Heinrichs Jochen, Scheben Armin, Bechteler Julia, Lee Gaik Ee, Schäfer-Verwimp Alfons, Hedenäs Lars, Singh Hukam, Pócs Tamás, Nascimbene Paul C, Peralta Denilson F, Renner Matt, Schmidt Alexander R
Department of Biology and Geobio-Center, University of Munich (LMU), Munich, Germany.
School of Marine and Environmental Sciences, University of Malaysia Terengganu, Terengganu, Malaysia.
PLoS One. 2016 May 31;11(5):e0156301. doi: 10.1371/journal.pone.0156301. eCollection 2016.
Cambay amber originates from the warmest period of the Eocene, which is also well known for the appearance of early angiosperm-dominated megathermal forests. The humid climate of these forests may have triggered the evolution of epiphytic lineages of bryophytes; however, early Eocene fossils of bryophytes are rare. Here, we present evidence for lejeuneoid liverworts and pleurocarpous mosses in Cambay amber. The preserved morphology of the moss fossil is inconclusive for a detailed taxonomic treatment. The liverwort fossil is, however, distinctive; its zig-zagged stems, suberect complicate-bilobed leaves, large leaf lobules, and small, deeply bifid underleaves suggest a member of Lejeuneaceae subtribe Lejeuneinae (Harpalejeunea, Lejeunea, Microlejeunea). We tested alternative classification possibilities by conducting divergence time estimates based on DNA sequence variation of Lejeuneinae using the age of the fossil for corresponding age constraints. Consideration of the fossil as a stem group member of Microlejeunea or Lejeunea resulted in an Eocene to Late Cretaceous age of the Lejeuneinae crown group. This reconstruction is in good accordance with published divergence time estimates generated without the newly presented fossil evidence. Balancing available evidence, we describe the liverwort fossil as the extinct species Microlejeunea nyiahae, representing the oldest crown group fossil of Lejeuneaceae.
坎贝琥珀形成于始新世最温暖的时期,这一时期也因早期以被子植物为主的高温森林的出现而闻名。这些森林的湿润气候可能引发了苔藓植物附生谱系的进化;然而,始新世早期的苔藓植物化石非常罕见。在这里,我们展示了坎贝琥珀中细鳞苔类叶苔和侧蒴藓类苔藓的证据。苔藓化石保存的形态对于详细的分类处理尚无定论。然而,叶苔化石却很独特;其之字形茎、近直立的复杂二裂叶、大叶小叶以及小而深裂的腹叶表明它是细鳞苔亚科(哈氏苔属、细鳞苔属、微鳞苔属)的一员。我们通过基于细鳞苔亚科的DNA序列变异进行分歧时间估计,并以化石年龄作为相应的年龄限制,来测试其他分类可能性。将该化石视为微鳞苔属或细鳞苔属的干群成员,会得出细鳞苔亚科冠群的年龄为始新世至晚白垩世。这一重建结果与在没有新发现的化石证据的情况下发表的分歧时间估计结果非常吻合。综合现有证据,我们将该叶苔化石描述为已灭绝的物种尼亚哈微鳞苔,它代表了细鳞苔科最古老的冠群化石。