Evaluation and Gap Analysis of Current and Potential Indicators for Deep Sea Habitats
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We Would Like to Thank the Referees for Constructive Review, That Helped Us to Improve the Manuscript
We would like to thank the Referees for constructive review, that helped us to improve the manuscript. Written below are our responses to the Referee’s comments. The comments were reproduced and are followed by our responses. Anonymous Referee #1 This paper presents an interesting multiproxy dataset to document the paleoceanography near Svalbard and compares traditional sedimentary and microfossil proxies with a novel approach involving ancient environmental DNA. As such, the dataset certainly deserves publishing, but I have some comments/reservations about the age model and the discussion of the results. The discussion has some writing-technical issues. In several cases the own results are presented, without clear arguments supporting the interpretation (e.g. P12, L9–11 & L28–30; P15, L12– 15) but rather followed by a literature review. The own results need to be better used to document the paleoceanographic/ environmental signal that is gained from this new site and data, before comparing to the literature. Figures integrating the own results with key records from previous studies is also advised. Major comments Referee’s comment: First of all, the raw data needs to be made publicly available and/or presented with the manuscript. Needed are tables that list unique sample labels and relevant metadata such as core coordinates, sampling depths, measured data for each proxy (sedimentology, foraminifer assemblage data, stable isotopes and aDNA), etc. Response: According to the Reviewer’s suggestion, the raw data will be provided as electronic supplementary material. Referee’s comment: Age model. The ages used for the age model seem arbitrary. What is the argument to choose 1500, 2700 and 7890 yr BP? Those ages are not the average of the 2 sigma calibrated yrs BP. -
Protist Phylogeny and the High-Level Classification of Protozoa
Europ. J. Protistol. 39, 338–348 (2003) © Urban & Fischer Verlag http://www.urbanfischer.de/journals/ejp Protist phylogeny and the high-level classification of Protozoa Thomas Cavalier-Smith Department of Zoology, University of Oxford, South Parks Road, Oxford, OX1 3PS, UK; E-mail: [email protected] Received 1 September 2003; 29 September 2003. Accepted: 29 September 2003 Protist large-scale phylogeny is briefly reviewed and a revised higher classification of the kingdom Pro- tozoa into 11 phyla presented. Complementary gene fusions reveal a fundamental bifurcation among eu- karyotes between two major clades: the ancestrally uniciliate (often unicentriolar) unikonts and the an- cestrally biciliate bikonts, which undergo ciliary transformation by converting a younger anterior cilium into a dissimilar older posterior cilium. Unikonts comprise the ancestrally unikont protozoan phylum Amoebozoa and the opisthokonts (kingdom Animalia, phylum Choanozoa, their sisters or ancestors; and kingdom Fungi). They share a derived triple-gene fusion, absent from bikonts. Bikonts contrastingly share a derived gene fusion between dihydrofolate reductase and thymidylate synthase and include plants and all other protists, comprising the protozoan infrakingdoms Rhizaria [phyla Cercozoa and Re- taria (Radiozoa, Foraminifera)] and Excavata (phyla Loukozoa, Metamonada, Euglenozoa, Percolozoa), plus the kingdom Plantae [Viridaeplantae, Rhodophyta (sisters); Glaucophyta], the chromalveolate clade, and the protozoan phylum Apusozoa (Thecomonadea, Diphylleida). Chromalveolates comprise kingdom Chromista (Cryptista, Heterokonta, Haptophyta) and the protozoan infrakingdom Alveolata [phyla Cilio- phora and Miozoa (= Protalveolata, Dinozoa, Apicomplexa)], which diverged from a common ancestor that enslaved a red alga and evolved novel plastid protein-targeting machinery via the host rough ER and the enslaved algal plasma membrane (periplastid membrane). -
Author's Manuscript (764.7Kb)
1 BROADLY SAMPLED TREE OF EUKARYOTIC LIFE Broadly Sampled Multigene Analyses Yield a Well-resolved Eukaryotic Tree of Life Laura Wegener Parfrey1†, Jessica Grant2†, Yonas I. Tekle2,6, Erica Lasek-Nesselquist3,4, Hilary G. Morrison3, Mitchell L. Sogin3, David J. Patterson5, Laura A. Katz1,2,* 1Program in Organismic and Evolutionary Biology, University of Massachusetts, 611 North Pleasant Street, Amherst, Massachusetts 01003, USA 2Department of Biological Sciences, Smith College, 44 College Lane, Northampton, Massachusetts 01063, USA 3Bay Paul Center for Comparative Molecular Biology and Evolution, Marine Biological Laboratory, 7 MBL Street, Woods Hole, Massachusetts 02543, USA 4Department of Ecology and Evolutionary Biology, Brown University, 80 Waterman Street, Providence, Rhode Island 02912, USA 5Biodiversity Informatics Group, Marine Biological Laboratory, 7 MBL Street, Woods Hole, Massachusetts 02543, USA 6Current address: Department of Epidemiology and Public Health, Yale University School of Medicine, New Haven, Connecticut 06520, USA †These authors contributed equally *Corresponding author: L.A.K - [email protected] Phone: 413-585-3825, Fax: 413-585-3786 Keywords: Microbial eukaryotes, supergroups, taxon sampling, Rhizaria, systematic error, Excavata 2 An accurate reconstruction of the eukaryotic tree of life is essential to identify the innovations underlying the diversity of microbial and macroscopic (e.g. plants and animals) eukaryotes. Previous work has divided eukaryotic diversity into a small number of high-level ‘supergroups’, many of which receive strong support in phylogenomic analyses. However, the abundance of data in phylogenomic analyses can lead to highly supported but incorrect relationships due to systematic phylogenetic error. Further, the paucity of major eukaryotic lineages (19 or fewer) included in these genomic studies may exaggerate systematic error and reduces power to evaluate hypotheses. -
Introduction to Marine Conservation Biology
Network of Conservation Educators & Practitioners Introduction to Marine Conservation Biology Author(s): Tundi Agardy Source: Lessons in Conservation, Vol. 1, pp. 5-43 Published by: Network of Conservation Educators and Practitioners, Center for Biodiversity and Conservation, American Museum of Natural History Stable URL: ncep.amnh.org/linc/ This article is featured in Lessons in Conservation, the official journal of the Network of Conservation Educators and Practitioners (NCEP). NCEP is a collaborative project of the American Museum of Natural History’s Center for Biodiversity and Conservation (CBC) and a number of institutions and individuals around the world. Lessons in Conservation is designed to introduce NCEP teaching and learning resources (or “modules”) to a broad audience. NCEP modules are designed for undergraduate and professional level education. These modules—and many more on a variety of conservation topics—are available for free download at our website, ncep.amnh.org. To learn more about NCEP, visit our website: ncep.amnh.org. All reproduction or distribution must provide full citation of the original work and provide a copyright notice as follows: “Copyright 2007, by the authors of the material and the Center for Biodiversity and Conservation of the American Museum of Natural History. All rights reserved.” Illustrations obtained from the American Museum of Natural History’s library: images.library.amnh.org/digital/ SYNTHESIS 5 Introduction to Marine Conservation Biology Tundi Agardy* *Sound Seas, Bethesda, MD, USA, email -
Deep-Ocean Climate Change Impacts on Habitat, Fish and Fisheries, by Lisa Levin, Maria Baker, and Anthony Thompson (Eds)
ISSN 2070-7010 FAO 638 FISHERIES AND AQUACULTURE TECHNICAL PAPER 638 Deep-ocean climate change impacts on habitat, fish and fisheries Deep-ocean climate change impacts on habitat, fish and fisheries This publication presents the outcome of a meeting between the FAO/UNEP ABNJ Deep-seas and Biodiversity project and the Deep Ocean Stewardship Initiative. It focuses on the impacts of climatic changes on demersal fisheries, and the interactions of these fisheries with other species and vulnerable marine ecosystems. Regional fisheries management organizations rely on scientific information to develop advice to managers. In recent decades, climate change has been a focus largely as a unidirectional forcing over decadal timescales. However, changes can occur abruptly when critical thresholds are crossed. Moreover, distribution changes are expected as populations shift from existing to new areas. Hence, there is a need for new monitoring programmes to help scientists understand how these changes affect productivity and biodiversity. costa = 9,4 mm ISBN 978-92-5-131126-4 ISSN 2070-7010 FA 9 789251 311264 CA2528EN/1/09.19 O Cover image: Time of emergence of seafloor climate changes. Figure 7 in Chapter 8 of this Technical Paper. FAO FISHERIES AND Deep-ocean climate change AQUACULTURE TECHNICAL impacts on habitat, fish and PAPER fisheries 638 Edited by Lisa Levin Center for Marine Biodiversity and Conservation and Integrative Oceanography Division Scripps Institution of Oceanography University of California San Diego United States of America Maria Baker University of Southampton National Oceanography Centre Southampton United Kingdom of Great Britain and Northern Ireland Anthony Thompson Consultant Fisheries and Aquaculture Department Food and Agriculture Organization of the United Nations Rome Italy FOOD AND AGRICULTURE ORGANIZATION OF THE UNITED NATIONS Rome, 2018 FAO. -
Levels of Biotic Organization - Alberto M
BIOLOGICAL SCIENCE FUNDAMENTALS AND SYSTEMATICS – Vol. I – Levels of Biotic Organization - Alberto M. Simonetta LEVELS OF BIOTIC ORGANIZATION Alberto M. Simonetta Dipartimento di Biologia Animale e Genetica, “L. Pardi,” University of Firenze, Italy Keywords: Morphology, systematics, ecological niche, parasites, symbionts, population. Contents 1. Introduction 2. The Development of Organization at the Individual Level 3. The Development of Organization: Embryology and Cycles 4. The Paleontological Account 5. The Intertaxa Organization and Evolution 6. Symbiosis and Parasitism 7. Conclusion Biographical Sketch Summary The level of biotic organization may be considered from different perspectives and these are briefly outlined. A merely structural level of the individuals is the most traditional approach, but it must be considered that there is a basic difference between a simple structure that is actually primitive and such highly evolved conditions as obtain in some parasitic or symbiotic organisms. Other levels of biotic organization that have to be considered concern the organization of communities and ecosystems, as well as symbioses. A brief discussion is therefore provided for each of the different aspects that biotic organization may take according the perspective from which it is considered. 1. Introduction Living beings may be studied from different, albeit converging perspectives. They may be studied from the simplest level of organization of the individual organism, such as that of procaryotes.UNESCO Then one may consider mo–re andEOLSS more complex levels of individual structure. But we may begin by considering the individual’s interactions with its immediate environment, and then follow the chains and networks of such organisms, until we reach the comprehensive idea of “biosphere” or, perhaps, given the close interactions thatSAMPLE have obtained since the origin CHAPTERS of life, between living organisms and all other components of the ecosystem, up to the so-called Gaia system. -
Systema Naturae. the Classification of Living Organisms
Systema Naturae. The classification of living organisms. c Alexey B. Shipunov v. 5.601 (June 26, 2007) Preface Most of researches agree that kingdom-level classification of living things needs the special rules and principles. Two approaches are possible: (a) tree- based, Hennigian approach will look for main dichotomies inside so-called “Tree of Life”; and (b) space-based, Linnaean approach will look for the key differences inside “Natural System” multidimensional “cloud”. Despite of clear advantages of tree-like approach (easy to develop rules and algorithms; trees are self-explaining), in many cases the space-based approach is still prefer- able, because it let us to summarize any kinds of taxonomically related da- ta and to compare different classifications quite easily. This approach also lead us to four-kingdom classification, but with different groups: Monera, Protista, Vegetabilia and Animalia, which represent different steps of in- creased complexity of living things, from simple prokaryotic cell to compound Nature Precedings : doi:10.1038/npre.2007.241.2 Posted 16 Aug 2007 eukaryotic cell and further to tissue/organ cell systems. The classification Only recent taxa. Viruses are not included. Abbreviations: incertae sedis (i.s.); pro parte (p.p.); sensu lato (s.l.); sedis mutabilis (sed.m.); sedis possi- bilis (sed.poss.); sensu stricto (s.str.); status mutabilis (stat.m.); quotes for “environmental” groups; asterisk for paraphyletic* taxa. 1 Regnum Monera Superphylum Archebacteria Phylum 1. Archebacteria Classis 1(1). Euryarcheota 1 2(2). Nanoarchaeota 3(3). Crenarchaeota 2 Superphylum Bacteria 3 Phylum 2. Firmicutes 4 Classis 1(4). Thermotogae sed.m. 2(5). -
Protista (PDF)
1 = Astasiopsis distortum (Dujardin,1841) Bütschli,1885 South Scandinavian Marine Protoctista ? Dingensia Patterson & Zölffel,1992, in Patterson & Larsen (™ Heteromita angusta Dujardin,1841) Provisional Check-list compiled at the Tjärnö Marine Biological * Taxon incertae sedis. Very similar to Cryptaulax Skuja Laboratory by: Dinomonas Kent,1880 TJÄRNÖLAB. / Hans G. Hansson - 1991-07 - 1997-04-02 * Taxon incertae sedis. Species found in South Scandinavia, as well as from neighbouring areas, chiefly the British Isles, have been considered, as some of them may show to have a slightly more northern distribution, than what is known today. However, species with a typical Lusitanian distribution, with their northern Diphylleia Massart,1920 distribution limit around France or Southern British Isles, have as a rule been omitted here, albeit a few species with probable norhern limits around * Marine? Incertae sedis. the British Isles are listed here until distribution patterns are better known. The compiler would be very grateful for every correction of presumptive lapses and omittances an initiated reader could make. Diplocalium Grassé & Deflandre,1952 (™ Bicosoeca inopinatum ??,1???) * Marine? Incertae sedis. Denotations: (™) = Genotype @ = Associated to * = General note Diplomita Fromentel,1874 (™ Diplomita insignis Fromentel,1874) P.S. This list is a very unfinished manuscript. Chiefly flagellated organisms have yet been considered. This * Marine? Incertae sedis. provisional PDF-file is so far only published as an Intranet file within TMBL:s domain. Diplonema Griessmann,1913, non Berendt,1845 (Diptera), nec Greene,1857 (Coel.) = Isonema ??,1???, non Meek & Worthen,1865 (Mollusca), nec Maas,1909 (Coel.) PROTOCTISTA = Flagellamonas Skvortzow,19?? = Lackeymonas Skvortzow,19?? = Lowymonas Skvortzow,19?? = Milaneziamonas Skvortzow,19?? = Spira Skvortzow,19?? = Teixeiromonas Skvortzow,19?? = PROTISTA = Kolbeana Skvortzow,19?? * Genus incertae sedis. -
Marine Biological Laboratory) Data Are All from EST Analyses
TABLE S1. Data characterized for this study. rDNA 3 - - Culture 3 - etK sp70cyt rc5 f1a f2 ps22a ps23a Lineage Taxon accession # Lab sec61 SSU 14 40S Actin Atub Btub E E G H Hsp90 M R R T SUM Cercomonadida Heteromita globosa 50780 Katz 1 1 Cercomonadida Bodomorpha minima 50339 Katz 1 1 Euglyphida Capsellina sp. 50039 Katz 1 1 1 1 4 Gymnophrea Gymnophrys sp. 50923 Katz 1 1 2 Cercomonadida Massisteria marina 50266 Katz 1 1 1 1 4 Foraminifera Ammonia sp. T7 Katz 1 1 2 Foraminifera Ovammina opaca Katz 1 1 1 1 4 Gromia Gromia sp. Antarctica Katz 1 1 Proleptomonas Proleptomonas faecicola 50735 Katz 1 1 1 1 4 Theratromyxa Theratromyxa weberi 50200 Katz 1 1 Ministeria Ministeria vibrans 50519 Katz 1 1 Fornicata Trepomonas agilis 50286 Katz 1 1 Soginia “Soginia anisocystis” 50646 Katz 1 1 1 1 1 5 Stephanopogon Stephanopogon apogon 50096 Katz 1 1 Carolina Tubulinea Arcella hemisphaerica 13-1310 Katz 1 1 2 Cercomonadida Heteromita sp. PRA-74 MBL 1 1 1 1 1 1 1 7 Rhizaria Corallomyxa tenera 50975 MBL 1 1 1 3 Euglenozoa Diplonema papillatum 50162 MBL 1 1 1 1 1 1 1 1 8 Euglenozoa Bodo saltans CCAP1907 MBL 1 1 1 1 1 5 Alveolates Chilodonella uncinata 50194 MBL 1 1 1 1 4 Amoebozoa Arachnula sp. 50593 MBL 1 1 2 Katz lab work based on genomic PCRs and MBL (Marine Biological Laboratory) data are all from EST analyses. Culture accession number is ATTC unless noted. GenBank accession numbers for new sequences (including paralogs) are GQ377645-GQ377715 and HM244866-HM244878. -
Micro-CT 3D Imaging Reveals the Internal Structure of Three Abyssal
www.nature.com/scientificreports OPEN Micro-CT 3D imaging reveals the internal structure of three abyssal xenophyophore species (Protista, Received: 14 March 2018 Accepted: 25 July 2018 Foraminifera) from the eastern Published: xx xx xxxx equatorial Pacifc Ocean Andrew J. Gooday1, Dan Sykes2,4, Tomasz Góral2, Mikhail V. Zubkov1,5 & Adrian G. Glover 3 Xenophyophores, giant foraminifera, are distinctive members of the deep-sea megafauna that accumulate large masses of waste material (‘stercomare’) within their agglutinated tests, and organise their cells as branching strands enclosed within an organic tube (the ‘granellare’ system). Using non- destructive, three-dimensional micro-CT imaging we explored these structures in three species from the abyssal eastern Pacifc Clarion-Clipperton Zone (CCZ). In Psammina spp., the low-density stercomare occupied much of the test interior, while high-density granellare strands branched throughout the structure. In Galatheammina sp. the test comprised a mixture of stercomare and test particles, with the granellare forming a web-like system of flaments. The granellare occupied 2.8–5.1%, the stercomare 72.4–82.4%, and test particles 14.7–22.5%, of the ‘body’ volume in the two Psammina species. The corresponding proportions in Galatheammina sp. were 1.7% (granellare), 39.5% (stercomare) and 58.8% (test particles). These data provide a potential basis for estimating the contribution of xenophyophores to seafoor biomass in areas like the CCZ where they dominate the megafauna. As in most xenophyophore species, the granellare hosted huge numbers of tiny barite crystals. We speculate that these help to support the extensive granellare system, as well as reducing the cell volume and lightening the metabolic burden required to maintain it. -
The Proterozoic Fossil Record of Heterotrophic Eukaryotes
Chapter 1 The Proterozoic Fossil Record of Heterotrophic Eukaryotes SUSANNAH M. PORTER Department of Earth Science, University of California, Santa Barbara, CA 93106, USA. 1. Introduction .................................................... 1 2. Eukaryotic Tree................................................. 2 3. Fossil Evidence for Proterozoic Heterotrophs ........................... 4 3.1. Opisthokonts ............................................... 4 3.2. Amoebozoa................................................ 5 3.3. Chromalveolates............................................ 7 3.4. Rhizaria................................................... 9 3.5. Excavates.................................................. 10 3.6. Summary.................................................. 10 4. Why Are Heterotrophs Rare in Proterozoic Rocks?........................ 12 5. Conclusions.................................................... 14 Acknowledgments.................................................. 15 References....................................................... 15 1. INTRODUCTION Nutritional modes of eukaryotes can be divided into two types: autotrophy, where the organism makes its own food via photosynthesis; and heterotrophy, where the organism gets its food from the environment, either by taking up dissolved organics (osmotrophy), or by ingesting particulate organic matter (phagotrophy). Heterotrophs dominate modern eukaryotic Neoproterozoic Geobiology and Paleobiology, edited by Shuhai Xiao and Alan Jay Kaufman, © 2006 Springer. Printed -
Radiolarian Tests As Microhabitats for Novel Benthic
Author's Accepted Manuscript Radiolarian tests as microhabitats for novel benthic foraminifera: Observations from the abyssal eastern equatorial pacific (clarion– Clipperton fracture zone) Aurélie Goineau, Andrew J. Gooday www.elsevier.com/locate/dsri PII: S0967-0637(15)00085-0 DOI: http://dx.doi.org/10.1016/j.dsr.2015.04.011 Reference: DSRI2487 To appear in: Deep-Sea Research I Received date: 4 February 2015 Revised date: 20 April 2015 Accepted date: 24 April 2015 Cite this article as: Aurélie Goineau, Andrew J. Gooday, Radiolarian tests as microhabitats for novel benthic foraminifera: Observations from the abyssal eastern equatorial pacific (clarion–Clipperton fracture zone), Deep-Sea Research I, http://dx.doi.org/10.1016/j.dsr.2015.04.011 This is a PDF file of an unedited manuscript that has been accepted for publication. As a service to our customers we are providing this early version of the manuscript. The manuscript will undergo copyediting, typesetting, and review of the resulting galley proof before it is published in its final citable form. Please note that during the production process errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain. Radiolarian tests as microhabitats for novel benthic foraminifera: observations from the abyssal eastern equatorial Pacific (Clarion–Clipperton Fracture Zone). Aurélie Goineau*, Andrew J. Gooday National Oceanography Centre, University of Southampton, Waterfront Campus, European Way, Southampton SO14 3ZH, United Kingdom * Corresponding author: [email protected] – +44 (0) 23 8059 6333 1 1. Introduction The work of H.L. Sanders and R.R. Hessler in the 1960s led to a realisation that the metazoan macrofauna (>300 µm fraction) inhabiting sedimented deep-sea habitats are much more diverse than had been realised (Hessler and Sanders, 1967; Sanders and Hessler, 1969).