Ladiges Pauline, Parra-O Carlos, Gibbs Adele, Udovicic Frank, Nelson Gareth, Bayly Michael
School of Botany, The University of Melbourne, Victoria 3010, Australia.
Instituto de Ciencias Naturales, Universidad Nacional de Colombia, A. A. 7495, Bogotá, Colombia.
Cladistics. 2011 Feb;27(1):29-41. doi: 10.1111/j.1096-0031.2010.00315.x.
Published phylogenies of two eucalypt clades, red bloodwoods Corymbia subgenus Corymbia and eudesmids Eucalyptus subgenus Eudesmia (Myrtaceae), were combined for an analysis of historical biogeographical area relationships within continental Australia. The method of paralogy-free subtree analysis was used to eliminate geographical paralogy; the paralogy-free subtrees were coded as characters for parsimony analysis to find the minimal and area cladogram, which proved to be informative of a continent-wide pattern. The eucalypt fossil record and molecular dating studies allow an interpretation of the biogeographical history in terms of major vicariance events that date from the early Paleogene. The summary area cladogram shows the wet jarrah forest region of South-West Western Australia, a region of high endemism, as the earliest to differentiate from all other areas, isolated by marine inundation across southern Australia and climatic cooling in the Late Eocene-Early Oligocene. From about this time, regionalization continued, with warmer conditions and monsoonal climate developing in central and northern Australia, and cooling in the south-east. Northern and eastern humid and semi-humid areas were related as a track, but with increased aridity in the interior of the continent, the monsoonal climate contracted northwards. The Australian Monsoon Tropics (AMT: Kimberley, Top End, Arnhem, Cape York and inland north-east Queensland) differentiated from eastern areas (Queensland wet tropics to McPherson-Macleay). Our results also show all arid and semi-arid regions as related, suggestive of a historically cohesive interior biota rather than repeated colonizations of the interior from the periphery of the continent. Climate largely differentiates hot arid areas in the north (Pilbara, Northern and Central deserts) from arid areas in the south (south-west interzone, Wheatbelt, Goldfields and Great Victoria Desert). © The Willi Hennig Society 2010.
已发表的两个桉属分支——赤桉亚属(Corymbia subgenus Corymbia)的红桉和桉亚属(Eucalyptus subgenus Eudesmia,桃金娘科)的桉类——的系统发育树被合并起来,用于分析澳大利亚大陆内部的历史生物地理区域关系。采用无并系同源性子树分析方法来消除地理并系同源性;将无并系同源性子树编码为性状进行简约分析,以找到最小和区域分支图,结果证明其能提供有关整个大陆模式的信息。桉属植物化石记录和分子年代测定研究有助于根据始于古近纪早期的主要隔离事件来解读生物地理历史。总结性区域分支图显示,西澳大利亚西南部的湿贾拉森林地区是一个特有性高的地区,它是最早从所有其他地区分化出来的,在晚始新世 - 早渐新世期间,被澳大利亚南部的海侵和气候变冷所隔离。大约从这个时候开始,区域分化持续进行,澳大利亚中部和北部出现了更温暖的气候和季风气候,而东南部则变冷。北部和东部的湿润和半湿润地区作为一个轨迹相互关联,但随着大陆内部干旱加剧,季风气候向北收缩。澳大利亚季风热带地区(AMT:金伯利、顶端地区、阿纳姆、约克角和昆士兰内陆东北部)与东部地区(昆士兰湿热带地区至麦克弗森 - 麦克利地区)分化开来。我们的研究结果还表明,所有干旱和半干旱地区都相互关联,这表明内陆生物群在历史上具有凝聚力,而不是从大陆边缘反复向内陆殖民。气候在很大程度上区分了北部的炎热干旱地区(皮尔巴拉、北部和中部沙漠)和南部的干旱地区(西南过渡带、小麦带、金矿地区和大维多利亚沙漠)。© 威利·亨尼希协会2010年。