Matches in SemOpenAlex for { <https://semopenalex.org/work/W2016670503> ?p ?o ?g. }
- W2016670503 endingPage "20" @default.
- W2016670503 startingPage "10" @default.
- W2016670503 abstract "This study explores the response of the Irano-Turanian flora to Quaternary glacial–interglacial cycles in SW Asia. We use new fossil pollen data to assess variation in abundance of Cousinia Cass. (Compositae), a large genus typical for the Irano-Turanian flora, during these cycles. The results are compared with modern topography, tectonic and palaeoclimatic history, and recent phylogenetic data to explain the extremely high speciation rate and level of endemism as well as the modern geographical distribution of the genus. Cousinia is consistently well-represented in glacial-age and late-glacial pollen assemblages of NW Iran and E Anatolia. In the ~ 200,000-year pollen sequence from Lake Urmia, NW Iran, Cousinia pollen shows significant values and is nearly continuously represented during both the last glacial (~ 70 ka to Holocene) and penultimate glacial periods (~ 190 to 130 ka). In contrast, its pollen is less frequent and occurs only sporadically during the last interglacial period and the Holocene. This pattern suggests that Cousinia could not only withstand Quaternary glaciations, but was a significant part of the glacial-age landscapes of the Irano-Turanian territory. We argue that the extremely high rate of speciation and endemism of Cousinia is due to (i) the continuous presence of a complex topography in the Middle East and Central Asia since Tertiary times, which created a wide range of environmental niches and facilitated the formation and persistence of isolated populations over long periods, (ii) relatively stable climate during the late Miocene–Pliocene compared to the Quaternary period that caused small species range shifts and gene flow, and (iii) a dampened impact of multiple glacial–interglacial cycles on the mountain regions of SW Asia compared to the higher latitude European mountain ranges. This left an extensive, non-glaciated altitudinal zone for the survival of Irano-Turanian species, thereby reducing extinction during glacial periods. During interglacial periods, many Cousinia species may have been geographically isolated in high mountain “interglacial refugia” of the Irano-Turanian region. Overall, the combination of the above factors during the Neogene resulted in geographical isolation and reduced gene flow, thereby fostering allopatric speciation in Cousinia and probably also in many other speciose Irano-Turanian plant taxa." @default.
- W2016670503 created "2016-06-24" @default.
- W2016670503 creator A5002550939 @default.
- W2016670503 creator A5019614873 @default.
- W2016670503 creator A5029947319 @default.
- W2016670503 creator A5035266385 @default.
- W2016670503 creator A5042137666 @default.
- W2016670503 creator A5051122091 @default.
- W2016670503 creator A5067431267 @default.
- W2016670503 creator A5071248765 @default.
- W2016670503 creator A5075016951 @default.
- W2016670503 date "2012-02-01" @default.
- W2016670503 modified "2023-09-30" @default.
- W2016670503 title "Ecological implications of Cousinia Cass. (Asteraceae) persistence through the last two glacial–interglacial cycles in the continental Middle East for the Irano-Turanian flora" @default.
- W2016670503 cites W147933922 @default.
- W2016670503 cites W1491976738 @default.
- W2016670503 cites W1610721733 @default.
- W2016670503 cites W1912585888 @default.
- W2016670503 cites W195821846 @default.
- W2016670503 cites W1965092199 @default.
- W2016670503 cites W1968425238 @default.
- W2016670503 cites W1968920596 @default.
- W2016670503 cites W1978776740 @default.
- W2016670503 cites W1979407478 @default.
- W2016670503 cites W1982171979 @default.
- W2016670503 cites W1982737118 @default.
- W2016670503 cites W1998917135 @default.
- W2016670503 cites W1999850088 @default.
- W2016670503 cites W2003433968 @default.
- W2016670503 cites W2007740340 @default.
- W2016670503 cites W2009148751 @default.
- W2016670503 cites W2026903476 @default.
- W2016670503 cites W2027287476 @default.
- W2016670503 cites W2028277640 @default.
- W2016670503 cites W2038947148 @default.
- W2016670503 cites W2043339008 @default.
- W2016670503 cites W2044048829 @default.
- W2016670503 cites W2045366837 @default.
- W2016670503 cites W2045594539 @default.
- W2016670503 cites W2053151969 @default.
- W2016670503 cites W2054340203 @default.
- W2016670503 cites W2056191994 @default.
- W2016670503 cites W2059474755 @default.
- W2016670503 cites W2061296005 @default.
- W2016670503 cites W2064442820 @default.
- W2016670503 cites W2064880246 @default.
- W2016670503 cites W2065491911 @default.
- W2016670503 cites W2066069078 @default.
- W2016670503 cites W2068474779 @default.
- W2016670503 cites W2069813348 @default.
- W2016670503 cites W2073132125 @default.
- W2016670503 cites W2079845229 @default.
- W2016670503 cites W2084502571 @default.
- W2016670503 cites W2089056038 @default.
- W2016670503 cites W2089462565 @default.
- W2016670503 cites W2091023995 @default.
- W2016670503 cites W2094903970 @default.
- W2016670503 cites W2095941838 @default.
- W2016670503 cites W2096601245 @default.
- W2016670503 cites W2097179538 @default.
- W2016670503 cites W2097706604 @default.
- W2016670503 cites W2101999386 @default.
- W2016670503 cites W2107121737 @default.
- W2016670503 cites W2112184907 @default.
- W2016670503 cites W2114605016 @default.
- W2016670503 cites W2115575384 @default.
- W2016670503 cites W2120348339 @default.
- W2016670503 cites W2120745711 @default.
- W2016670503 cites W2123575603 @default.
- W2016670503 cites W2124631232 @default.
- W2016670503 cites W2131924853 @default.
- W2016670503 cites W2133935355 @default.
- W2016670503 cites W2136419158 @default.
- W2016670503 cites W2139686227 @default.
- W2016670503 cites W2140308583 @default.
- W2016670503 cites W2141023161 @default.
- W2016670503 cites W2144392862 @default.
- W2016670503 cites W2148958850 @default.
- W2016670503 cites W2151047196 @default.
- W2016670503 cites W2151072068 @default.
- W2016670503 cites W2159082182 @default.
- W2016670503 cites W2160283423 @default.
- W2016670503 cites W2172603263 @default.
- W2016670503 cites W2315765270 @default.
- W2016670503 cites W2319754122 @default.
- W2016670503 cites W2344346796 @default.
- W2016670503 cites W254970029 @default.
- W2016670503 cites W269331071 @default.
- W2016670503 cites W4211061961 @default.
- W2016670503 cites W4229554031 @default.
- W2016670503 cites W4242118851 @default.
- W2016670503 cites W4256478848 @default.
- W2016670503 doi "https://doi.org/10.1016/j.revpalbo.2012.01.005" @default.
- W2016670503 hasPublicationYear "2012" @default.
- W2016670503 type Work @default.
- W2016670503 sameAs 2016670503 @default.
- W2016670503 citedByCount "68" @default.
- W2016670503 countsByYear W20166705032012 @default.