2008
DOI: 10.1016/j.foreco.2008.01.027
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Ecology of tertiary relict endemic Liquidambar orientalis Mill. forests

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Cited by 40 publications
(23 citation statements)
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“…These disjunctive distributions are remnants of their wide distribution during the Tertiary period. This genus had flourished well in a wide area covering East Asia, Central Asia, Asia Minor, America and Central Europe during the Miocene, and disappeared in Europe and Northwest America in the Pleistocene as a result of extensive glaciations (Öztürk et al, 2008 ). After these glaciations, the natural distributions of Liquidambar species were forced into refugia in East Asia, Turkey and North America (Ozdilek et al, 2012 ).…”
Section: Introductionmentioning
confidence: 99%
“…These disjunctive distributions are remnants of their wide distribution during the Tertiary period. This genus had flourished well in a wide area covering East Asia, Central Asia, Asia Minor, America and Central Europe during the Miocene, and disappeared in Europe and Northwest America in the Pleistocene as a result of extensive glaciations (Öztürk et al, 2008 ). After these glaciations, the natural distributions of Liquidambar species were forced into refugia in East Asia, Turkey and North America (Ozdilek et al, 2012 ).…”
Section: Introductionmentioning
confidence: 99%
“…Both were known and utilised in antiquity, for example as an incense, medicinal or cosmetic product 32 . While their modern distribution (South of Europe and the Middle East 33 for the former, and the South of Turkey, Cyprus and Rhodes 34 for the latter) would favour S. officinalis as the source of the archaeological resin, both were considered as a potential match. GC/MS investigation of fresh S. officinalis ( Fig.…”
Section: Resultsmentioning
confidence: 99%
“…Liquidambar formosana Hance is a Neogene relict plant of the genus Liquidambar from the monotypic family Altingiaceae are mainly distributed in subtropical China and has a long evolutionary history [14,15]. Genus Liquidambar had flourished well in a wide region covering East Asia, Central Asia, Asia Minor, America, and Central Europe during the Miocene, and then disappeared in Europe and Northwest America in the Pleistocene as a result of extensive glaciations [16,17]. Although now restricted in the south of China, L. formosana has a long fossil record of pollen (about 70 Ma) in the northeast of China.…”
Section: Introductionmentioning
confidence: 99%