Escapa Ignacio, Leslie Andrew
Consejo Nacional de Investigaciones Cientificas y Tecnológicas. Museo Paleontológico Egidio Feruglio, Fontana Av. 140, Trelew, Chubut, 9100, Argentina
Department of Ecology and Evolutionary Biology, Brown University, Box G-W, 80 Waterman Street, Providence, Rhode Island 02906 USA.
Am J Bot. 2017 Feb;104(2):322-334. doi: 10.3732/ajb.1600321. Epub 2017 Feb 17.
Plants preserved in different fossil modes provide complementary data concerning the paleobiology and evolutionary relationships among plant groups. New material from the Early Jurassic of Patagonia shows the importance of combining these sources of information, as we describe the first compression/impression fossils of , a genus of the extinct conifer family Cheirolepidiaceae previously known from permineralized fossils. These fossils extend the temporal range of this genus and may allow its wider recognition in the fossil record.
We studied fossil plants from the Early Jurassic (Pleinsbachian-Toarcian) locality of Taquetrén in Patagonia, Argentina using standard paleobotanical preparation and description techniques.
consists of isolated ovuliferous scales and small seed cones with helically arranged bract-scale complexes attached to scale-leaf foliage. Bract-scale complexes consist of separated bracts and ovuliferous scales with two seeds and three broad distal lobes.
represents the oldest known Cheirolepidiaceae seed cones from the Southern Hemisphere, and this material highlights the importance of compression and impression fossils in understanding the distribution of fossil taxa. This material also suggests that Cheirolepidiaceae cone scales can be easily confused with those of another common conifer family, the Araucariaceae, which has important implications for accurately understanding Mesozoic conifer diversity and paleoecology.
保存在不同化石模式下的植物为植物类群间的古生物学和进化关系提供了互补数据。来自巴塔哥尼亚早侏罗世的新材料显示了整合这些信息来源的重要性,因为我们描述了 的首批压型/印模化石, 是已灭绝的南洋杉科一个属,此前仅通过矿化化石为人所知。这些化石扩展了该属的时间范围,并可能使其在化石记录中得到更广泛的识别。
我们使用标准的古植物学制备和描述技术,研究了来自阿根廷巴塔哥尼亚塔奎特伦早侏罗世(普连斯巴奇阶—托尔阶)地点的化石植物。
由分离的含胚珠鳞片和小种子球果组成,带有附着在鳞片叶枝叶上呈螺旋状排列的苞鳞复合体。苞鳞复合体由分离的苞鳞和含胚珠鳞片组成,含两个种子和三个宽阔的远端裂片。
代表了南半球已知最古老的南洋杉科种子球果,这些材料突出了压型和印模化石在理解化石分类群分布方面的重要性。这些材料还表明,南洋杉科的球果鳞片很容易与另一个常见针叶树科——南洋杉科的鳞片混淆,这对于准确理解中生代针叶树的多样性和古生态具有重要意义。