Pedley L
Queensland Herbarium, Meiers Road, Indooroopilly, Queensland, Australia 4068.
Bot J Linn Soc. 1986 Apr;92(3):219-254. doi: 10.1111/j.1095-8339.1986.tb01429.x. Epub 2008 Jun 28.
The morphology of seedlings, leaves, flowers and inflorescences, anatomy of the pod, the occurrence of extra-floral nectaries, free amino acids of the seeds, flavonoid compounds in heartwoods, cyanogenic compounds and porate, colporate and extraporate pollen, and susceptibility to rusts, all indicate that three genera, Miller, Raf. and Martius, should be recognized. These correspond to currently accepted subgenera of The size of these more narrowly circumscribed genera is in keeping with the size of genera of other tribes of low diversity in Leguminosae. and arose independently from the Ingeae, with being derived from Section is more advanced than section of , and sections and , both with at least some species with bipinnate foliage, are the most advanced of , while the other sections and have only phyllodinous species. Long-range dispersal of from the Australian region has occurred, but the broad pattern of distribution is interpreted in terms of plate tectonics. was present in Australia in the late Cretaceous but did not become widespread until the general drying of the continent in the Miocene. The flora of SW Australia has been isolated from the rest of the continent by climatic barriers since the late Tertiary and has a high proportion of endemic species. Barriers to plant migration in the east have operated only intermittently and there is no area comparable in endemism to the southwest.
幼苗、叶片、花朵和花序的形态、豆荚的解剖结构、花外蜜腺的存在、种子中的游离氨基酸、心材中的黄酮类化合物、含氰化合物以及具孔、具沟和具额外孔的花粉,还有对锈病的易感性,所有这些都表明应该承认三个属,即米勒属(Miller)、拉夫属(Raf.)和马蒂乌斯属(Martius)。这些对应于目前被接受的[具体属名未提及]的亚属。这些界定更狭窄的属的大小与豆科中其他低多样性部落的属的大小一致。[具体内容不完整,推测此处可能是说这三个属]独立于印加族(Ingeae)起源,[具体属名未提及]由[具体来源未提及]衍生而来。[具体属名未提及]的[具体部分未提及]比[另一属名未提及]的[具体部分未提及]更进化,[具体属名未提及]的[具体部分未提及]和[具体部分未提及],两者都至少有一些具二回羽状叶的物种,是[具体属名未提及]中最进化的,而其他部分[具体部分未提及]和[具体部分未提及]只有叶状柄物种。[具体属名未提及]从澳大利亚地区发生了远距离扩散,但分布的广泛模式是根据板块构造来解释的。[具体属名未提及]在晚白垩世存在于澳大利亚,但直到中新世该大陆普遍干燥时才广泛分布。自第三纪晚期以来,澳大利亚西南部的植物区系因气候屏障而与大陆其他地区隔离,并且特有物种比例很高。东部植物迁移的障碍只是间歇性地起作用,没有一个地区在特有性方面能与西南部相比。