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Neogene palynology of the Solimões Basin, Brazilian Amazonia 巴西亚马逊河Solimões盆地新近纪孢粉学
IF 1.6 3区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2010-11-02 DOI: 10.1127/PALB/284/2010/13
S. D. Silva-Caminha, C. Jaramillo, M. Absy
The tropics of South America hold the largest plant diversity in the world, yet the origins and processes leading to this high diversity still remain elusive. The Neogene sedimentary and fossil record of Amazonia could contain important clues to understanding the evolution of the Amazonian forest. Here, we study the pollen and spore record of two drill cores of the Neogene Solimões Formation taken in northwestern Brazil, east of the Iquitos Arch. We studied 41 palynological samples and used several techniques to analyze the results, including Unitary Associations, a quantitative biostratigraphic technique, and Multidimensional Scaling Analysis. We describe 109 species, 51 of which are new, and seven new combinations. The biostratigraphic analysis indicates that the age of the Solimões Formation in the study area is Late Miocene/Early Pliocene. This age is younger than that of nearby sections located west of the Iquitos arch, suggesting that the Iquitos Arch was active during the accumulation of the Solimões Formation. The pollen/spore assemblages indicate that the Solimões accumulated in fluvial deposits. We did not find evidence of either marine/tidal-flat deposits or extensive lakes.
南美洲热带地区拥有世界上最大的植物多样性,但导致这种高度多样性的起源和过程仍然难以捉摸。亚马逊地区新近纪的沉积和化石记录可能为了解亚马逊森林的演变提供重要线索。本文对巴西西北部伊基托斯拱门以东新近系Solimões组两个岩心的花粉和孢子记录进行了研究。我们研究了41个孢粉样品,并使用多种技术对结果进行了分析,包括单一关联、定量生物地层技术和多维尺度分析。我们描述了109个物种,其中51个是新物种,还有7个新组合。生物地层分析表明,研究区Solimões组的时代为晚中新世/上新世早期。这一年龄比伊基托斯拱西侧附近剖面的年龄要小,说明伊基托斯拱在Solimões组的聚集过程中是活跃的。花粉/孢子组合表明Solimões沉积在河流沉积物中。我们没有发现海洋/潮滩沉积物或广泛湖泊的证据。
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引用次数: 83
Choerospondias turovensis n. sp., a new Anacardiacean species of the European Neogene identified from the Turów brown coal open-cast mine Turów褐煤露天矿中发现的欧洲新近系阿纳卡亚纲一新种
IF 1.6 3区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2010-11-02 DOI: 10.1127/PALB/284/2010/1
R. Kowalski
Remains of the genus Choerospondias Burtt et Hill of the family Anacardiaceae are reported from the Lowest Middle Miocene flora of the Turów brown coal open-cast mine. Choerospondias turovensis n. sp. is described and compared with the single contemporary representative, Choerospondias axillaris (Roxb.) B. L. Burtt et W. Hill. This is the first report of remains of this genus from the European Neogene.
报道了Turów褐煤露天矿中中新世晚期植物区系中发现的菊苣属(Choerospondias Burtt et Hill)化石。描述了turovensichoerospondias n. sp.并将其与单一的当代代表,Choerospondias axillaris (Roxb.)进行了比较。B. L.伯特和W.希尔。这是欧洲新近纪首次报道的该属化石。
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引用次数: 5
Evidence for fungivory in Cretaceous amber forests from Gondwana and Laurasia 冈瓦纳和劳亚的白垩纪琥珀林中真菌的证据
IF 1.6 3区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2010-10-04 DOI: 10.1127/PALB/283/2010/157
A. Schmidt, H. Dörfelt, Steffi Struwe, V. Perrichot
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引用次数: 24
Insect herbivores on Laurophyllum lanigeroides (Engelhardt 1922) Wilde: the role of a distinct plant-insect associational suite in host taxonomic assignment 昆虫在Laurophyllum lanigeroides上的食草动物(Engelhardt 1922)王尔德:一个独特的植物-昆虫组合在寄主分类分配中的作用
IF 1.6 3区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2010-10-04 DOI: 10.1127/PALB/283/2010/137
T. Wappler, M. Tokuda, J. Yukawa, V. Wilde
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引用次数: 10
A brief review of the fossil history of plantmasquerade by insects 昆虫伪装植物的化石史述评
IF 1.6 3区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2010-10-04 DOI: 10.1127/PALB/283/2010/175
S. Wedmann
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引用次数: 11
Plant-Insect Interactions in Deep Time: Contributions from the 8th International Organisation of Palaeobotany Conference in Bonn, Germany, August 30 – September 5, 2008 深层植物与昆虫的相互作用:2008年8月30日至9月5日在德国波恩举行的第八届国际古植物学组织会议的贡献
IF 1.6 3区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2010-10-04 DOI: 10.1127/PALB/283/2010/99
T. Wappler
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引用次数: 1
Coevolution of early angiosperms and their pollinators: Evidence from pollen 早期被子植物及其传粉者的共同进化:来自花粉的证据
IF 1.6 3区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2010-10-04 DOI: 10.1127/PALB/283/2010/103
David Winship, Shusheng Hu
Pollen morphology has traditionally been used to distinguish wind from animal pollination in angiosperms. In addition, the body of literature on Cretaceous angiosperm pollen clumps that may have had either a botanical or zoological origin is growing. Modern pollination biology studies suggest that the evolution of pollen clumping in flowers, resulting in floral pollen clumps, is attributable to insect pollination and that sticky pollen may be ancestral in angiosperms. The study of feces from pollen-eating insects suggests that pollen-containing coprolites (fossil insect fecal pellets) may provide information on both the organisms consuming the pollen and the identity of potential pollinators. We present here a preliminary study on dispersed pollen samples from Aptian to Campanian strata in the U.S.A. to examine the frequency of pollination modes based on dispersed pollen and to track the presence of pollen clumps. Criteria were developed to distinguish between floral pollen clumps and pollen-containing coprolites that show that fossil floral pollen clumps are irregularly shaped with rough surfaces and are composed of a single species of well-preserved grains, while the pollen-containing coprolites are regularly shaped with smooth surfaces and contain damaged grains. The preliminary data on the frequency of dispersed pollen support previous hypotheses that the Early Cretaceous angiosperms were insect-pollinated and that wind pollination became important later during the mid-Cretaceous. These pollen data also support the idea that ambophilous pollination, by both animals and wind, may have also existed early on. Floral pollen clumps appear only rarely until the mid-Cretaceous. The temporal distribution of clumps suggests that the pollen from early flowers were not sticky and that stickiness may have evolved with an adaptation to more advanced pollinators. Pollen-containing coprolites are found throughout the Cretaceous and vary in overall form, as well as in the preservation of individual grains. Based on previous studies of pollen-containing coprolites of insect origin, it seems likely that a number of insect digestive strategies, similar to those found in living members of Coleoptera, Diptera, and Hymenoptera were already in place by the late Mesozoic.
在被子植物中,花粉形态传统上被用来区分风传粉和动物传粉。此外,关于白垩纪被子植物花粉团可能有植物或动物起源的文献越来越多。现代传粉生物学研究认为,花粉在花中结块的进化与昆虫传粉有关,粘稠花粉可能起源于被子植物。对食花粉昆虫粪便的研究表明,含花粉的粪化石(化石昆虫粪便颗粒)可能提供有关食用花粉的生物和潜在传粉者身份的信息。本文对美国阿普tian至坎帕尼亚地层的分散花粉样本进行了初步研究,以研究基于分散花粉的传粉模式的频率,并追踪花粉团的存在。我们建立了区分花花粉团和含花粉粪化石的标准,表明化石花花粉团形状不规则,表面粗糙,由单一种保存完好的颗粒组成,而含花粉粪化石形状规则,表面光滑,含有损坏的颗粒。关于花粉传播频率的初步数据支持了之前的假设,即早白垩纪被子植物是昆虫传粉的,而风传粉在晚白垩纪中期变得重要。这些花粉数据也支持了一种观点,即动物和风的两栖授粉可能在早期就存在了。花花粉团很少出现,直到白垩纪中期。团块的时间分布表明,早期花朵的花粉不粘,这种粘可能是为了适应更高级的传粉者而进化的。含花粉的粪化石在整个白垩纪都有发现,它们的整体形态各不相同,保存的单个颗粒也各不相同。根据先前对昆虫起源的含花粉粪化石的研究,昆虫的一些消化策略似乎与鞘翅目、双翅目和膜翅目昆虫的消化策略相似,在中生代晚期就已经存在了。
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引用次数: 16
Dedicated to the memory of late Prof. Dr. Maurits Lindström, forever the expert on the Ordovician of Sweden 谨以此纪念已故的Maurits博士教授Lindström,他是瑞典奥陶纪的专家
IF 1.6 3区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2010-07-05 DOI: 10.1127/PALB/283/2010/5
Y. Grahn, J. Nõlvak
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引用次数: 26
An association of Alethopteris foliage, Trigonocarpus ovules and Bernaultia-like pollen organs from the Middle Pennsylvanian of Nova Scotia, Canada 加拿大新斯科舍省中宾夕法尼亚植物Alethopteris叶片、Trigonocarpus胚珠和bernaultia样花粉器官的组合
IF 1.6 3区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2010-07-05 DOI: 10.1127/PALB/283/2010/73
C. Cleal, E. Zodrow, M. Mastalerz
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引用次数: 17
On a Chinese Givetian lycopod, Longostachys latisporophyllus Zhu, Hu et Feng, emend: its morphology, anatomy and reconstruction 中国吉田一种石松属植物Longostachys latisporophyllus Zhu, Hu, et Feng,订正:形态、解剖和重建
IF 1.6 3区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2010-06-01 DOI: 10.1127/PALB/283/2010/1
Chongyang Cai, Chen Lizhu
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引用次数: 2
期刊
Palaeontographica Abteilung B-Palaeophytologie Palaeobotany-Palaeophytology
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