FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2904105811> ?p ?o ?g. }

• W2904105811 endingPage "51" @default.
• W2904105811 startingPage "44" @default.
• W2904105811 abstract "The climate conditions during Marine Isotope Stage (MIS) 3 were similar to present-day conditions, but whether humidity then exceeded present levels is debated, and the driving mechanisms of palaeoclimate evolution since MIS 3 remain unclear. Here, we use pollen data from Wulagai Lake, Inner Mongolia, to reconstruct vegetation and climate changes since the middle MIS 3. The steppe biome is reconstructed as the first dominant biome and the desert biome as the second, and the results show that the vegetation was steppe over the last 43,800 years. Poaceae, Artemisia, Caryophyllaceae and Humulus were abundant from middle to late MIS 3, indicating humid climate conditions. As drought-tolerant species such as Hippophae, Nitraria and Chenopodiaceae spread during MIS 2, the climate became arid. The Holocene is characterized by the dominance of steppe with mixed coniferous-broadleaved forests in the Greater Hinggan Range, and the desert biome retains high affinity scores, indicating that the climate was semi-arid. The climate from middle to late MIS 3 was wetter than in the Holocene; this shift was related to changes in the Northern Hemisphere's solar insolation and ice volume. The humid conditions during MIS 3 were attributed to strong ice–albedo feedback, which led to evaporation that was less than the precipitation. The enhanced evaporation caused by increased solar insolation and decreased ice volume might have exceeded the precipitation during the Holocene and resulted in low effective humidity in the Wulagai Lake basin." @default.
• W2904105811 created "2018-12-22" @default.
• W2904105811 creator A5066102428 @default.
• W2904105811 creator A5067436536 @default.
• W2904105811 creator A5069229762 @default.
• W2904105811 creator A5077575953 @default.
• W2904105811 creator A5085075467 @default.
• W2904105811 creator A5090005540 @default.
• W2904105811 date "2019-03-01" @default.
• W2904105811 modified "2023-09-27" @default.
• W2904105811 title "Vegetation and climate changes since the middle MIS 3 inferred from a Wulagai Lake pollen record, Inner Mongolia, Northeastern China" @default.
• W2904105811 cites W1224479729 @default.
• W2904105811 cites W132956249 @default.
• W2904105811 cites W1965358009 @default.
• W2904105811 cites W1967314489 @default.
• W2904105811 cites W1972587755 @default.
• W2904105811 cites W1982071821 @default.
• W2904105811 cites W1994007098 @default.
• W2904105811 cites W1994758570 @default.
• W2904105811 cites W1995083616 @default.
• W2904105811 cites W1995713342 @default.
• W2904105811 cites W2000655296 @default.
• W2904105811 cites W2013848216 @default.
• W2904105811 cites W2013878295 @default.
• W2904105811 cites W2018870464 @default.
• W2904105811 cites W2027175220 @default.
• W2904105811 cites W2027187464 @default.
• W2904105811 cites W2028689071 @default.
• W2904105811 cites W2028695454 @default.
• W2904105811 cites W2033075721 @default.
• W2904105811 cites W2040399010 @default.
• W2904105811 cites W2042501609 @default.
• W2904105811 cites W2050684125 @default.
• W2904105811 cites W2052087726 @default.
• W2904105811 cites W2054338044 @default.
• W2904105811 cites W2055792591 @default.
• W2904105811 cites W2058530169 @default.
• W2904105811 cites W2072450543 @default.
• W2904105811 cites W2076592609 @default.
• W2904105811 cites W2086192317 @default.
• W2904105811 cites W2089832886 @default.
• W2904105811 cites W2094168188 @default.
• W2904105811 cites W2094347870 @default.
• W2904105811 cites W2096165408 @default.
• W2904105811 cites W2096484028 @default.
• W2904105811 cites W2099358694 @default.
• W2904105811 cites W2106814658 @default.
• W2904105811 cites W2124637748 @default.
• W2904105811 cites W2125600063 @default.
• W2904105811 cites W2141459972 @default.
• W2904105811 cites W2141625253 @default.
• W2904105811 cites W2149010791 @default.
• W2904105811 cites W2150037729 @default.
• W2904105811 cites W2155706641 @default.
• W2904105811 cites W2182526330 @default.
• W2904105811 cites W2266279946 @default.
• W2904105811 cites W2393883870 @default.
• W2904105811 cites W2475704307 @default.
• W2904105811 cites W2558782821 @default.
• W2904105811 cites W2606572456 @default.
• W2904105811 cites W2766933213 @default.
• W2904105811 cites W2776319111 @default.
• W2904105811 cites W2799395054 @default.
• W2904105811 cites W4237866035 @default.
• W2904105811 cites W4246027503 @default.
• W2904105811 cites W759036854 @default.
• W2904105811 doi "https://doi.org/10.1016/j.revpalbo.2018.12.006" @default.
• W2904105811 hasPublicationYear "2019" @default.
• W2904105811 type Work @default.
• W2904105811 sameAs 2904105811 @default.
• W2904105811 citedByCount "10" @default.
• W2904105811 countsByYear W29041058112019 @default.
• W2904105811 countsByYear W29041058112020 @default.
• W2904105811 countsByYear W29041058112021 @default.
• W2904105811 countsByYear W29041058112022 @default.
• W2904105811 countsByYear W29041058112023 @default.
• W2904105811 crossrefType "journal-article" @default.
• W2904105811 hasAuthorship W2904105811A5066102428 @default.
• W2904105811 hasAuthorship W2904105811A5067436536 @default.
• W2904105811 hasAuthorship W2904105811A5069229762 @default.
• W2904105811 hasAuthorship W2904105811A5077575953 @default.
• W2904105811 hasAuthorship W2904105811A5085075467 @default.
• W2904105811 hasAuthorship W2904105811A5090005540 @default.
• W2904105811 hasConcept C100970517 @default.
• W2904105811 hasConcept C105895522 @default.
• W2904105811 hasConcept C107054158 @default.
• W2904105811 hasConcept C110872660 @default.
• W2904105811 hasConcept C111368507 @default.
• W2904105811 hasConcept C127313418 @default.
• W2904105811 hasConcept C132651083 @default.
• W2904105811 hasConcept C140345934 @default.
• W2904105811 hasConcept C142724271 @default.
• W2904105811 hasConcept C150772632 @default.
• W2904105811 hasConcept C153294291 @default.
• W2904105811 hasConcept C18903297 @default.
• W2904105811 hasConcept C205649164 @default.
• W2904105811 hasConcept C2776133958 @default.
• W2904105811 hasConcept C2776289648 @default.

• next