FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2068371799> ?p ?o ?g. }

• W2068371799 endingPage "658" @default.
• W2068371799 startingPage "644" @default.
• W2068371799 abstract "Abstract Aim Our aims were: (1) to use recently published phylogenies of six widely distributed clades of highland‐type fishes in a comparative analysis that investigates relationships among North American highlands; (2) to construct a map of relevant (pre‐historic) river geography; and (3) to apply ecological paradigms to interpret patterns of highland‐fish cladogenesis. Our principal questions were: (1) does highland endemism correspond to pre‐historic river drainages; and (2) do patterns of speciation conform to any relevant paradigm? Location Twenty‐two North American highlands, east to west from Appalachia to the Basin and Range, north to south from the Canadian Shield to the Mesa Central. Methods We used three‐item analysis to find shared highland‐area relationships, and we used dated phylogenies and geological literature to construct a map of relevant, pre‐historic river drainages. We applied the taxon‐cycle concept to interpret results. Results Three‐item analysis identified 375 most‐parsimonious trees with a retention index of 80.4%. An intersection tree reconstructed from shared three‐area statements had a completeness index of 80.3%. Nodes on the tree identified seven major branches of one to eight highland areas each that were congruent with late Miocene river drainage patterns. Sister‐area relationships within nodes were congruent with Plio‐Pleistocene events. Older taxa have restricted distributions and some younger members of each clade are broadly distributed, consistent with predictions of the taxon cycle. Main conclusions Progenitors of highland endemics were widespread across an aggraded, alluvial landscape by the early Miocene. Middle Miocene drainage rearrangements facilitated further range expansion. Accelerated erosion in the middle Miocene, caused by tectonic uplift and climate change, created highland‐type (sediment‐starved) habitats. Parallel colonization and adaptation to these habitats and geographical isolation in the late Miocene and early Pliocene led to speciation of highland endemics. Plio‐Pleistocene drainage rearrangements allowed populations of tolerant (derivative) taxa to expand again and colonize highland areas, including emerging ones." @default.
• W2068371799 created "2016-06-24" @default.
• W2068371799 creator A5026964686 @default.
• W2068371799 creator A5035124798 @default.
• W2068371799 creator A5072439286 @default.
• W2068371799 date "2013-12-17" @default.
• W2068371799 modified "2023-10-16" @default.
• W2068371799 title "Miocene rivers and taxon cycles clarify the comparative biogeography of North American highland fishes" @default.
• W2068371799 cites W1495179065 @default.
• W2068371799 cites W1642974483 @default.
• W2068371799 cites W181718397 @default.
• W2068371799 cites W185072987 @default.
• W2068371799 cites W1882773626 @default.
• W2068371799 cites W1912887918 @default.
• W2068371799 cites W1915177094 @default.
• W2068371799 cites W1934939404 @default.
• W2068371799 cites W1964427340 @default.
• W2068371799 cites W1964958587 @default.
• W2068371799 cites W1965476074 @default.
• W2068371799 cites W1969119266 @default.
• W2068371799 cites W1969383041 @default.
• W2068371799 cites W1971225852 @default.
• W2068371799 cites W1971265456 @default.
• W2068371799 cites W1974090808 @default.
• W2068371799 cites W1975709047 @default.
• W2068371799 cites W1976894260 @default.
• W2068371799 cites W1977191667 @default.
• W2068371799 cites W1984933097 @default.
• W2068371799 cites W1985331092 @default.
• W2068371799 cites W1992082466 @default.
• W2068371799 cites W1995593798 @default.
• W2068371799 cites W2000568635 @default.
• W2068371799 cites W2003044517 @default.
• W2068371799 cites W2004131007 @default.
• W2068371799 cites W2005256852 @default.
• W2068371799 cites W2009721882 @default.
• W2068371799 cites W2013942337 @default.
• W2068371799 cites W2014273112 @default.
• W2068371799 cites W2015734380 @default.
• W2068371799 cites W2018410592 @default.
• W2068371799 cites W2019632054 @default.
• W2068371799 cites W2021800930 @default.
• W2068371799 cites W2022695947 @default.
• W2068371799 cites W2028477745 @default.
• W2068371799 cites W2030867945 @default.
• W2068371799 cites W2035622691 @default.
• W2068371799 cites W2036631110 @default.
• W2068371799 cites W2038772350 @default.
• W2068371799 cites W2041941946 @default.
• W2068371799 cites W2044723675 @default.
• W2068371799 cites W2049743598 @default.
• W2068371799 cites W2050254711 @default.
• W2068371799 cites W2050566362 @default.
• W2068371799 cites W2050786803 @default.
• W2068371799 cites W2053452757 @default.
• W2068371799 cites W2059211290 @default.
• W2068371799 cites W2059218387 @default.
• W2068371799 cites W2061551074 @default.
• W2068371799 cites W2062889538 @default.
• W2068371799 cites W2065234515 @default.
• W2068371799 cites W2066240087 @default.
• W2068371799 cites W2066299694 @default.
• W2068371799 cites W2069060448 @default.
• W2068371799 cites W2075118059 @default.
• W2068371799 cites W2076776804 @default.
• W2068371799 cites W2088751485 @default.
• W2068371799 cites W2093081919 @default.
• W2068371799 cites W2096887404 @default.
• W2068371799 cites W2097059816 @default.
• W2068371799 cites W2097669784 @default.
• W2068371799 cites W2105342560 @default.
• W2068371799 cites W2108977935 @default.
• W2068371799 cites W2112457648 @default.
• W2068371799 cites W2113850264 @default.
• W2068371799 cites W2114823514 @default.
• W2068371799 cites W2117384519 @default.
• W2068371799 cites W2117786574 @default.
• W2068371799 cites W2118283339 @default.
• W2068371799 cites W2118785714 @default.
• W2068371799 cites W2127403458 @default.
• W2068371799 cites W2130730391 @default.
• W2068371799 cites W2133539117 @default.
• W2068371799 cites W2136109027 @default.
• W2068371799 cites W2148994456 @default.
• W2068371799 cites W2149930359 @default.
• W2068371799 cites W2151106402 @default.
• W2068371799 cites W2155880045 @default.
• W2068371799 cites W2157463139 @default.
• W2068371799 cites W2158009709 @default.
• W2068371799 cites W2161163117 @default.
• W2068371799 cites W2161863815 @default.
• W2068371799 cites W2169061517 @default.
• W2068371799 cites W2170505236 @default.
• W2068371799 cites W2170739632 @default.
• W2068371799 cites W2172552196 @default.
• W2068371799 cites W2173860918 @default.
• W2068371799 cites W2174444320 @default.
• W2068371799 cites W2177232905 @default.

• next