2009
DOI: 10.1111/j.1365-2699.2008.02057.x
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Geohistorical and current environmental influences on floristic differentiation in the Ryukyu Archipelago, Japan

Abstract: Aim Floristic differentiation in the Ryukyu Archipelago has been explained primarily by geohistory, specifically landbridge formation and vicariance at the Tokara and Kerama Gaps, two deep-sea channels through the island arc. This ignores current environmental effects, which may also be important. We therefore tested whether the floristic differentiation pattern is explained primarily by the historical effect of the gaps as barriers, or whether a better understanding of floristic differentiation is achieved wh… Show more

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Cited by 49 publications
(75 citation statements)
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References 51 publications
(118 reference statements)
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“…A). This corresponds with other island groups stretched across large areas, where geographical lines may separate compositional groups (e.g., Kuril Archipelago, Pietsch et al, ; Ryukyu Archipelago, Nakamura et al, ; Malesia, Webb & Ree, ).…”
Section: Discussionsupporting
confidence: 66%
“…A). This corresponds with other island groups stretched across large areas, where geographical lines may separate compositional groups (e.g., Kuril Archipelago, Pietsch et al, ; Ryukyu Archipelago, Nakamura et al, ; Malesia, Webb & Ree, ).…”
Section: Discussionsupporting
confidence: 66%
“…Hirao et al, ; Kubota, Hirao, Fujii, & Murakami, ; Wepfer et al, ), and we demonstrate for the first time how extensions of island biogeography theory might apply to the Ryūkyū archipelago. Previous work in this system has suggested that both current and historic environmental factors should be considered simultaneously when assessing diversity of the Ryūkyūs (Nakamura, Suwa, Denda, & Yokota, ) and that climate and historic land connectivity drives ant community composition across the islands of East Asia (Wepfer et al, ). Here, we were unable to differentiate between the effects of contemporary and historic processes.…”
Section: Discussionmentioning
confidence: 99%
“…Palaeogeographically, during the Neogene, the Ryukyu Archipelago formed a land‐bridge and connected to the surrounding landmasses more than once, to Kyushu of the main Japanese islands in the north and to south‐eastern China via Taiwan in the south (Ota, 1998). These land connections allowed various lineages of terrestrial organisms to expand their ranges among the islands (Ota, 1998; Nakamura et al ., 2009). During the Pliocene (approximately 1.8–5.0 Mya), however, subsidence created two deep‐water passages in the island arc: the Tokara Gap (the Tokara tectonic strait) to the north of Amamioshima Island and the Kerama Gap to the south of Okinawajima Island (Fig.…”
Section: Discussionmentioning
confidence: 99%