Bryophyte Diversity Is Related to Vascular Plant Diversity And

Total Page:16

File Type:pdf, Size:1020Kb

Bryophyte Diversity Is Related to Vascular Plant Diversity And Ecological Indicators 120 (2021) 106947 Contents lists available at ScienceDirect Ecological Indicators journal homepage: www.elsevier.com/locate/ecolind Bryophyte diversity is related to vascular plant diversity and microhabitat T under disturbance in karst caves ⁎ Hai Rena,b, ,1, Faguo Wanga,1, Wen Yea,1, Qianmei Zhanga, Taotao Hana, Yao Huanga,b, Guowei Chua, Dafeng Huic, Qinfeng Guod a CAS Engineering Laboratory for Vegetation Ecosystem Restoration on Islands and Coastal Zones, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou 510650, China b University of Chinese Academy of Sciences, Beijing 100049, China c Department of Biological Sciences, Tennessee State University, Nashville, TN 37209, USA d Southern Research Station, USDA Forest Service, Asheville, NC 28804, USA ARTICLE INFO ABSTRACT Keywords: Plant diversity, habitat properties, and their relationships in karst caves remain poorly understood. We surveyed Plant diversity vascular plant and bryophyte diversities and measured the habitat characteristics in six karst caves in south Habitat heterogeneity China with different disturbance histories (one had been disturbed by poultry feeding, three had been disturbed Light and water status by tourism, and two were undisturbed). The plant diversity differences among the six caves were analyzed using Soil nutrient cluster analysis, and the relationships of plant diversity and microhabitat were assessed using canonical cor- Restoration respondence analysis. We found a total of 43 angiosperm species from 27 families, 20 lycophyte and fern species from 9 families, and 20 species of bryophytes from 13 families in the six caves. Habitat characteristics including light intensity, air relative humidity, air temperature, and soil properties varied among the caves. The plant diversity in karst caves was not rich, but the species composition was unique. The caves with high disturbance had the lowest species richness, numbers of individuals, and Shannon-Wiener diversity indices but the highest Simpson’s dominance indices. The caves with less disturbance had the highest numbers of species, numbers of individuals, and Shannon-Wiener diversity indices but the lowest Simpson’s dominance indices. The disturbed caves were often dominated by drought-tolerant, tenacious mosses (bryophytes), while the relatively un- disturbed caves contained abundant liverworts (bryophytes), which were better adapted to humid environments. Plant diversity in karst caves was closely related to habitat heterogeneity, light and water status, and nutrient availability. Tourism and poultry farming were associated with the degradation of vegetation in some karst caves. Protecting and restoring bryophytes might facilitate the settlement, growth, and succession of vascular plants in karst caves. Bryophytes can be used as indicators of overall plant diversity and restoration status in karst caves. 1. Introduction features, the ecosystems in karst regions are fragile and extremely vulnerable to human disturbance (Brandt et al., 2018). Increased Karst landscapes are widely distributed and account for nearly 15% human exploitation of natural resources and agricultural activities have of the world’s land surface. The karst regions of China cover 1.9 million resulted in vegetation loss and land degradation during the last half km2 (about 0.54 million km2 are underlain by carbonate rocks) and are century in the karst regions of China (Tong et al., 2018). Karst soils are among the largest karst regions in the world (Yuan, 1994). The average thin and have great spatial heterogeneity, and these properties affect density of karst caves is 6.4/km2 in China as a whole and is 41.8/km2 in the conservation and restoration of the plant communities that they South China (Zhang, 1986). Topographic features of karst regions in- support (Cong et al., 2017; Wang et al., 2020). The structure, function, clude caves, sinkholes, and mogotes. Because of these geological and dynamics of karst vegetation in China have been recently ⁎ Corresponding author at: CAS Engineering Laboratory for Vegetation Ecosystem Restoration on Islands and Coastal Zones, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou 510650, China. E-mail addresses: [email protected], [email protected] (H. Ren), [email protected] (F. Wang), [email protected] (W. Ye), [email protected] (Q. Zhang), [email protected] (T. Han), [email protected] (Y. Huang), [email protected] (G. Chu), [email protected] (D. Hui), [email protected] (Q. Guo). 1 Contribute equally. https://doi.org/10.1016/j.ecolind.2020.106947 Received 28 February 2020; Received in revised form 13 August 2020; Accepted 8 September 2020 1470-160X/ © 2020 Elsevier Ltd. All rights reserved. H. Ren, et al. Ecological Indicators 120 (2021) 106947 investigated (Wang et al., 2011, 2020; Voloscuk et al., 2016; Zhang 2.2. Plant survey, soil sampling, and analysis et al., 2016; Cong et al., 2017; Cao et al., 2020; Tong et al., 2020). Although caves are threatened biodiversity hotspots, they receive The study involved six caves of similar size and altitude: Caves A, B, little governmental attention or appropriate management (Barr, 1964; C, and D are located in Dixiahe (the distance between them is < 2 km), Medellin et al., 2017). There is no governmental agency or non-gov- and Caves E and F are located in Shangbaichang (the distance between ernmental organization concerned with the conservation of cave eco- them is about 1 km). Shangbaichang is about 21 km away from Dixiahe. systems in China or in many other countries (Whitte, 2009). There are Caves A, B, and C were developed into tourist spots in 1988. At present, caving expeditions, but such expeditions concentrate on exploration there are 800,000 visitors every year at Cave A. Cave B was closed to rather than on the investigating cave organisms. Disturbances by tourism and subjected to natural restoration after 2000. Cave C was farming, visitors, tourism infrastructure, and changes in water flow can protected after 2010. Caves D and E were relatively undisturbed. Cave F have devastating effects on the highly adapted and range-restricted has long been used to feed poultry and is highly disturbed. The major organisms that live in caves (Whitte, 2009). Cave conservation and disturbances to caves A, B, and C included atmospheric, water, and restoration therefore require the attention of researchers and govern- noise pollution, the damage and interference on animals and plants, mental agencies (Elliott, 2006). The use of mosses as nurse plants to and the damages caused by the construction of scenic spots. The major restore endangered herbs in karst caves is one of the few studies of karst disturbances at cave F included atmosphere pollution and the con- cave restoration (Ren et al., 2010a). sumption of plants by poultry. We could not find three replicate caves Although cave vegetation and soils are important in the study of with similar size and altitude for each disturbance type in Lianzhou autogenic/primary succession, cave ecology, evolutionary biology, and City. Therefore, we did not conduct any univariate statistical compar- global change biology, they are poorly understood (Barr, 1964; Bai isons of richness and diversity values among disturbance types or lo- et al., 2020). Karst caves and their entrances have dim light with lim- cation types within the caves. ited nutrient availability, high humidity, and relatively low tempera- At each cave, we established three plots, each with an area of ture fluctuations (Northup and Lavoie, 2001). The karst cave plant 5 m × 5 m, along a transect from the entrance of the cave to deep into community is a relic of the surrounding karst forest community and is the cave; the intervals between plots (from the entrance inward) were strongly dominated by understory life forms and taxa. The vegetation at 10, 30, and 60 m. Hereafter, the plots at the entrance, at the deepest cave entrances usually has low species richness and a small number of location, and at the intermediate location are referred to as entrance individuals (Supplementary Fig. 1 and Supplementary Fig. 2). In con- plots, deep plots, and intermediate plots. A light gradient existed among trast, the plant communities in karst caves are often diverse (Monro the plots at each cave because the light exposure declined with distance et al., 2018). Bryophytes are the most common plants in karst caves from the cave entrance. Field sampling was conducted at the beginning (Mulec and Kubešová, 2010; Cong et al., 2017; Puglisi et al, 2019). of November 2018. Bryophytes may be used as indicators of plant diversity and ecosystem All plant species were identified in each plot, and the height, den- health in karst caves. The plant diversity in karst caves is closely related sity, and crown of all plant species were measured (Ren et al., 2010b). to micro-habitat properties. As noted earlier, human disturbance such Three subplots with an area of 1 m × 1 m each were established in each as tourism and agriculture can lead to habitat and vegetation de- plot; the bryophyte, lichen, and algal species and their coverage area gradation in karst caves (Belnap and Lange, 2013; Liu et al., 2019; were recorded in each subplot (Li et al., 2015; Cong et al., 2017; Wu Pakeman et al., 2019). Leaf nutrient concentrations of cave-dwelling et al., 2019). We also collected soil samples during vegetation surveys. plants often reveal convergent adaptations to cave environments (Bai Because the soils around the cave entrances
Recommended publications
  • The First Megafossil Record of Goniophlebium (Polypodiaceae
    Available online at www.sciencedirect.com ScienceDirect Palaeoworld 26 (2017) 543–552 The first megafossil record of Goniophlebium (Polypodiaceae) from the Middle Miocene of Asia and its paleoecological implications a,e a,e a c a,d a,b,∗ Cong-Li Xu , Jian Huang , Tao Su , Xian-Chun Zhang , Shu-Feng Li , Zhe-Kun Zhou a Key Laboratory of Tropical Forest Ecology, Xishuangbanna Tropical Botanical Garden, Chinese Academy of Sciences, Menglun, Mengla 666303, Yunnan, China b Key Laboratory for Plant Diversity and Biogeography of East Asia, Kunming Institute of Botany, Chinese Academy of Sciences, Kunming 650201, China c State Key Laboratory of Systematic and Evolutionary Botany, Institute of Botany, Chinese Academy of Sciences, Beijing 100093, China d State Key Laboratory of Paleobiology and Stratigraphy, Nanjing Institute of Geology and Paleontology, Chinese Academy of Sciences, Nanjing 210008, China e University of the Chinese Academy of Sciences, Beijing 100049, China Received 30 August 2016; accepted 19 January 2017 Available online 17 April 2017 Abstract The first megafossil record of Goniophlebium macrosorum Xu et Zhou n. sp., is described from the Middle Miocene Climate Optimum (MMCO) (15.2–16.5 Ma) sediments in Wenshan, southeastern Yunnan, China. The fossils are with well-preserved leaf pinnae and in situ spores, and are represented by pinnatifid fronds and crenate pinna margins, with oval sori almost covering 3/5 area of areolae on each side of the main costa. In situ spores have verrucate outer ornamentation, and are elliptical in polar view and bean-shaped in equatorial view. The venation is characterized by anastomosing veins with simple included veinlets forming 2–3 order pentagonal areolae.
    [Show full text]
  • Prescribed Fire Decreases Lichen and Bryophyte Biomass and Alters Functional Group Composition in Pacific Northwest Prairies Author(S): Lalita M
    Prescribed Fire Decreases Lichen and Bryophyte Biomass and Alters Functional Group Composition in Pacific Northwest Prairies Author(s): Lalita M. Calabria, Kate Petersen, Sarah T. Hamman and Robert J. Smith Source: Northwest Science, 90(4):470-483. Published By: Northwest Scientific Association DOI: http://dx.doi.org/10.3955/046.090.0407 URL: http://www.bioone.org/doi/full/10.3955/046.090.0407 BioOne (www.bioone.org) is a nonprofit, online aggregation of core research in the biological, ecological, and environmental sciences. BioOne provides a sustainable online platform for over 170 journals and books published by nonprofit societies, associations, museums, institutions, and presses. Your use of this PDF, the BioOne Web site, and all posted and associated content indicates your acceptance of BioOne’s Terms of Use, available at www.bioone.org/page/terms_of_use. Usage of BioOne content is strictly limited to personal, educational, and non-commercial use. Commercial inquiries or rights and permissions requests should be directed to the individual publisher as copyright holder. BioOne sees sustainable scholarly publishing as an inherently collaborative enterprise connecting authors, nonprofit publishers, academic institutions, research libraries, and research funders in the common goal of maximizing access to critical research. Lalita M. Calabria1, Kate Petersen,The Evergreen State College, 2700 Evergreen Parkway NW, Olympia, Washington 98505 Sarah T. Hamman, The Center for Natural Lands Management, 120 Union Ave SE #215, Olympia, Washington 98501 and Robert J. Smith, Department of Botany and Plant Pathology, 2082 Cordley Hall, Oregon State University, Corvallis, Oregon 97331 Prescribed Fire Decreases Lichen and Bryophyte Biomass and Alters Functional Group Composition in Pacific Northwest Prairies Abstract The reintroduction of fire to Pacific Northwest prairies has been useful for removing non-native shrubs and supporting habitat for fire-adapted plant and animal species.
    [Show full text]
  • Bryophyte Life Cycle
    MARCH 2016LEARNING | VELD & FLORA ABOUT BIODIVERSITY Veld & Flora MARCHFACTSHEET: 2016 | VELD MOSS & FLORA 24 25 3. BRYOPHYTE LIFE CYCLE Gametophyte (n) UNDERSTANDING THE GERMINATION MALE ALTERNATION OF GENERATIONS The way that almost all land plants reproduce is by means of two distinct, alternating life forms, a sexual phase that produces and releases gametes or sex cells and allows fertilisation, and a dispersal phase – both of which are adaptations to an essentially waterless environment. The sexual phase is known as the GAMETOPHYTE or haploid spores (n) generation and the dispersal phase is the SPOROPHYTE or diploid (2n) generation. Mature gametophyte plants produce haploid sex cells (egg and sperm) in sex organs (the male antheridia and female archegonia). These sex cells (also called gametes) fuse during fertilisation to form a diploid (2n) zygote which COPING OUT OF WATER grows, by means of mitosis (that results in two daughter cells each having Sperm (n) the same number and kind of chromosomes as the parent cell), into a new released Bryophytes, which include moss, are primitive plants that give us some idea sporophyte plant. The diploid sporophyte produces haploid (n) spores (i.e. from male of how the first plants that ventured onto land coped with their new waterless FEMALE each spore has a single set of chromosomes) by means of the process environment. They share many features with other plants, but differ in some of cell division called meiosis. Meiosis results in four daughter cells each ways – such as the lack of an effective vascular system (specialised tissue for with half the number of chromosomes of the parent cell.
    [Show full text]
  • The Origin of Alternation of Generations in Land Plants
    Theoriginof alternation of generations inlandplants: afocuson matrotrophy andhexose transport Linda K.E.Graham and LeeW .Wilcox Department of Botany,University of Wisconsin, 430Lincoln Drive, Madison,WI 53706, USA (lkgraham@facsta¡.wisc .edu ) Alifehistory involving alternation of two developmentally associated, multicellular generations (sporophyteand gametophyte) is anautapomorphy of embryophytes (bryophytes + vascularplants) . Microfossil dataindicate that Mid ^Late Ordovicianland plants possessed such alifecycle, and that the originof alternationof generationspreceded this date.Molecular phylogenetic data unambiguously relate charophyceangreen algae to the ancestryof monophyletic embryophytes, and identify bryophytes as early-divergentland plants. Comparison of reproduction in charophyceans and bryophytes suggests that the followingstages occurredduring evolutionary origin of embryophytic alternation of generations: (i) originof oogamy;(ii) retention ofeggsand zygotes on the parentalthallus; (iii) originof matrotrophy (regulatedtransfer ofnutritional and morphogenetic solutes fromparental cells tothe nextgeneration); (iv)origin of a multicellularsporophyte generation ;and(v) origin of non-£ agellate, walled spores. Oogamy,egg/zygoteretention andmatrotrophy characterize at least some moderncharophyceans, and arepostulated to represent pre-adaptativefeatures inherited byembryophytes from ancestral charophyceans.Matrotrophy is hypothesizedto have preceded originof the multicellularsporophytes of plants,and to represent acritical innovation.Molecular
    [Show full text]
  • Microsorum 3 Tohieaense (Polypodiaceae)
    Systematic Botany (2018), 43(2): pp. 397–413 © Copyright 2018 by the American Society of Plant Taxonomists DOI 10.1600/036364418X697166 Date of publication June 21, 2018 Microsorum 3 tohieaense (Polypodiaceae), a New Hybrid Fern from French Polynesia, with Implications for the Taxonomy of Microsorum Joel H. Nitta,1,2,3 Saad Amer,1 and Charles C. Davis1 1Department of Organismic and Evolutionary Biology and Harvard University Herbaria, Harvard University, Cambridge, Massachusetts 02138, USA 2Current address: Department of Botany, National Museum of Nature and Science, 4-1-1 Amakubo, Tsukuba, Japan, 305-0005 3Author for correspondence ([email protected]) Communicating Editor: Alejandra Vasco Abstract—A new hybrid microsoroid fern, Microsorum 3 tohieaense (Microsorum commutatum 3 Microsorum membranifolium) from Moorea, French Polynesia is described based on morphology and molecular phylogenetic analysis. Microsorum 3 tohieaense can be distinguished from other French Polynesian Microsorum by the combination of sori that are distributed more or less in a single line between the costae and margins, apical pinna wider than lateral pinnae, and round rhizome scales with entire margins. Genetic evidence is also presented for the first time supporting the hybrid origin of Microsorum 3 maximum (Microsorum grossum 3 Microsorum punctatum), and possibly indicating a hybrid origin for the Hawaiian endemic Microsorum spectrum. The implications of hybridization for the taxonomy of microsoroid ferns are discussed, and a key to the microsoroid ferns of the Society Islands is provided. Keywords—gapCp, Moorea, rbcL, Society Islands, Tahiti, trnL–F. Hybridization, or interbreeding between species, plays an et al. 2008). However, many species formerly placed in the important role in evolutionary diversification (Anderson 1949; genus Microsorum on the basis of morphology (Bosman 1991; Stebbins 1959).
    [Show full text]
  • Polypodiaceae (PDF)
    This PDF version does not have an ISBN or ISSN and is not therefore effectively published (Melbourne Code, Art. 29.1). The printed version, however, was effectively published on 6 June 2013. Zhang, X. C., S. G. Lu, Y. X. Lin, X. P. Qi, S. Moore, F. W. Xing, F. G. Wang, P. H. Hovenkamp, M. G. Gilbert, H. P. Nooteboom, B. S. Parris, C. Haufler, M. Kato & A. R. Smith. 2013. Polypodiaceae. Pp. 758–850 in Z. Y. Wu, P. H. Raven & D. Y. Hong, eds., Flora of China, Vol. 2–3 (Pteridophytes). Beijing: Science Press; St. Louis: Missouri Botanical Garden Press. POLYPODIACEAE 水龙骨科 shui long gu ke Zhang Xianchun (张宪春)1, Lu Shugang (陆树刚)2, Lin Youxing (林尤兴)3, Qi Xinping (齐新萍)4, Shannjye Moore (牟善杰)5, Xing Fuwu (邢福武)6, Wang Faguo (王发国)6; Peter H. Hovenkamp7, Michael G. Gilbert8, Hans P. Nooteboom7, Barbara S. Parris9, Christopher Haufler10, Masahiro Kato11, Alan R. Smith12 Plants mostly epiphytic and epilithic, a few terrestrial. Rhizomes shortly to long creeping, dictyostelic, bearing scales. Fronds monomorphic or dimorphic, mostly simple to pinnatifid or 1-pinnate (uncommonly more divided); stipes cleanly abscising near their bases or not (most grammitids), leaving short phyllopodia; veins often anastomosing or reticulate, sometimes with included veinlets, or veins free (most grammitids); indument various, of scales, hairs, or glands. Sori abaxial (rarely marginal), orbicular to oblong or elliptic, occasionally elongate, or sporangia acrostichoid, sometimes deeply embedded, sori exindusiate, sometimes covered by cadu- cous scales (soral paraphyses) when young; sporangia with 1–3-rowed, usually long stalks, frequently with paraphyses on sporangia or on receptacle; spores hyaline to yellowish, reniform, and monolete (non-grammitids), or greenish and globose-tetrahedral, trilete (most grammitids); perine various, usually thin, not strongly winged or cristate.
    [Show full text]
  • Extant Diversity of Bryophytes Emerged from Successive Post-Mesozoic Diversification Bursts
    ARTICLE Received 20 Mar 2014 | Accepted 3 Sep 2014 | Published 27 Oct 2014 DOI: 10.1038/ncomms6134 Extant diversity of bryophytes emerged from successive post-Mesozoic diversification bursts B. Laenen1,2, B. Shaw3, H. Schneider4, B. Goffinet5, E. Paradis6,A.De´samore´1,2, J. Heinrichs7, J.C. Villarreal7, S.R. Gradstein8, S.F. McDaniel9, D.G. Long10, L.L. Forrest10, M.L. Hollingsworth10, B. Crandall-Stotler11, E.C. Davis9, J. Engel12, M. Von Konrat12, E.D. Cooper13, J. Patin˜o1, C.J. Cox14, A. Vanderpoorten1,* & A.J. Shaw3,* Unraveling the macroevolutionary history of bryophytes, which arose soon after the origin of land plants but exhibit substantially lower species richness than the more recently derived angiosperms, has been challenged by the scarce fossil record. Here we demonstrate that overall estimates of net species diversification are approximately half those reported in ferns and B30% those described for angiosperms. Nevertheless, statistical rate analyses on time- calibrated large-scale phylogenies reveal that mosses and liverworts underwent bursts of diversification since the mid-Mesozoic. The diversification rates further increase in specific lineages towards the Cenozoic to reach, in the most recently derived lineages, values that are comparable to those reported in angiosperms. This suggests that low diversification rates do not fully account for current patterns of bryophyte species richness, and we hypothesize that, as in gymnosperms, the low extant bryophyte species richness also results from massive extinctions. 1 Department of Conservation Biology and Evolution, Institute of Botany, University of Lie`ge, Lie`ge 4000, Belgium. 2 Institut fu¨r Systematische Botanik, University of Zu¨rich, Zu¨rich 8008, Switzerland.
    [Show full text]
  • Bryophyte Diversity and Vascular Plants
    DISSERTATIONES BIOLOGICAE UNIVERSITATIS TARTUENSIS 75 BRYOPHYTE DIVERSITY AND VASCULAR PLANTS NELE INGERPUU TARTU 2002 DISSERTATIONES BIOLOGICAE UNIVERSITATIS TARTUENSIS 75 DISSERTATIONES BIOLOGICAE UNIVERSITATIS TARTUENSIS 75 BRYOPHYTE DIVERSITY AND VASCULAR PLANTS NELE INGERPUU TARTU UNIVERSITY PRESS Chair of Plant Ecology, Department of Botany and Ecology, University of Tartu, Estonia The dissertation is accepted for the commencement of the degree of Doctor philosophiae in plant ecology at the University of Tartu on June 3, 2002 by the Council of the Faculty of Biology and Geography of the University of Tartu Opponent: Ph.D. H. J. During, Department of Plant Ecology, the University of Utrecht, Utrecht, The Netherlands Commencement: Room No 218, Lai 40, Tartu on August 26, 2002 © Nele Ingerpuu, 2002 Tartu Ülikooli Kirjastuse trükikoda Tiigi 78, Tartu 50410 Tellimus nr. 495 CONTENTS LIST OF PAPERS 6 INTRODUCTION 7 MATERIAL AND METHODS 9 Study areas and field data 9 Analyses 10 RESULTS 13 Correlation between bryophyte and vascular plant species richness and cover in different plant communities (I, II, V) 13 Environmental factors influencing the moss and field layer (II, III) 15 Effect of vascular plant cover on the growth of bryophytes in a pot experiment (IV) 17 The distribution of grassland bryophytes and vascular plants into different rarity forms (V) 19 Results connected with nature conservation (I, II, V) 20 DISCUSSION 21 CONCLUSIONS 24 SUMMARY IN ESTONIAN. Sammaltaimede mitmekesisus ja seosed soontaimedega. Kokkuvõte 25 < TÄNUSÕNAD. Acknowledgements 28 REFERENCES 29 PAPERS 33 2 5 LIST OF PAPERS The present thesis is based on the following papers which are referred to in the text by the Roman numerals.
    [Show full text]
  • Fern Classification
    16 Fern classification ALAN R. SMITH, KATHLEEN M. PRYER, ERIC SCHUETTPELZ, PETRA KORALL, HARALD SCHNEIDER, AND PAUL G. WOLF 16.1 Introduction and historical summary / Over the past 70 years, many fern classifications, nearly all based on morphology, most explicitly or implicitly phylogenetic, have been proposed. The most complete and commonly used classifications, some intended primar• ily as herbarium (filing) schemes, are summarized in Table 16.1, and include: Christensen (1938), Copeland (1947), Holttum (1947, 1949), Nayar (1970), Bierhorst (1971), Crabbe et al. (1975), Pichi Sermolli (1977), Ching (1978), Tryon and Tryon (1982), Kramer (in Kubitzki, 1990), Hennipman (1996), and Stevenson and Loconte (1996). Other classifications or trees implying relationships, some with a regional focus, include Bower (1926), Ching (1940), Dickason (1946), Wagner (1969), Tagawa and Iwatsuki (1972), Holttum (1973), and Mickel (1974). Tryon (1952) and Pichi Sermolli (1973) reviewed and reproduced many of these and still earlier classifica• tions, and Pichi Sermolli (1970, 1981, 1982, 1986) also summarized information on family names of ferns. Smith (1996) provided a summary and discussion of recent classifications. With the advent of cladistic methods and molecular sequencing techniques, there has been an increased interest in classifications reflecting evolutionary relationships. Phylogenetic studies robustly support a basal dichotomy within vascular plants, separating the lycophytes (less than 1 % of extant vascular plants) from the euphyllophytes (Figure 16.l; Raubeson and Jansen, 1992, Kenrick and Crane, 1997; Pryer et al., 2001a, 2004a, 2004b; Qiu et al., 2006). Living euphyl• lophytes, in turn, comprise two major clades: spermatophytes (seed plants), which are in excess of 260 000 species (Thorne, 2002; Scotland and Wortley, Biology and Evolution of Ferns and Lycopliytes, ed.
    [Show full text]
  • Havens for Wildlife
    )"7&/4'038*-%-*'& 4FDUJPO# .PTTFT -JWFSXPSUTBOE'FSOT This sheet explains what mosses, liverworts and Liverworts ferns are, where they occur and guidelines on how Liverworts are similar to to care for them in a burial ground. mosses but tend to be The earliest land plants were related to ferns and leafy and are less common. mosses. They started life growing on the edge of lakes Liverworts are mostly found and rivers 400 million years ago. Today most ferns, in woodland and by streams mosses and liverworts still need to grow in moist or rivers but can also be found places. on shady stones and damp soil in burial grounds. They are With our damp climate many burial sites prove ideal for strange, distinctive looking ferns, mosses and liverworts, particularly in the western plants and worth looking at areas of Britain and Ireland. closely or photographing their Adder’s-tongue Fern intricate shapes and subtle colours. MOSSES AND LIVERWORTS Mosses and liverworts are known as FERNS ‘bryophytes’. They are small, green plants *OUIFDPPM XFUDMJNBUFPGUIF6,UIFSFBSFUZQFTPG which do not have !owers or seeds but fern. Look out for ferns on west or north facing walls produce spores instead. There are over in particular. The shady areas of burial grounds, and 1000 di"erent species of bryophyte in under trees, where grass cutters don’t reach, will also UIF6,BOEUIFZUFOEUPCFGPVOEJO be places where ferns can !ourish undisturbed. sheltered, damp places as most of them cannot survive drying out. Few mosses An amazing fact about ferns is that once established PSMJWFSXPSUTIBWF&OHMJTIOBNFTBOEB they can survive in quite dry places, such as walls.
    [Show full text]
  • An Inverse Latitudinal Diversity Gradient in European Bryophytes Received: 26 November 2015 Rubén G
    www.nature.com/scientificreports OPEN The mossy north: an inverse latitudinal diversity gradient in European bryophytes Received: 26 November 2015 Rubén G. Mateo1,2,3, Olivier Broennimann1, Signe Normand4, Blaise Petitpierre1, Accepted: 19 April 2016 Miguel B. Araújo5,6,7, Jens-C. Svenning4, Andrés Baselga8, Federico Fernández-González3, Published: 06 May 2016 Virgilio Gómez-Rubio9, Jesús Muñoz10, Guillermo M. Suarez11, Miska Luoto12, Antoine Guisan1,* & Alain Vanderpoorten2,* It remains hotly debated whether latitudinal diversity gradients are common across taxonomic groups and whether a single mechanism can explain such gradients. Investigating species richness (SR) patterns of European land plants, we determine whether SR increases with decreasing latitude, as predicted by theory, and whether the assembly mechanisms differ among taxonomic groups. SR increases towards the south in spermatophytes, but towards the north in ferns and bryophytes. SR patterns in spermatophytes are consistent with their patterns of beta diversity, with high levels of nestedness and turnover in the north and in the south, respectively, indicating species exclusion towards the north and increased opportunities for speciation in the south. Liverworts exhibit the highest levels of nestedness, suggesting that they represent the most sensitive group to the impact of past climate change. Nevertheless, although the extent of liverwort species turnover in the south is substantially and significantly lower than in spermatophytes, liverworts share with the latter a higher nestedness in the north and a higher turn-over in the south, in contrast to mosses and ferns. The extent to which the similarity in the patterns displayed by spermatophytes and liverworts reflects a similar assembly mechanism remains, however, to be demonstrated.
    [Show full text]
  • Plant Evolution and Diversity Part 1: Bryophytes and Ferns the Three Domains • Plant-Like Protists Are Autotrophs – They Contain Chloroplasts and Make Their Own Food
    Plant Evolution and Diversity Part 1: Bryophytes and Ferns The Three Domains • Plant-like protists are autotrophs – they contain chloroplasts and make their own food. • Animal-like and fungus-like protists and are heterotrophs. Fungi – not plants Non-photosynthetic eukaryotes, saprophytic, Reproduce by spores, chitin cell walls (not cellulose) Includes yeast What is a plant? Traditional View of Biology: Animals and Plants Problem: Microscopic Organisms (Bacteria, Fungi, Algae) Complication: Endosymbiotic origin of organelles (Lynn Margulis) Membrane-bound structures in eukaryotic cells are derived from formerly free-living organisms that have become intimately symbiotic What is a Plant? 1. Eukaryotic - nucleus 2. Chloroplasts present 3. Cell wall with cellulose 4. Autotrophic – make own food What is a Plant? 1. Eukaryotic 2. Chloroplasts present 3. Cell wall with cellulose 4. Autotrophic 5. Complex Life Cycle (alternation of generations) Algae - Diverse, single-celled to complex seaweeds Photosynthetic eukaryotes, green plants Plant-like protists – “Algae” • Diverse group – green, red, and brown algae. • Single celled or multicellular. • Autotrophs (plants), form the foundation of Earth’s food chains. • Produce much of Earth’s oxygen. Green Algae – Chlorophytes and Charophytes • Chlorophyll a and b, like land plants • Many forms – single celled, filamentous, colonial, sheets • May have other pigments, orange or red • Related to land plants Ulva – Sea Lettuce • Chlorophyte - Marine • Sheets 2 cells thick • Alternation of Generations like land plants Chara – Stonewort • Charophyte • Freshwater • Calcium carbonate deposits, crusty feel branch • Whorls of branches • Reproductive structures at nodes main axis node a. Chara, several individuals b. One individual a: © Bob Gibbons/Alamy; b: © Kingsley Stern The phylogeny of land plants The likely ancestor are charophycean algae • same chloroplast DNA, ribosomal DNA • same membrane structure, peroxisomes, sperm cells Chara Land plants are most closely related to freshwater green algae known as charophytes.
    [Show full text]