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Growth and Population Dynamics of Posidonia Oceanica on the S~Anishmediterranean Coast: Elucidatina Seacrrass Decline
MARINE ECOLOGY PROGRESS SERIES Vol. 137: 203-213, 1996 Published June 27 Mar Ecol Prog Ser Growth and population dynamics of Posidonia oceanica on the S~anishMediterranean coast: elucidatina seacrrass decline Nuria ~arba'l*,Carlos M. ~uarte',Just cebrianl, Margarita E. ~allegos~, Birgit Olesen3, Kaj sand-~ensen~ 'Centre dlEstudis Avanqats de Blanes, C.S.I.C., Cami de Santa Barbara sin, E-17300 Blanes, Girona, Spain 'Departamento de Hidrobiologia, Universidad Autonoma Metropolitana- Iztapalapa, Michocan y Purisima, col. Vicentina, AP 55-535, 09340 Mexico D.F., Mexico 3Department of Plant Ecology, University of Aarhus, Nordlandsvej 68, DK-8240 Risskov. Denmark 'Freshwater Biological Laboratory. University of Copenhagen, 51 Helsingersgade, DK-3400 Hillered. Denmark ABSTRACT: The growth and population dynamics of Posidonia oceanica were examined in 29 mead- ows along 1000 km of the Spanish Mediterranean coast (from 36"46' to 42"22' N). oceanica devel- oped the densest meadows (1141 shoots m-') and the highest aboveground biomass (1400 g DW m") between 38 and 39"N. P. oceanica shoots produced, on average, 1 leaf every 47 d, though leaf forma- tion rates in the populations increased from north to south (range 5 7 to 8.9leaves shoot-' yr-'). P ocean- ica is a long-living seagrass, with shoots able to live for at least 30 yr P, oceanica recruited shoots at low rates (0.02 to 0.5 In units yr-l) which did not balance the mortality rates (0.06 to 0.5 In unlts yr.') found in most (57 %) of the meadows. If the present disturbance and rate of decline are maintained, shoot den- sity is predicted to decline by 50% over the coming 2 to 24 yr. -
Global Seagrass Distribution and Diversity: a Bioregional Model ⁎ F
Journal of Experimental Marine Biology and Ecology 350 (2007) 3–20 www.elsevier.com/locate/jembe Global seagrass distribution and diversity: A bioregional model ⁎ F. Short a, , T. Carruthers b, W. Dennison b, M. Waycott c a Department of Natural Resources, University of New Hampshire, Jackson Estuarine Laboratory, Durham, NH 03824, USA b Integration and Application Network, University of Maryland Center for Environmental Science, Cambridge, MD 21613, USA c School of Marine and Tropical Biology, James Cook University, Townsville, 4811 Queensland, Australia Received 1 February 2007; received in revised form 31 May 2007; accepted 4 June 2007 Abstract Seagrasses, marine flowering plants, are widely distributed along temperate and tropical coastlines of the world. Seagrasses have key ecological roles in coastal ecosystems and can form extensive meadows supporting high biodiversity. The global species diversity of seagrasses is low (b60 species), but species can have ranges that extend for thousands of kilometers of coastline. Seagrass bioregions are defined here, based on species assemblages, species distributional ranges, and tropical and temperate influences. Six global bioregions are presented: four temperate and two tropical. The temperate bioregions include the Temperate North Atlantic, the Temperate North Pacific, the Mediterranean, and the Temperate Southern Oceans. The Temperate North Atlantic has low seagrass diversity, the major species being Zostera marina, typically occurring in estuaries and lagoons. The Temperate North Pacific has high seagrass diversity with Zostera spp. in estuaries and lagoons as well as Phyllospadix spp. in the surf zone. The Mediterranean region has clear water with vast meadows of moderate diversity of both temperate and tropical seagrasses, dominated by deep-growing Posidonia oceanica. -
Morpho-Chronological Variations and Primary Production in Posidonia
Morpho-chronological variations and primary production in Posidonia sea grass from Western Australia Gérard Pergent, Christine Pergent-Martini, Catherine Fernandez, Pasqualini Vanina, Diana Walker To cite this version: Gérard Pergent, Christine Pergent-Martini, Catherine Fernandez, Pasqualini Vanina, Diana Walker. Morpho-chronological variations and primary production in Posidonia sea grass from Western Aus- tralia. Journal of the Marine Biological Association of the United Kingdom, Cambridge University Press, 2004, 84 (5), pp.895-899. 10.1017/S0025315404010161h. hal-01768985 HAL Id: hal-01768985 https://hal.archives-ouvertes.fr/hal-01768985 Submitted on 17 Apr 2018 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. J. Mar. Biol. Ass. U.K. (2004), 84, 895^899 Printed in the United Kingdom Morpho-chronological variations and primary production in Posidonia sea grass from Western Australia P Ge¤rard Pergent* , Christine Pergent-Martini*, Catherine Fernandez*, O Vanina Pasqualini* and Diana Walker O *Equipe Ecosyste' mes Littoraux, Faculty of Sciences, -
Use of Posidonia Oceanica Seedlings from Beach- Cast Fruits for Seagrass Planting
DOI 10.1515/bot-2012-0200 Botanica Marina 2013; 56(2): 185–195 Jorge Terrados * , Arnaldo Mar í n and David Celdr á n Use of Posidonia oceanica seedlings from beach- cast fruits for seagrass planting Abstract: Posidonia oceanica seedlings produced from biological productivity, nutrient cycling, carbon burial beach-cast fruits were planted in an area where this and sediment stabilisation (Hemminga and Duarte 2000 ). Mediterranean seagrass was lost as a consequence of fish- In the last century, human populations in coastal zones farming. The effects of substratum type (dead matte vs. have been rapidly increasing. This has increased anthro- meadow) and planting level (above vs. below bottom sur- pogenic impacts on seagrass ecosystems, in turn leading face) on seedling survivorship and leaf development were to a worldwide decline of seagrasses (Orth et al. 2006a , evaluated after 3 years. Seedling capacity to resist uproot- Waycott et al. 2009 ). Seagrass declines have stimulated ing was also tested by comparing survivorship and leaf interest in seagrass restoration research, and several development after 2 years in seedlings firmly anchored approaches have been used (Fonseca et al. 1998 , Treat in dead matte by artificial means (mesh-pot) with those and Lewis 2006 , Paling et al. 2009 ) because adaptation to planted without any anchoring other than their roots. Sur- local conditions and to the features of the seagrass species vivorship in dead matte was 44 % after 3 years and was to be planted is required. A record of seagrass presence in not affected by planting level. Seedling planting inside the past, knowledge about what caused seagrass loss and the meadow led to complete mortality after 3 years. -
Chemotyping the Lignin of Posidonia Seagrasses
APL001 Analytical Pyrolysis Letters 1 Chemotyping the lignin of Posidonia seagrasses JOERI KAAL1,O SCAR SERRANO 2,J OSÉ CARLOS DEL RÍO3, AND JORGE RENCORET3 1Pyrolyscience, Santiago de Compostela, Spain 2Edith Cowan University, Joondalup, Australia 3IRNAS, CSIC, Seville, Spain Compiled January 18, 2019 A recent paper in Organic Geochemistry entitled "Radi- cally different lignin composition in Posidonia species may link to differences in organic carbon sequestration capacity" discusses the remarkable difference in lignin chemistry between two kinds of “Neptune grass”, i.e. Posidonia oceanica and Posidonia australis. A recent paper in Organic Geochemistry entitled "Radically different lignin composition in Posidonia species may link to differences in organic carbon sequestration capacity" discusses the remarkable difference in lignin chemistry between two kinds of “Neptune grass”, i.e. Posidonia oceanica and Posidonia australis. Initial efforts using analytical pyrolysis techniques (Py-GC- MS and THM-GC-MS) showed that the endemic Mediterranean Fig. 1. Posidonia oceanica mat deposits in Portlligat (Western member of the Posidonia genus, P. oceanica, has abnormally Mediterranean). Photo: Kike Ballesteros high amounts of p-HBA (para-hydroxybenzoic acid) whereas the down-under variety does not. State-of-the-art lignin charac- terization in Seville (DFRC, 2D-NMR) showed that the p-HBA ranean high-carbon accumulator (see figure below), but it proba- is part of the lignin backbone, and not glycosylated as initially bly contains slightly more p-HBA than Posidonia australis. Posido- expected, and P. oceanica is now the producer of the most exten- nia sinuosa is not capable of producing big mat deposits neither, sively p-HBA-acylated lignin known in the Plant Kingdom. -
GENOME EVOLUTION in MONOCOTS a Dissertation
GENOME EVOLUTION IN MONOCOTS A Dissertation Presented to The Faculty of the Graduate School At the University of Missouri In Partial Fulfillment Of the Requirements for the Degree Doctor of Philosophy By Kate L. Hertweck Dr. J. Chris Pires, Dissertation Advisor JULY 2011 The undersigned, appointed by the dean of the Graduate School, have examined the dissertation entitled GENOME EVOLUTION IN MONOCOTS Presented by Kate L. Hertweck A candidate for the degree of Doctor of Philosophy And hereby certify that, in their opinion, it is worthy of acceptance. Dr. J. Chris Pires Dr. Lori Eggert Dr. Candace Galen Dr. Rose‐Marie Muzika ACKNOWLEDGEMENTS I am indebted to many people for their assistance during the course of my graduate education. I would not have derived such a keen understanding of the learning process without the tutelage of Dr. Sandi Abell. Members of the Pires lab provided prolific support in improving lab techniques, computational analysis, greenhouse maintenance, and writing support. Team Monocot, including Dr. Mike Kinney, Dr. Roxi Steele, and Erica Wheeler were particularly helpful, but other lab members working on Brassicaceae (Dr. Zhiyong Xiong, Dr. Maqsood Rehman, Pat Edger, Tatiana Arias, Dustin Mayfield) all provided vital support as well. I am also grateful for the support of a high school student, Cady Anderson, and an undergraduate, Tori Docktor, for their assistance in laboratory procedures. Many people, scientist and otherwise, helped with field collections: Dr. Travis Columbus, Hester Bell, Doug and Judy McGoon, Julie Ketner, Katy Klymus, and William Alexander. Many thanks to Barb Sonderman for taking care of my greenhouse collection of many odd plants brought back from the field. -
The Global Distribution and Status of Seagrass Ecosystems
The global distribution and status of seagrass ecosystems ^^ ^^^H Discussion paper prepared for tlie UNEP-WCWIC Global Seagrass Workshop St Pete's Beach, Florida, 9 November, 2001 Prepared by: Mark D. Spalding, Michelle L. Taylor, Sergio Martins, Edmund P. Green, and Mary Edwards WA.. WORLD CONSERVATION MONITORING CENTRE Digitized by tine Internet Archive in 2010 witii funding from UNEP-WCIVIC, Cambridge Iittp://www.archive.org/details/globaldistributi01spal The global distribution and status of seagrass ecosystems Discussion paper prepared for tlie UNEP-WCIVIC Global Seagrass Workshop St Pete's Beach, Florida, 9 November, 2001 Prepared by: Mark D. Spalding, Michelle L. Taylor, Sergio Martins, Edmund P. Green, and Mary Edwards With assistance from: Mark Taylor and Corinna Ravilious Table of Contents Introduction to the workshop 2 The global distribution and status of seagrass ecosystems 3 Introduction 3 Definitions 3 The diversity of seagrasses 3 Species distribution 4 Associated Species 6 Productivity and biomass 7 The distribution and area of seagrass habitat 8 The value of seagrasses 13 Threats to seagrasses 13 Management Interventions 14 Bibliography; 16 29 Annex 1 : Seagrass Species Lists by Country Annex 2 - Species distribution maps 34 Annex 3 - Seagrass distribution maps 68 74 Annex 4 -Full list of MPAs by country ; /4^ ] UNEP WCMC Introduction to the workshop The Global Seagrass Workshop of 9 November 2001 has been set up with the expressed aim to develop a global synthesis on the distribution and status of seagrasses world-wide. Approximately 20 seagrass experts from 14 counu-ies, representing all of the major seagrass regions of the world have been invited to share their knowledge and expertise. -
The Genus Ruppia L. (Ruppiaceae) in the Mediterranean Region: an Overview
Aquatic Botany 124 (2015) 1–9 Contents lists available at ScienceDirect Aquatic Botany journal homepage: www.elsevier.com/locate/aquabot The genus Ruppia L. (Ruppiaceae) in the Mediterranean region: An overview Anna M. Mannino a,∗, M. Menéndez b, B. Obrador b, A. Sfriso c, L. Triest d a Department of Sciences and Biological Chemical and Pharmaceutical Technologies, Section of Botany and Plant Ecology, University of Palermo, Via Archirafi 38, 90123 Palermo, Italy b Department of Ecology, University of Barcelona, Av. Diagonal 643, 08028 Barcelona, Spain c Department of Environmental Sciences, Informatics & Statistics, University Ca’ Foscari of Venice, Calle Larga S. Marta, 2137 Venice, Italy d Research Group ‘Plant Biology and Nature Management’, Vrije Universiteit Brussel, Pleinlaan 2, B-1050 Brussels, Belgium article info abstract Article history: This paper reviews the current knowledge on the diversity, distribution and ecology of the genus Rup- Received 23 December 2013 pia L. in the Mediterranean region. The genus Ruppia, a cosmopolitan aquatic plant complex, is generally Received in revised form 17 February 2015 restricted to shallow waters such as coastal lagoons and brackish habitats characterized by fine sediments Accepted 19 February 2015 and high salinity fluctuations. In these habitats Ruppia meadows play an important structural and func- Available online 26 February 2015 tional role. Molecular analyses revealed the presence of 16 haplotypes in the Mediterranean region, one corresponding to Ruppia maritima L., and the others to various morphological forms of Ruppia cirrhosa Keywords: (Petagna) Grande, all together referred to as the “R. cirrhosa s.l. complex”, which also includes Ruppia Aquatic angiosperms Ruppia drepanensis Tineo. -
Nacionalni Park Brijuni
EVALUATION REPORT Nacionalni park Brijuni Location: Off the coast of western Istria, Republic of Croatia, Northern Adriatic Sea, Mediterranean Blue Park Status: Nominated (2021), Evaluated (2021) MPAtlas.org ID: 15663 Manager(s): Marno Milotić, Public Institution Brijuni National Park MAPS 2 1. ELIGIBILITY CRITERIA 1.1 Biodiversity Value 4 1.2 Implementation 6 2. AWARD STATUS CRITERIA 2.1 Regulations 9 2.2 Design, Management, and Compliance 11 3. SYSTEM PRIORITIES 3.1 Ecosystem Representation 16 3.2 Ecological Spatial Connectivity 17 SUPPLEMENTAL INFORMATION: Evidence of MPA Effects 17 Figure 1: Brijuni National Park covers 26.5 km2 of marine area off the Istrian coast of Croatia in the Northern Adriatic Sea. It contains 14 uninhabited islands and includes the surrounding sea and shelf area. Brijuni National Park is divided into four zones: 1a) the Zone of Very Strict Protection and 1b) the Zone of Strict Protection are shown together in dark blue – the Regulations-Based Classification score is 1 (fully protected); 2) the Zone of Directed Protection is shown in light blue and the Regulations-Based Classification Score is 4 (highly protected); and 3) the Zone of Usage is shown in dark blue and lined – the Regulations-Based Classification score is 3 (fully protected). See Section 2.1 for an explanation of the the Regulations-Based Classification scores. (Source: Marine Protection Atlas, Marine Conservation Institute) - 2 - Figure 2: Brijuni National Park’s Zone of Strict Protection has two sub-zones: 1a) Zone of Very Strict Protection shown in dark green and 1b) Zone of Strict Protection shown in light green. -
Absence of Evidence Is Not Evidence of Absence
UNEP-WCMC Technical Briefing Note December, 2015 Absence of evidence is not evidence of absence Working with data deficiency in global biodiversity spatial datasets Key messages More data is unknown than known in both the terrestrial and marine realms, due to numerous technical, logistical and financial challenges in biodiversity data collection at a global scale. Data deficiencies are therefore a common feature within global datasets. Users of global biodiversity datasets are often faced with uncertainty when interpreting data deficiencies: It is not always possible to infer whether the Interpretative approaches to data deficiency (red: false value, green: features themselves are absent, or whether the data required was absent. true value) Cases of confirmed absence of biodiversity features are also rarely highlighted within datasets. The absence of data may coincide with areas on-the-ground where the feature of interest exists, and areas where it does not exist. This may lead to two interpretative scenarios (see above right): - The true negative: No data is displayed in the area of interest because the biodiversity feature does not occur there. - The false negative: No data is displayed in the area of interest, however the biodiversity feature does occur on site. It is commonly misinterpreted that data deficiency (or data absence) is evidence that the feature is absent, but this is often not the case. Data deficiencies should be interpreted as “unknowns” with the potential for both presence and absence until further investigation or supplementary information is available to confirm whether a particular feature exists. This principle also applies to cases of species categorized as Data Deficient on the IUCN Red List of Threatened Species1. -
Restoration of Seagrass Meadows in the Mediterranean Sea: a Critical Review of Effectiveness and Ethical Issues
water Review Restoration of Seagrass Meadows in the Mediterranean Sea: A Critical Review of Effectiveness and Ethical Issues Charles-François Boudouresque 1,*, Aurélie Blanfuné 1,Gérard Pergent 2 and Thierry Thibaut 1 1 Aix-Marseille University and University of Toulon, MIO (Mediterranean Institute of Oceanography), CNRS, IRD, Campus of Luminy, 13009 Marseille, France; [email protected] (A.B.); [email protected] (T.T.) 2 Università di Corsica Pasquale Paoli, Fédération de Recherche Environnement et Societé, FRES 3041, Corti, 20250 Corsica, France; [email protected] * Correspondence: [email protected] Abstract: Some species of seagrasses (e.g., Zostera marina and Posidonia oceanica) have declined in the Mediterranean, at least locally. Others are progressing, helped by sea warming, such as Cymodocea nodosa and the non-native Halophila stipulacea. The decline of one seagrass can favor another seagrass. All in all, the decline of seagrasses could be less extensive and less general than claimed by some authors. Natural recolonization (cuttings and seedlings) has been more rapid and more widespread than was thought in the 20th century; however, it is sometimes insufficient, which justifies transplanting operations. Many techniques have been proposed to restore Mediterranean seagrass meadows. However, setting aside the short-term failure or half-success of experimental operations, long-term monitoring has usually been lacking, suggesting that possible failures were considered not worthy of a scientific paper. Many transplanting operations (e.g., P. oceanica) have been carried out at sites where the species had never previously been present. Replacing the natural Citation: Boudouresque, C.-F.; ecosystem (e.g., sandy bottoms, sublittoral reefs) with P. -
On the Sea-Grasses in Japan (III)
On the Sea-grasses in Japan (III). General Consideration on the Japanese Sea-grasses By Shigeru Niiki Received October 3, 1933 I. Characters of Sea-Grasses A. Shape B. Morphological Differences from the Allied Fresh Water Plants II. Distribution of Sea-Grasses A. General Distribution B. Sea-Grasses in the World C. On Non-Occurrence of Posidonia in Japan III. Floristic Consideration of Sea-Grasses in Japan A. Zosteraceae B. Cymodoceaceae C. Ilydrocaritaceae IV. Summary V. Literature There are eight genera of sea-grasses known in the world. Of these, with the exception of Posidonia, seven remaining genera represented by 15 species, are found in Japan. They have been described in my previous papers (9, 10 and 11). Among them the great majority of Zostera and Phyllospadix species are endemic, while Gym odocea, Diplanthera except one, and all species of the Hydrocaritaceae belong to the Indo-1\Ialay element. The morphological characters of sea-grasses together with their ecological and floristic distribution in general may now be considered. I. Characters of Sea-Grasses A. Shape The leaf is ribbon-like in form except in Halophila and the vegetative shoots grow all the year round except in the northern form of Zostera nana. The arrangement of leaves vary in different families; in the Hydro- 172 THE BOTANICAL MAGAZINE (vol. XLVIII,No. X67 caritaceae they are arranged on the upper and lower side of the rhizome and without axillant leaf on the branches except the rhizome of T halassia (11), while in all other families leaves are attached to the lateral sides of rhizome, and each branch is provided with an axillant leaf.