FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2040278045> ?p ?o ?g. }

• W2040278045 endingPage "159" @default.
• W2040278045 startingPage "148" @default.
• W2040278045 abstract "The mid-Cretaceous serves as an excellent laboratory for testing the dynamics of the climate under greenhouse state of the Earth. This study is focused on the cyclicity record of foraminiferal assemblages in the Lower Saxony Basin during the Middle Albian. The short eccentricity, obliquity, and precession cycles are consistently recorded in absolute and relative abundance of most opportunistic benthic and planktic foraminifers. The question is why foraminifers reacted to orbital cycles and what they actually record in the “equable” global climate. It is suggested that seasonality changes modulated by orbital cycles are responsible for the Milankovitch cyclicity records. It is well known that the axial obliquity directly influences seasonal contrasts in mid- and high latitudes. The precession modulated by the eccentricity of the Earth orbit further affects the contrast of seasons. Therefore, seasonal dynamics of precipitation/runoff and storm tracks patterns, and to a lesser extent temperature contrasts, are most likely factors controlling Milankovitch-scale cyclic fluctuations of foraminiferal assemblages and other proxies sensitive to productivity changes. It can be deduced that periods of the highest seasonal contrasts were dominated by opportunistic, abundant taxa, such as benthic Valvulineria–Gyroidinoides group and planktic hedbergellids, which record the strongest obliquity signals. The Lower Saxony and adjacent Boreal basins were possibly controlled by humid climate with relatively dry summers and wet winter seasons. This study confronted with the presented conceptual model and former climate models supports the conclusion that the temperate zone surrounding Tethys was sensitive to seasonal changes modulated by orbital cyclicity. The mid-latitudinal climate of the greenhouse Earth seems to be more dynamic and more seasonal than expected." @default.
• W2040278045 created "2016-06-24" @default.
• W2040278045 creator A5024065306 @default.
• W2040278045 date "2009-05-01" @default.
• W2040278045 modified "2023-10-05" @default.
• W2040278045 title "Foraminiferal response to seasonality modulated by orbital cycles in the Cretaceous mid-latitudes: The Albian record from the Lower Saxony Basin" @default.
• W2040278045 cites W1963526089 @default.
• W2040278045 cites W1966771540 @default.
• W2040278045 cites W1966990542 @default.
• W2040278045 cites W1967969727 @default.
• W2040278045 cites W1968915767 @default.
• W2040278045 cites W1969111769 @default.
• W2040278045 cites W1972168971 @default.
• W2040278045 cites W1978761019 @default.
• W2040278045 cites W1979251481 @default.
• W2040278045 cites W1979466042 @default.
• W2040278045 cites W1980743781 @default.
• W2040278045 cites W1984322081 @default.
• W2040278045 cites W1985294064 @default.
• W2040278045 cites W1989031124 @default.
• W2040278045 cites W1993740103 @default.
• W2040278045 cites W2007188189 @default.
• W2040278045 cites W2011776591 @default.
• W2040278045 cites W2014517632 @default.
• W2040278045 cites W2017075543 @default.
• W2040278045 cites W2017255556 @default.
• W2040278045 cites W2020324637 @default.
• W2040278045 cites W2029129723 @default.
• W2040278045 cites W2036239253 @default.
• W2040278045 cites W2044863472 @default.
• W2040278045 cites W2048888468 @default.
• W2040278045 cites W2049636003 @default.
• W2040278045 cites W2051573661 @default.
• W2040278045 cites W2052324726 @default.
• W2040278045 cites W2053792822 @default.
• W2040278045 cites W2054234673 @default.
• W2040278045 cites W2064212328 @default.
• W2040278045 cites W2065067233 @default.
• W2040278045 cites W2072602454 @default.
• W2040278045 cites W2079257506 @default.
• W2040278045 cites W2083309408 @default.
• W2040278045 cites W2086254897 @default.
• W2040278045 cites W2088149005 @default.
• W2040278045 cites W2091721562 @default.
• W2040278045 cites W2105260260 @default.
• W2040278045 cites W2120321494 @default.
• W2040278045 cites W2120805501 @default.
• W2040278045 cites W2130125993 @default.
• W2040278045 cites W2131100035 @default.
• W2040278045 cites W2132115359 @default.
• W2040278045 cites W2141614982 @default.
• W2040278045 cites W2142856217 @default.
• W2040278045 cites W2606715276 @default.
• W2040278045 cites W4256313693 @default.
• W2040278045 doi "https://doi.org/10.1016/j.palaeo.2009.03.006" @default.
• W2040278045 hasPublicationYear "2009" @default.
• W2040278045 type Work @default.
• W2040278045 sameAs 2040278045 @default.
• W2040278045 citedByCount "17" @default.
• W2040278045 countsByYear W20402780452013 @default.
• W2040278045 countsByYear W20402780452014 @default.
• W2040278045 countsByYear W20402780452015 @default.
• W2040278045 countsByYear W20402780452017 @default.
• W2040278045 countsByYear W20402780452018 @default.
• W2040278045 countsByYear W20402780452020 @default.
• W2040278045 countsByYear W20402780452021 @default.
• W2040278045 countsByYear W20402780452023 @default.
• W2040278045 crossrefType "journal-article" @default.
• W2040278045 hasAuthorship W2040278045A5024065306 @default.
• W2040278045 hasConcept C100537666 @default.
• W2040278045 hasConcept C109007969 @default.
• W2040278045 hasConcept C111368507 @default.
• W2040278045 hasConcept C114990195 @default.
• W2040278045 hasConcept C115343472 @default.
• W2040278045 hasConcept C121332964 @default.
• W2040278045 hasConcept C122523270 @default.
• W2040278045 hasConcept C12294951 @default.
• W2040278045 hasConcept C125311221 @default.
• W2040278045 hasConcept C125403950 @default.
• W2040278045 hasConcept C127313418 @default.
• W2040278045 hasConcept C1276947 @default.
• W2040278045 hasConcept C132651083 @default.
• W2040278045 hasConcept C13280743 @default.
• W2040278045 hasConcept C150846664 @default.
• W2040278045 hasConcept C151730666 @default.
• W2040278045 hasConcept C15739521 @default.
• W2040278045 hasConcept C178100555 @default.
• W2040278045 hasConcept C18903297 @default.
• W2040278045 hasConcept C30860409 @default.
• W2040278045 hasConcept C33683781 @default.
• W2040278045 hasConcept C49204034 @default.
• W2040278045 hasConcept C55173820 @default.
• W2040278045 hasConcept C81461190 @default.
• W2040278045 hasConcept C81502235 @default.
• W2040278045 hasConcept C83042747 @default.
• W2040278045 hasConcept C86803240 @default.
• W2040278045 hasConceptScore W2040278045C100537666 @default.
• W2040278045 hasConceptScore W2040278045C109007969 @default.

• next