15.2 the Diversity of Ocean Life

Total Page:16

File Type:pdf, Size:1020Kb

15.2 the Diversity of Ocean Life Section 15.2 15.2 The Diversity of Ocean Life 1 FOCUS Section Objectives 15.5 Recognize how marine Key Concepts Vocabulary Reading Strategy organisms can be classified. How can marine ◆ plankton Building Vocabulary Copy the table below. organisms be classified? ◆ phytoplankton As you read, add definitions and examples to 15.6 Differentiate between complete the table. plankton and nekton. What is the difference ◆ zooplankton between plankton and ◆ nekton 15.7 Describe the area of the ocean Definitions Examples nekton? ◆ benthos Plankton: organisms that drift with in which most benthic In which area of the ◆ photic zone ocean currents bacteria organisms live. ocean can most benthos ◆ intertidal zone organisms be found Phytoplankton: a. ? b. ? 15.8 List the factors used to divide ◆ neritic zone living? the ocean into marine zones. ◆ oceanic zone Zooplankton: c. ? d. ? What factors are used to ◆ pelagic zone divide the ocean into Nekton: e. ? f. ? ◆ benthic zone marine life zones? Benthos: g. ? h. ? ◆ abyssal zone Reading Focus Build Vocabulary L2 Concept Map Have students make a concept map using the term marine life A wide variety of organisms inhabit the marine environment. These zones as the starting point that connects organisms range in size from microscopic bacteria and algae to the to the following three terms: availability largest organisms alive today—blue whales, which are as long as three of sunlight, distance from shore, and depth. Figure 7 Plankton are organisms buses lined up end to end. Marine biologists have identified over Students should use the following terms that drift with ocean currents. 250,000 marine species. This number is constantly increasing as new A This photo shows a variety of organisms are discovered. to complete their concept map: pelagic phytoplankton from the Atlantic zone, photic zone, oceanic zone, benthic Ocean. B The zooplankton shown Most marine organisms live within the sunlit surface waters. Strong zone, abyssal zone, intertidal zone, and here include copepods and the sunlight supports photosynthesis by marine algae. Algae either directly larval stages of other common or indirectly provide food for the majority of organisms. All marine neritic zone. marine organisms. algae live near the surface because they need sunlight to survive. Most L2 marine animals also live near the surface because this is where they Reading Strategy A a. plankton capable of photosynthesis can find food. b. microscopic algae c. animal plankton Classification of Marine Organisms d. larval fish Marine organisms can be classified according to where they live e. organisms capable of moving and how they move. They can be classified as either plankton (floaters) independently of ocean currents or nekton (swimmers). All other organisms are benthos, or bottom f. fish B dwellers. g. organisms living on or near the ϭ ocean bottom Plankton Plankton (planktos wandering) include all organ- h. marine worms isms—algae, animals, and bacteria—that drift with ocean currents. Just because plankton drift does not mean they are unable to swim. 2 INSTRUCT Many plankton can swim but either move very weakly or move only vertically. Classification of Marine Animals 428 Chapter 15 Build Reading Literacy L2 Refer to p. 362D in Chapter 13, which provides the guidelines for this reading strategy. Use Prior Knowledge Have students write the names of several ocean organisms they know about or have heard about. Next to each name, have students write a description of the organism, where it lives, and how it obtains food. After students have read the section, have them review their lists and make corrections, if necessary. Logical 428 Chapter 15 L1 Among plankton, the algae that undergo photosynthesis are called Figure 8 Nekton includes all Use Visuals animals capable of moving Figure 7 Have students examine the phytoplankton. Most phytoplankton, such as diatoms, are micro- independently of ocean currents. scopic. Animal plankton, are called zooplankton. Zooplankton include A This squid can use propulsion to two photographs. Explain that the the larval stages of many marine organisms such as fish, sea stars, lobsters, move through the water. B This phytoplankton organisms shown in school of grunts swims through photograph A include dinoflagellates and crabs. Figure 7 shows members of each group. the water with ease. Inferring Why do you think and diatoms. Explain that long narrow Nekton Nekton (nektos ϭ swimming) include all animals some organisms, such as fish, projections and other distinctive shapes capable of moving independently of the ocean currents, by swim- are classified as plankton during contribute to the ability of these some stages of their lives and ming or other means of propulsion. Nekton are able to determine nekton during other stages? organisms to stay afloat. Remind their position within the ocean and in many cases complete long students that diatoms have shell-like migrations. Nekton include most adult fish and squid, marine mam- A tests. Ask: What may happen to these mals, and marine reptiles. Figure 8 shows examples of nekton. hard parts after these organisms die? Fish may appear to exist everywhere in the oceans, but they are (decay, or fall to the bottom and contribute more abundant near continents and islands and in colder waters. Some to the sediment layer) Explain that the fish, such as salmon, swim upstream in fresh water rivers to spawn. zooplankton shown in photograph B Many eels do just the reverse, growing to maturity in fresh water and are larval and adult copepods. Inform then swimming out of the streams to breed in the depths of the ocean. students that copepods are small B crustaceans (related to crab and shrimp) Benthos The term benthos (benthos = bottom) describes on which many larger organisms depend organisms living on or in the ocean bottom. Figure 9 shows some for food. Ask: What are the likely examples of benthos organisms. The shallow coastal ocean floor con- functions of the appendages on tains a wide variety of physical conditions and nutrient levels. Most the larger specimens shown in the benthos organisms can be found living in this area. Shallow coastal photograph? (feeding and swimming) areas are the only locations where large marine algae, often called sea- Visual, Logical weeds, are found attached to the bottom. These are the only areas of L2 the seafloor that receive enough sunlight for the algae to survive. Build Science Skills Throughout most of the deeper parts of the seafloor, animals live Classifying Show students photographs in perpetual darkness, where photosynthesis cannot occur. They must or dried or preserved specimens of feed on each other or on whatever nutrients fall from the productive organisms to classify as plankton, surface waters. The deep-sea bottom is an environment of coldness, nekton, or benthos. Ask students to stillness, and darkness. Under these conditions, life progresses slowly. Figure 9 Benthos describes explain the reasoning behind their organisms living on or in the classification decisions. (Possible answers: Organisms that live in the deep sea usually are widely distributed ocean bottom. A Sea star because physical conditions vary little on the deep-ocean floor. B Coral crab Plankton are microscopic or very small. Phytoplankton have green pigment and show the ability to photosynthesize. Zooplankton have small swimming A B appendages; examples include diatoms, dinoflagellates, copepods, jellyfish, larval fish. Nekton have swimming appendages, are large and strong enough to swim against ocean currents; examples include adult fish, dolphins, whales, squid. Benthos live on the ocean bottom; examples include sea stars, most crabs, sea anemones, sea snails, clams, mussels.) Visual, Logical Ocean Water and Ocean Life 429 Customize for Inclusion Students Behaviorally Disordered Have students board or butcher paper. Have students add work together to create a two-dimensional labeled organisms to appropriate areas of their model of ocean life zones on the classroom model. Students can make their own drawings bulletin board. Students can use Figure 10 as of organisms, cut out photographs from old a starting point. Challenge students to draw or magazines, or photocopy illustrations from Answer to . paint and label continental shelf, continental books. slope, ocean basin, photic zone, aphotic zone, Figure 8 As larvae, fish are not able and benthic zone on a large piece of poster to move against ocean currents, they drift with the current. As adults, fish are able to swim and move independ- ently of ocean currents. Ocean Water and Ocean Life 429 Section 15.2 (continued) Marine Life Zones The distribution of marine organisms is affected by the chemistry, Marine Life Zones physics, and geology of the oceans. Marine organisms are influenced Use Community by a variety of physical factors. Three factors are used to divide the L2 For: Links on marine ecosystems Resources Visit: www.SciLinks.org ocean into distinct marine life zones: the availability of sunlight, the Aquarium Field Trip Take students Web Code: cjn-5152 distance from shore, and the water depth. Figure 10 shows the dif- on a field trip to a local public aquarium ferent zones in which marine life can be found. or museum with ocean life exhibits. Alternatively, students could visit a Availability of Sunlight The upper part of the ocean into ϭ pet store that specializes in saltwater which sunlight penetrates is called the photic zone (photos light). aquariums. Have students select one or The clarity of seawater is affected by many factors, such as the amount more organisms they observe during of plankton, suspended sediment, and decaying organic particles in their visit and write a short paper the water. In addition, the amount of sunlight varies with atmospheric describing it. Encourage students to conditions, time of day, season of the year, and latitude. classify each of their organisms as The euphotic zone is the portion of the photic zone near the sur- belonging to plankton, nekton, or face where light is strong enough for photosynthesis to occur.
Recommended publications
  • Continental Shelf the Last Maritime Zone
    Continental Shelf The Last Maritime Zone The Last Maritime Zone Published by UNEP/GRID-Arendal Copyright © 2009, UNEP/GRID-Arendal ISBN: 978-82-7701-059-5 Printed by Birkeland Trykkeri AS, Norway Disclaimer Any views expressed in this book are those of the authors and do not necessarily reflect the views or policies of UNEP/GRID-Arendal or contributory organizations. The designations employed and the presentation of material in this book do not imply the expression of any opinion on the part of the organizations concerning the legal status of any country, territory, city or area of its authority, or deline- ation of its frontiers and boundaries, nor do they imply the validity of submissions. All information in this publication is derived from official material that is posted on the website of the UN Division of Ocean Affairs and the Law of the Sea (DOALOS), which acts as the Secretariat to the Com- mission on the Limits of the Continental Shelf (CLCS): www.un.org/ Depts/los/clcs_new/clcs_home.htm. UNEP/GRID-Arendal is an official UNEP centre located in Southern Norway. GRID-Arendal’s mission is to provide environmental informa- tion, communications and capacity building services for information management and assessment. The centre’s core focus is to facili- tate the free access and exchange of information to support decision making to secure a sustainable future. www.grida.no. Continental Shelf The Last Maritime Zone Continental Shelf The Last Maritime Zone Authors and contributors Tina Schoolmeester and Elaine Baker (Editors) Joan Fabres Øystein Halvorsen Øivind Lønne Jean-Nicolas Poussart Riccardo Pravettoni (Cartography) Morten Sørensen Kristina Thygesen Cover illustration Alex Mathers Language editor Harry Forster (Interrelate Grenoble) Special thanks to Yannick Beaudoin Janet Fernandez Skaalvik Lars Kullerud Harald Sund (Geocap AS) Continental Shelf The Last Maritime Zone Foreword During the past decade, many coastal States have been engaged in peacefully establish- ing the limits of their maritime jurisdiction.
    [Show full text]
  • Diversity and Community Structure of Pelagic Cnidarians in the Celebes and Sulu Seas, Southeast Asian Tropical Marginal Seas
    Deep-Sea Research I 100 (2015) 54–63 Contents lists available at ScienceDirect Deep-Sea Research I journal homepage: www.elsevier.com/locate/dsri Diversity and community structure of pelagic cnidarians in the Celebes and Sulu Seas, southeast Asian tropical marginal seas Mary M. Grossmann a,n, Jun Nishikawa b, Dhugal J. Lindsay c a Okinawa Institute of Science and Technology Graduate University (OIST), Tancha 1919-1, Onna-son, Okinawa 904-0495, Japan b Tokai University, 3-20-1, Orido, Shimizu, Shizuoka 424-8610, Japan c Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Yokosuka 237-0061, Japan article info abstract Article history: The Sulu Sea is a semi-isolated, marginal basin surrounded by high sills that greatly reduce water inflow Received 13 September 2014 at mesopelagic depths. For this reason, the entire water column below 400 m is stable and homogeneous Received in revised form with respect to salinity (ca. 34.00) and temperature (ca. 10 1C). The neighbouring Celebes Sea is more 19 January 2015 open, and highly influenced by Pacific waters at comparable depths. The abundance, diversity, and Accepted 1 February 2015 community structure of pelagic cnidarians was investigated in both seas in February 2000. Cnidarian Available online 19 February 2015 abundance was similar in both sampling locations, but species diversity was lower in the Sulu Sea, Keywords: especially at mesopelagic depths. At the surface, the cnidarian community was similar in both Tropical marginal seas, but, at depth, community structure was dependent first on sampling location Marginal sea and then on depth within each Sea. Cnidarians showed different patterns of dominance at the two Sill sampling locations, with Sulu Sea communities often dominated by species that are rare elsewhere in Pelagic cnidarians fi Community structure the Indo-Paci c.
    [Show full text]
  • Understanding the Sexual Recruitment of One of the Oldest and Largest Organisms on Earth, the Seagrass Posidonia Oceanica
    RESEARCH ARTICLE Understanding the sexual recruitment of one of the oldest and largest organisms on Earth, the seagrass Posidonia oceanica 1☯ 2☯ 1☯ Laura Guerrero-MeseguerID *, Carlos Sanz-LaÂzaro , Arnaldo MarõÂn 1 Departamento de EcologõÂa e HidrologõÂa. Facultad de BiologõÂa, Universidad de Murcia, Campus de Espinardo, Murcia, Spain, 2 Departamento de EcologõÂa, PabelloÂn 13, Universidad de Alicante, Alicante, Spain ☯ These authors contributed equally to this work. * [email protected] a1111111111 Abstract a1111111111 a1111111111 The seagrass Posidonia oceanica is considered one of the oldest and largest living organ- a1111111111 isms on Earth. Notwithstanding, given the difficulty of monitoring its fruits and seeds in the a1111111111 field, the development of P. oceanica during its sexual recruitment is not completely under- stood. We studied the stages of development of P. oceanica seeds from their dispersion in the fruit interior to their settlement in sediment through histological, ultrastructural and meso- cosm experiments. P. oceanica sexual recruitment can be divided into three main stages OPEN ACCESS that focus on maximising photosynthesis and anchoring the seedlings to the sediment. In Citation: Guerrero-Meseguer L, Sanz-LaÂzaro C, the first stage (fruit dispersion), seeds perform photosynthesis while being transported MarõÂn A (2018) Understanding the sexual recruitment of one of the oldest and largest inside the fruit along the sea surface. In the second stage (seed adhesion), seeds develop organisms on Earth, the seagrass Posidonia adhesive microscopic hairs that cover the primary and secondary roots and favour seed oceanica. PLoS ONE 13(11): e0207345. https://doi. adhesion to the substrate. In the last stage (seedling anchorage), roots attach the seedlings org/10.1371/journal.pone.0207345 to the substrate by orienting them towards the direction of light to maximise photosynthesis.
    [Show full text]
  • Methane Cold Seeps As Biological Oases in the High‐
    LIMNOLOGY and Limnol. Oceanogr. 00, 2017, 00–00 VC 2017 The Authors Limnology and Oceanography published by Wiley Periodicals, Inc. OCEANOGRAPHY on behalf of Association for the Sciences of Limnology and Oceanography doi: 10.1002/lno.10732 Methane cold seeps as biological oases in the high-Arctic deep sea Emmelie K. L. A˚ strom€ ,1* Michael L. Carroll,1,2 William G. Ambrose, Jr.,1,2,3,4 Arunima Sen,1 Anna Silyakova,1 JoLynn Carroll1,2 1CAGE - Centre for Arctic Gas Hydrate, Environment and Climate, Department of Geosciences, UiT The Arctic University of Norway, Tromsø, Norway 2Akvaplan-niva, FRAM – High North Research Centre for Climate and the Environment, Tromsø, Norway 3Division of Polar Programs, National Science Foundation, Arlington, Virginia 4Department of Biology, Bates College, Lewiston, Maine Abstract Cold seeps can support unique faunal communities via chemosynthetic interactions fueled by seabed emissions of hydrocarbons. Additionally, cold seeps can enhance habitat complexity at the deep seafloor through the accretion of methane derived authigenic carbonates (MDAC). We examined infaunal and mega- faunal community structure at high-Arctic cold seeps through analyses of benthic samples and seafloor pho- tographs from pockmarks exhibiting highly elevated methane concentrations in sediments and the water column at Vestnesa Ridge (VR), Svalbard (798 N). Infaunal biomass and abundance were five times higher, species richness was 2.5 times higher and diversity was 1.5 times higher at methane-rich Vestnesa compared to a nearby control region. Seabed photos reveal different faunal associations inside, at the edge, and outside Vestnesa pockmarks. Brittle stars were the most common megafauna occurring on the soft bottom plains out- side pockmarks.
    [Show full text]
  • Coastal and Marine Ecological Classification Standard (2012)
    FGDC-STD-018-2012 Coastal and Marine Ecological Classification Standard Marine and Coastal Spatial Data Subcommittee Federal Geographic Data Committee June, 2012 Federal Geographic Data Committee FGDC-STD-018-2012 Coastal and Marine Ecological Classification Standard, June 2012 ______________________________________________________________________________________ CONTENTS PAGE 1. Introduction ..................................................................................................................... 1 1.1 Objectives ................................................................................................................ 1 1.2 Need ......................................................................................................................... 2 1.3 Scope ........................................................................................................................ 2 1.4 Application ............................................................................................................... 3 1.5 Relationship to Previous FGDC Standards .............................................................. 4 1.6 Development Procedures ......................................................................................... 5 1.7 Guiding Principles ................................................................................................... 7 1.7.1 Build a Scientifically Sound Ecological Classification .................................... 7 1.7.2 Meet the Needs of a Wide Range of Users ......................................................
    [Show full text]
  • The Distributions Of, and Relationship Between, 3He and Nitrate in Eddies
    ARTICLE IN PRESS Deep-Sea Research II 55 (2008) 1389– 1397 Contents lists available at ScienceDirect Deep-Sea Research II journal homepage: www.elsevier.com/locate/dsr2 The distributions of, and relationship between, 3He and nitrate in eddies W.J. Jenkins Ã, D.J. McGillicuddy Jr., D.E. Lott III Department of Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA article info abstract Article history: We present and discuss the distribution of 3He and its relationship to nutrients in two eddies (cyclone Accepted 4 February 2008 C1 and anticyclone A4) with a view towards examining eddy-related mechanisms whereby nutrients Available online 9 May 2008 are transported from the upper 200–300 m into the euphotic zone of the Sargasso Sea. The different Keywords: behavior of these tracers in the euphotic zone results in changes in their distributions and relationships Biogeochemical tracers that may provide important clues as to the nature of physical and biological processes involved. Tracer techniques The cyclonic eddy (C1) is characterized by substantial 3He excesses within the euphotic zone. The 3 He distribution of this excess 3He is strongly suggestive of both past and recent ongoing deep-water Eddies injection into the euphotic zone. Crude mass balance calculations suggest that an average of Atlantic Ocean approximately 1.470.7 mol mÀ2 of nitrate has been introduced into the euphotic zone of eddy C1, Sargasso Sea consistent with the integrated apparent oxygen utilization anomaly in the aphotic zone below. The 3 He–NO3 relationship within the eddy deviates substantially from the linear thermocline trend, suggestive of incomplete drawdown of nutrients and/or substantial mixing between euphotic and aphotic zone waters.
    [Show full text]
  • Grade 3 Unit 2 Overview Open Ocean Habitats Introduction
    G3 U2 OVR GRADE 3 UNIT 2 OVERVIEW Open Ocean Habitats Introduction The open ocean has always played a vital role in the culture, subsistence, and economic well-being of Hawai‘i’s inhabitants. The Hawaiian Islands lie in the Pacifi c Ocean, a body of water covering more than one-third of the Earth’s surface. In the following four lessons, students learn about open ocean habitats, from the ocean’s lighter surface to the darker bottom fl oor thousands of feet below the surface. Although organisms are scarce in the deep sea, there is a large diversity of organisms in addition to bottom fi sh such as polycheate worms, crustaceans, and bivalve mollusks. They come to realize that few things in the open ocean have adapted to cope with the increased pressure from the weight of the water column at that depth, in complete darkness and frigid temperatures. Students fi nd out, through instruction, presentations, and website research, that the vast open ocean is divided into zones. The pelagic zone consists of the open ocean habitat that begins at the edge of the continental shelf and extends from the surface to the ocean bottom. This zone is further sub-divided into the photic (sunlight) and disphotic (twilight) zones where most ocean organisms live. Below these two sub-zones is the aphotic (darkness) zone. In this unit, students learn about each of the ocean zones, and identify and note animals living in each zone. They also research and keep records of the evolutionary physical features and functions that animals they study have acquired to survive in harsh open ocean habitats.
    [Show full text]
  • THE CASE AGAINST Marine Mammals in Captivity Authors: Naomi A
    s l a m m a y t T i M S N v I i A e G t A n i p E S r a A C a C E H n T M i THE CASE AGAINST Marine Mammals in Captivity The Humane Society of the United State s/ World Society for the Protection of Animals 2009 1 1 1 2 0 A M , n o t s o g B r o . 1 a 0 s 2 u - e a t i p s u S w , t e e r t S h t u o S 9 8 THE CASE AGAINST Marine Mammals in Captivity Authors: Naomi A. Rose, E.C.M. Parsons, and Richard Farinato, 4th edition Editors: Naomi A. Rose and Debra Firmani, 4th edition ©2009 The Humane Society of the United States and the World Society for the Protection of Animals. All rights reserved. ©2008 The HSUS. All rights reserved. Printed on recycled paper, acid free and elemental chlorine free, with soy-based ink. Cover: ©iStockphoto.com/Ying Ying Wong Overview n the debate over marine mammals in captivity, the of the natural environment. The truth is that marine mammals have evolved physically and behaviorally to survive these rigors. public display industry maintains that marine mammal For example, nearly every kind of marine mammal, from sea lion Iexhibits serve a valuable conservation function, people to dolphin, travels large distances daily in a search for food. In learn important information from seeing live animals, and captivity, natural feeding and foraging patterns are completely lost.
    [Show full text]
  • Marine Nature Conservation in the Pelagic Environment: a Case for Pelagic Marine Protected Areas?
    Marine nature conservation in the pelagic environment: a case for pelagic Marine Protected Areas? Susan Gubbay September 2006 Contents Contents......................................................................................................................................... 1 Executive summary....................................................................................................................... 2 1 Introduction........................................................................................................................... 4 2 The pelagic environment....................................................................................................... 4 2.1 An overview...................................................................................................................... 4 2.2 Characteristics of the pelagic environment ....................................................................... 5 2.3 Spatial and temporal structure in the pelagic environment ............................................... 6 2.4 Marine life....................................................................................................................... 10 3 Biodiversity conservation in the pelagic environment........................................................ 12 3.1 Environmental concerns.................................................................................................. 12 3.2 Legislation, policy and management tools...................................................................... 15
    [Show full text]
  • Respiration in the Mesopelagic and Bathypelagic Zones of the Oceans
    CHAPTER 10 Respiration in the mesopelagic and bathypelagic zones of the oceans Javier Arístegui1, Susana Agustí2, Jack J. Middelburg3, and Carlos M. Duarte2 1 Facultad de Ciencias del Mar, Universidad de las Palmas de Gran Canaria, Spain 2 IMEDEA (CSIC–UIB), Spain 3 Netherlands Institute of Ecology, The Netherlands Outline In this chapter the mechanisms of transport and remineralization of organic matter in the dark water-column and sediments of the oceans are reviewed. We compare the different approaches to estimate respiration rates, and discuss the discrepancies obtained by the different methodologies. Finally, a respiratory carbon budget is produced for the dark ocean, which includes vertical and lateral fluxes of organic matter. In spite of the uncertainties inherent in the different approaches to estimate carbon fluxes and oxygen consumption in the dark ocean, estimates vary only by a factor of 1.5. Overall, direct measurements of respiration, as well as − indirect approaches, converge to suggest a total dark ocean respiration of 1.5–1.7 Pmol C a 1. Carbon mass − balances in the dark ocean suggest that the dark ocean receives 1.5–1.6 Pmol C a 1, similar to the estimated respiration, of which >70% is in the form of sinking particles. Almost all the organic matter (∼92%) is remineralized in the water column, the burial in sediments accounts for <1%. Mesopelagic (150–1000 m) − − respiration accounts for ∼70% of dark ocean respiration, with average integrated rates of 3–4 mol C m 2 a 1, − − 6–8 times greater than in the bathypelagic zone (∼0.5 mol C m 2 a 1).
    [Show full text]
  • The Anthropocene Biosphere
    ANR0010.1177/2053019615591020The Anthropocene ReviewWilliams et al. 591020research-article2015 Review The Anthropocene Review 1 –24 The Anthropocene biosphere © The Author(s) 2015 Reprints and permissions: sagepub.co.uk/journalsPermissions.nav DOI: 10.1177/2053019615591020 anr.sagepub.com Mark Williams,1 Jan Zalasiewicz,1 PK Haff,2 Christian Schwägerl,3 Anthony D Barnosky4,5,6 and Erle C Ellis7 Abstract The geological record preserves evidence for two fundamental stages in the evolution of Earth’s biosphere, a microbial stage from ~3.5 to 0.65 Ga, and a metazoan stage evident by c. 650 Ma. We suggest that the modern biosphere differs significantly from these previous stages and shows early signs of a new, third stage of biosphere evolution characterised by: (1) global homogenisation of flora and fauna; (2) a single species (Homo sapiens) commandeering 25–40% of net primary production and also mining fossil net primary production (fossil fuels) to break through the photosynthetic energy barrier; (3) human-directed evolution of other species; and (4) increasing interaction of the biosphere with the technosphere (the global emergent system that includes humans, technological artefacts, and associated social and technological networks). These unique features of today’s biosphere may herald a new era in the planet’s history that could persist over geological timescales. Keywords biosphere, evolution, global ecosystem, neobiotic species, planetary state, production and consumption, technosphere Introduction Humans transport organisms around the globe (McNeely, 2001 and references therein), con- struct unique agricultural and urban ‘anthromes’ for organisms to live in (e.g. Ellis, 2013; Ellis et al., 2012, 2013a, 2013b), and have concentrated biomass into a particular set of plants and animals (e.g.
    [Show full text]
  • MARINE ENVIRONMENTS Teaching Module for Grades 6-12
    MARINE ENVIRONMENTS Teaching Module for Grades 6-12 Dear Educator, We are pleased to present you with the first in a series of teaching and learning modules developed by the DEEPEND (Deep-Pelagic Nekton Dynamics) consortium and their consultants. DEEPEND is a research network focusing primarily on the pelagic zone of the Gulf of Mexico, therefore the majority of the lessons will be based around this topic. Whenever possible, the lessons will focus specifically on events of the Gulf of Mexico or work from the DEEPEND scientists. All modules in this series aim to engage students in grades 6 through 12 in STEM disciplines, while promoting student learning of the marine environment. We hope these lessons enable teachers to address student misconceptions and apprehensions regarding the unique organisms and properties of marine ecosystems. We intend for these modules to be a guide for teaching. Teachers are welcome to use the lessons in any order they wish, use just portions of lessons, and may modify the lessons as they wish. Furthermore, educators may share these lessons with other school districts and teachers; however, please do not receive monetary gain for lessons in any of the modules. Moreover, please provide credit to photographers and authors whenever possible. This first module focuses on the marine environment in general including biological, chemical, and physical properties of the water column. We have provided a variety of activities and extensions within this module such that lessons can easily be adapted for various grade and proficiency levels. Given that education reform strives to incorporate authentic science experiences, many of these lessons encourage exploration and experimentation to encourage students to think and act like a scientist.
    [Show full text]