Carpenter Raymond J, McLoughlin Stephen, Hill Robert S, McNamara Kenneth J, Jordan Gregory John
School of Biological Sciences, University of Tasmania, Private Bag 55, Hobart, Tasmania 7001, Australia School of Earth and Environmental Sciences, Benham Bldg DX 650 312, University of Adelaide, South Australia 5005, Australia.
Department of Palaeobiology, Swedish Museum of Natural History, Box 50007 104 05 Stockholm, Sweden.
Am J Bot. 2014 Sep;101(9):1486-97. doi: 10.3732/ajb.1400191.
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Globally, the origins of xeromorphic traits in modern angiosperm lineages are obscure but are thought to be linked to the early Neogene onset of seasonally arid climates. Stomatal encryption is a xeromorphic trait that is prominent in Banksia, an archetypal genus centered in one of the world's most diverse ecosystems, the ancient infertile landscape of Mediterranean-climate southwestern Australia.•
We describe Banksia paleocrypta, a sclerophyllous species with encrypted stomata from silcretes of the Walebing and Kojonup regions of southwestern Australia dated as Late Eocene.•
Banksia paleocrypta shows evidence of foliar xeromorphy ∼20 Ma before the widely accepted timing for the onset of aridity in Australia. Species of Banksia subgenus Banksia with very similar leaves are extant in southwestern Australia. The conditions required for silcrete formation infer fluctuating water tables and climatic seasonality in southwestern Australia in the Eocene, and seasonality is supported by the paucity of angiosperm closed-forest elements among the fossil taxa preserved with B. paleocrypta. However, climates in the region during the Eocene are unlikely to have experienced seasons as hot and dry as present-day summers.•
The presence of B. paleocrypta within the center of diversity of subgenus Banksia in edaphically ancient southwestern Australia is consistent with the continuous presence of this lineage in the region for ≥40 Ma, a testament to the success of increasingly xeromorphic traits in Banksia over an interval in which numerous other lineages became extinct.
研究前提:在全球范围内,现代被子植物谱系中旱生性状的起源尚不清楚,但被认为与新近纪早期季节性干旱气候的出现有关。气孔加密是一种旱生性状,在山龙眼科植物中很突出,山龙眼科是一个典型的属,集中分布在世界上最多样化的生态系统之一,即澳大利亚西南部地中海气候的古老贫瘠景观中。
方法:我们描述了山龙眼古隐种,这是一种硬叶物种,其气孔加密,来自澳大利亚西南部瓦勒宾和科乔纳普地区的硅质岩,年代为始新世晚期。
主要结果:山龙眼古隐种显示出叶旱生特征的证据,比澳大利亚干旱开始的广泛接受时间早约2000万年。山龙眼亚属中具有非常相似叶子的物种现存于澳大利亚西南部。硅质岩形成所需的条件表明,始新世时澳大利亚西南部地下水位波动且气候具有季节性,而山龙眼古隐种所保存的化石类群中被子植物封闭森林元素的稀少也支持了季节性。然而,始新世该地区的气候不太可能经历过如今夏季那样炎热干燥的季节。
结论:在土壤古老的澳大利亚西南部山龙眼亚属的多样性中心存在山龙眼古隐种,这与该谱系在该地区持续存在≥4000万年一致,证明了在许多其他谱系灭绝的时期里,山龙眼科植物中旱生性状越来越成功。