cites W2892225831 @default.
• W3033221037 cites W2903524071 @default.
• W3033221037 cites W2910702274 @default.
• W3033221037 cites W2918772958 @default.
• W3033221037 cites W4306293736 @default.
• W3033221037 doi "https://doi.org/10.1016/j.palaeo.2020.109821" @default.
• W3033221037 hasPublicationYear "2020" @default.
• W3033221037 type Work @default.
• W3033221037 sameAs 3033221037 @default.
• W3033221037 citedByCount "5" @default.
• W3033221037 countsByYear W30332210372022 @default.
• W3033221037 countsByYear W30332210372023 @default.
• W3033221037 crossrefType "journal-article" @default.
• W3033221037 hasAuthorship W3033221037A5001753624 @default.
• W3033221037 hasAuthorship W3033221037A5009185493 @default.
• W3033221037 hasAuthorship W3033221037A5027374040 @default.
• W3033221037 hasAuthorship W3033221037A5035298412 @default.
• W3033221037 hasAuthorship W3033221037A5039271608 @default.
• W3033221037 hasConcept C109007969 @default.
• W3033221037 hasConcept C127313418 @default.
• W3033221037 hasConcept C146588470 @default.
• W3033221037 hasConcept C151730666 @default.
• W3033221037 hasConcept C191897082 @default.
• W3033221037 hasConcept C192562407 @default.
• W3033221037 hasConcept C2780659211 @default.
• W3033221037 hasConcept C49015763 @default.
• W3033221037 hasConcept C93257316 @default.
• W3033221037 hasConceptScore W3033221037C109007969 @default.
• W3033221037 hasConceptScore W3033221037C127313418 @default.
• W3033221037 hasConceptScore W3033221037C146588470 @default.
• W3033221037 hasConceptScore W3033221037C151730666 @default.
• W3033221037 hasConceptScore W3033221037C191897082 @default.
• W3033221037 hasConceptScore W3033221037C192562407 @default.
• W3033221037 hasConceptScore W3033221037C2780659211 @default.
• W3033221037 hasConceptScore W3033221037C49015763 @default.
• W3033221037 hasConceptScore W3033221037C93257316 @default.
• W3033221037 hasLocation W30332210371 @default.
• W3033221037 hasOpenAccess W3033221037 @default.
• W3033221037 hasPrimaryLocation W30332210371 @default.
• W3033221037 hasRelatedWork W1497967409 @default.
• W3033221037 hasRelatedWork W2022766401 @default.
• W3033221037 hasRelatedWork W2049297378 @default.
• W3033221037 hasRelatedWork W2057210365 @default.
• W3033221037 hasRelatedWork W2079705210 @default.
• W3033221037 hasRelatedWork W2118995100 @default.
• W3033221037 hasRelatedWork W2182019131 @default.

• next