FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2791973436> ?p ?o ?g. }

• W2791973436 endingPage "319" @default.
• W2791973436 startingPage "303" @default.
• W2791973436 abstract "Abstract. A consistent chronostratigraphic framework is required to understand the effect of major paleoclimate perturbations on both marine and terrestrial ecosystems. Transient global warming events in the early Eocene, at 56–54 Ma, show the impact of large-scale carbon input into the ocean–atmosphere system. Here we provide the first timescale synchronization of continental and marine deposits spanning the Paleocene–Eocene Thermal Maximum (PETM) and the interval just prior to the Eocene Thermal Maximum 2 (ETM-2). Cyclic variations in geochemical data come from continental drill cores of the Bighorn Basin Coring Project (BBCP, Wyoming, USA) and from marine deep-sea drilling deposits retrieved by the Ocean Drilling Program (ODP). Both are dominated by eccentricity-modulated precession cycles used to construct a common cyclostratigraphic framework. Integration of age models results in a revised astrochronology for the PETM in deep-sea records that is now generally consistent with independent 3He age models. The duration of the PETM is estimated at ∼ 200 kyr for the carbon isotope excursion and ∼ 120 kyr for the associated pelagic clay layer. A common terrestrial and marine age model shows a concurrent major change in marine and terrestrial biota ∼ 200 kyr before ETM-2. In the Bighorn Basin, the change is referred to as Biohorizon B and represents a period of significant mammalian turnover and immigration, separating the upper Haplomylus–Ectocion Range Zone from the Bunophorus Interval Zone and approximating the Wa-4–Wa-5 land mammal zone boundary. In sediments from ODP Site 1262 (Walvis Ridge), major changes in the biota at this time are documented by the radiation of a “second generation” of apical spine-bearing sphenolith species (e.g., S. radians and S. editus), the emergence of T. orthostylus, and the marked decline of D. multiradiatus." @default.
• W2791973436 created "2018-03-29" @default.
• W2791973436 creator A5005945864 @default.
• W2791973436 creator A5032109623 @default.
• W2791973436 creator A5035200956 @default.
• W2791973436 creator A5043879539 @default.
• W2791973436 creator A5059240559 @default.
• W2791973436 creator A5061736979 @default.
• W2791973436 creator A5069257605 @default.
• W2791973436 creator A5085483998 @default.
• W2791973436 date "2018-03-08" @default.
• W2791973436 modified "2023-10-17" @default.
• W2791973436 title "Synchronizing early Eocene deep-sea and continental records – cyclostratigraphic age models for the Bighorn Basin Coring Project drill cores" @default.
• W2791973436 cites W1482739399 @default.
• W2791973436 cites W1598314256 @default.
• W2791973436 cites W1819501304 @default.
• W2791973436 cites W1861805319 @default.
• W2791973436 cites W1862378376 @default.
• W2791973436 cites W1874262011 @default.
• W2791973436 cites W1877298222 @default.
• W2791973436 cites W1905640277 @default.
• W2791973436 cites W1964116684 @default.
• W2791973436 cites W1975632341 @default.
• W2791973436 cites W1976215537 @default.
• W2791973436 cites W1990578110 @default.
• W2791973436 cites W1996417990 @default.
• W2791973436 cites W2008377426 @default.
• W2791973436 cites W2008391360 @default.
• W2791973436 cites W2008880745 @default.
• W2791973436 cites W2015529439 @default.
• W2791973436 cites W2020712595 @default.
• W2791973436 cites W2026823059 @default.
• W2791973436 cites W2029120025 @default.
• W2791973436 cites W2032855124 @default.
• W2791973436 cites W2033052384 @default.
• W2791973436 cites W2072235428 @default.
• W2791973436 cites W2073378033 @default.
• W2791973436 cites W2078352383 @default.
• W2791973436 cites W2081274126 @default.
• W2791973436 cites W2089205895 @default.
• W2791973436 cites W2089561449 @default.
• W2791973436 cites W2098896322 @default.
• W2791973436 cites W2099179162 @default.
• W2791973436 cites W2101372386 @default.
• W2791973436 cites W2110233655 @default.
• W2791973436 cites W2114332853 @default.
• W2791973436 cites W2117159119 @default.
• W2791973436 cites W2120595970 @default.
• W2791973436 cites W2126102606 @default.
• W2791973436 cites W2130957548 @default.
• W2791973436 cites W2131079535 @default.
• W2791973436 cites W2132448110 @default.
• W2791973436 cites W2138691699 @default.
• W2791973436 cites W2140477756 @default.
• W2791973436 cites W2152918533 @default.
• W2791973436 cites W2157438953 @default.
• W2791973436 cites W2215188800 @default.
• W2791973436 cites W2310649619 @default.
• W2791973436 cites W2349305435 @default.
• W2791973436 cites W2587456915 @default.
• W2791973436 cites W2598544278 @default.
• W2791973436 cites W2600591310 @default.
• W2791973436 cites W2730064841 @default.
• W2791973436 cites W4306293736 @default.
• W2791973436 doi "https://doi.org/10.5194/cp-14-303-2018" @default.
• W2791973436 hasPublicationYear "2018" @default.
• W2791973436 type Work @default.
• W2791973436 sameAs 2791973436 @default.
• W2791973436 citedByCount "34" @default.
• W2791973436 countsByYear W27919734362018 @default.
• W2791973436 countsByYear W27919734362019 @default.
• W2791973436 countsByYear W27919734362020 @default.
• W2791973436 countsByYear W27919734362021 @default.
• W2791973436 countsByYear W27919734362022 @default.
• W2791973436 countsByYear W27919734362023 @default.
• W2791973436 crossrefType "journal-article" @default.
• W2791973436 hasAuthorship W2791973436A5005945864 @default.
• W2791973436 hasAuthorship W2791973436A5032109623 @default.
• W2791973436 hasAuthorship W2791973436A5035200956 @default.
• W2791973436 hasAuthorship W2791973436A5043879539 @default.
• W2791973436 hasAuthorship W2791973436A5059240559 @default.
• W2791973436 hasAuthorship W2791973436A5061736979 @default.
• W2791973436 hasAuthorship W2791973436A5069257605 @default.
• W2791973436 hasAuthorship W2791973436A5085483998 @default.
• W2791973436 hasBestOaLocation W27919734361 @default.
• W2791973436 hasConcept C109007969 @default.
• W2791973436 hasConcept C111368507 @default.
• W2791973436 hasConcept C127313418 @default.
• W2791973436 hasConcept C127413603 @default.
• W2791973436 hasConcept C151730666 @default.
• W2791973436 hasConcept C15739521 @default.
• W2791973436 hasConcept C184751465 @default.
• W2791973436 hasConcept C186240526 @default.
• W2791973436 hasConcept C20364790 @default.
• W2791973436 hasConcept C25197100 @default.
• W2791973436 hasConcept C2780518792 @default.
• W2791973436 hasConcept C6385141 @default.
• W2791973436 hasConcept C78519656 @default.

• next