The Open Ocean. College of Marine Sciences, Shanghai Ocean University

Similar documents
OCEANOGRAPHY Chapter 13

Marine lifestyles and relationships

4/28/2013. Transmission of Light in Seawater. Color in the Ocean Color of ocean ranges from deep blue to yellow-green Factors Turbidity from runoff

Productivity and fisheries. Energy flow. Biological pyramids. Why study production processes?

Taxonomy. Classification of Marine Organisms 11/7/2012. CH 12 Marine Life and the Marine Environment

Ecology. Limiting factors. Introduction to Marine Ecology. Ecological communities and ecosystems

Essentials of Oceanography Eleventh Edition

biology Slide 1 of 39 End Show Copyright Pearson Prentice Hall

4-4 Aquatic Ecosystems

Ecosystem refers to the organism which live in a particular area, the relationship between them, and their physical environment.

What factors affect life in aquatic ecosystems?

Marine Microbial Processes

Lesson Overview 4.5 Aquatic Ecosystems

ECOLOGY Energy Flow Packet 2 of 4

Includes the coastal zone and the pelagic zone, the realm of the oceanographer. I. Ocean Circulation

Producers. living systems need energy to function. autotrophs. Sunlight is the main energy source for life on Earth.

Aquatic Communities Aquatic communities can be classified as freshwater

SUNLIGHT & OCEAN ZONATION

Ocean Water. Properties of Ocean Water. Section 21.1 Objectives. Chapter 21. Chapter 21, Section 1

OCN201 Fall Exam 3 (Biological Secton / Final) 75 Points

21.1 Properties of Ocean Water. Section 21.1 Objectives

Marine Life. Communities

3 2 Energy Flow Slide 1 of 41

(Brief) History of Life

Biology. Slide 1 of 41. End Show. Copyright Pearson Prentice Hall

10/17/ Energy Flow. Producers. Where does the energy for life processes come from?

Continued from Lecture 20a

Honors Biology Unit 5 Chapter 34 THE BIOSPHERE: AN INTRODUCTION TO EARTH S DIVERSE ENVIRONMENTS

Biology. Slide 1 of 41. End Show. Copyright Pearson Prentice Hall

Classification of systems. Aquatic Ecosystems. Lakes 9/9/2013. Chapter 25

Energy. Raw materials to make building blocks of life. From sun or chemicals. From food

Marine Ecology. Biotic The biotic factors are the interactions among living organisms. Zonation Two major divisions in the marine world.

Ecosystems and Food Webs

Biological Oceanography

Ch. 7 Aquatic Ecology

SUSTAINING ECOSYSTEMS

Ecosystems and the Biosphere: Energy Flow Through the Ecosystem and the Recycling of Matter

Chapter 5 AQUATIC BIOMES

Lab: Modeling Ecosystems Virtual Lab B I O L O G Y : I n t e r a c t i o n s i n E c o s y s t e m s

What Keeps Us and Other Organisms Alive?

Notes: Ocean Environments and Food Webs. Source: CMAPP

The Energy of Life Chapter 3

Energy Flow Through an Ecosystem:

Think About It (not on notes)

Ecosystem consists of the organism which live in a particular area, the relationship between them, and their physical environment.

CHAPTER 2: PRINCIPLES OF ECOLOGY 11/29/16

California Current Ecosystem Plankton Food Web

Class XII Chapter 14 Ecosystem Biology

1. According to the serial endosymbiosis theory, prokaryotes developed when eukaryotes lost their organelles.

3 2 Energy Flow. Slide 1 of 41. Copyright Pearson Prentice Hall

Biology Slide 1 of 41

Aquatic respiration and ocean metabolism

Climate: describes the average condition, including temperature and precipitation, over long periods in a given area

microzooplankton ( µm, e.g. ciliates); mesozooplankton (200 µm-20 mm, e.g. calanoid copepods); macrozooplankton (2-20 cm, e.g.

9 th -12 th Grade Whale Watching Adventure Packet

The Dead Zone. Use the notes provided (attached to this sheet) to answer the following questions.

Lesson 21: Marine Ecosystems

Guided Notes Unit 3B: Matter and Energy

Freshwater ecosystems

This article is provided courtesy of the American Museum of Natural History.

4/13/2015. The Biosphere

Chapter 6. Aquatic Biodiversity. Chapter Overview Questions

Marine Processes and Ecology

California Current Ecosystem Plankton Food Web

BIOLOGY NOTES. Ecology is the study of how organisms interact with each other and their environment

Ch 3 - The Biosphere. 3.1 What is Ecology?

Ecology: Chapters Worksheet

Today: Dinner Time! Yum Yum

AP Environmental Science

LIMNOLOGY. Inland Water Ecosystems. JACOB KALFF McGill University. Prentice Hall. Upper Saddle River, New Jersey 07458

Part IV Living World

aerobic cellular respiration a process by which organisms convert sugar into usable energy (SRB, IG)

What is ECOLOGY? The study of the biotic and abiotic factors in an environment and their interactions.

Life in Water. Chapter 3

populations and human systems in marine ecosystem models

ECOSYSTEMS. Follow along in chapter 54. *Means less important

Ecosystems. Trophic relationships determine the routes of energy flow and chemical cycling in ecosystems.

Relationships in Ecosystems

What is Ecology? Abiotic (non-living) Biotic (living)

Chapter Concepts LIFE IN WATER. The Hydrologic Cycle. The Hydrologic Cycle

The Biosphere Chapter 3. What Is Ecology? Section 3-1

Part I: Salish Sea Introduction. Review:

Chapter 3: Communities, Biomes, and Ecosystems

The Ecology of Tropical Lakes and Rivers

Keystone Biology Remediation B4: Ecology

1. Global Climate. Latitude and Sunlight Intensity 12/4/2014. Chapter 52: Introduction to Ecology and the Biosphere. 1.

Production and Life OCEA 101

Multiple Choice. Name Class Date

Ecosystem Ecology: Part 1. September 22, 2014 Mr. Alvarez

Biology Ecology Unit Chapter 2 Study Guide

Unit 2: Ecology. Chapters 2: Principles of Ecology

Biology Chapter Two. Principles of Ecology

Ecology the scientific study of interactions between different organisms and between organisms and their environment or surroundings

Ecology. Climate. Global Climate. Chapter 52: Introduction to Ecology and the Biosphere

Summary. 3 1 What Is Ecology? 3 2 Energy Flow. Name Class Date

Food/Energy Web Student Pages 1

Today: Dinner Time! Yum Yum. Primary Producers = base of food web

6/27/11. Aquatic Community Ecology (BIOL 312) Summer I. Ecological Principles. What is an ecological community? Ecological Principles

Chapter 22: Energy in the Ecosystem

Nutrient Cycling. Hydrologic (Water) Cycle. Nitrogen Cycle: Atmospheric Gases

Transcription:

The Open Ocean

Regions of the Open Sea Beyond the shallow coastal seas over the continental shelves (neritic zone) lies the open ocean (oceanic zone). The photic zone is the layer that receives enough sunlight for phytoplankton to survive. The photic zone roughly corresponds to the epipelagic zone, a term used more in reference to the location of pelagic animals in the upper 200 meters of the ocean. Below this is the aphotic zone, which extends to the ocean bottom. In this zone, light rapidly disappears until the environment is totally dark.

Life in the Open Sea Two groups of organisms inhabit the oceanic zone: plankton and nekton. GLOSSARY The plankton are a diverse group of organisms that live in the water column of large bodies of water and that cannot swim against a current. They provide a crucial source of food to many large aquatic organisms, such as fish and whales. The nekton are species with ability to swim strongly against ocean currents, they are restricted to the large, muscular, streamlined, higher consumers among the animals, such as tuna and other pelagic fishes and whales.

Classification of plankton The two most familiar kinds of plankton are phytoplankton and zooplankton. Phytoplankton are primary producers. Zooplankton are the heterotrophic eukaryotic microbes and those animals that are so small or are such weak swimmers that their distribution in the sea is determined by ocean currents. Seston are particles, living or dead, suspended in seawater. Tripton are particles of dead organic matter suspended in seawater; largely synonymous with detritus and POM (particulate organic matter). Holoplankton are organisms that are planktonic throughout their life cycles. Meroplankton are planktonic stages of an organism that is benthic or nektonic at other stages in its life history. Neuston are plankton that live at or near the surface of the ocean. GLOSSARY

Size of plankton Macroplankton were those organisms that were visible to the naked eye and generally exceeded 1 millimeter. Microplankton were small plankton that could be caught with standard plankton

Life History of Plankton Seston are particles, living or dead, suspended in seawater. Tripton are particles of dead organic matter suspended in seawater; largely synonymous with detritus and POM (particulate organic matter). Holoplankton are organisms that are planktonic throughout their life cycles. Meroplankton are planktonic stages of an organism that is benthic or nektonic at other stages in its life history. Neuston are plankton that live at or near the surface of the ocean. GLOSSARY

Plankton Migration Many open-ocean zooplankton make daily migrations from the surface of the sea to depths of nearly 1600 m. Some marine biologists believe that these movements take advantage of the benefits of feeding on the phytoplankton that live only in the photic zone and reduce to some extent the threat of predation by plankton-eating fishes, which are also more abundant in the epipelagic zone.

Cnidarian Zooplankton The largest members of the plankton are jellyfish. One of the most common is the moon jellyfish. The largest is the Lion s Mane jellyfish. Moon jellyfish Lion's mane jellyfish Pelagia noctiluca

Molluscan Zooplankton

Nekton Nekton are the actively swimming organisms whose movements are not governed by currents or tides. Included in this group of animals are some larger invertebrates, fishes, reptiles, birds, and mammals. The invertebrates that reign supreme in the open sea are the squids.

Fish in the Open Ocean-Sailfish

Tuna

Tuna Tunas must swim constantly (some cruising at 27 kilometers, or 16 miles, per hour) or they will sink for lack of a swim bladder. This level of activity requires a large amount of energy and a good supply of oxygen. To supply the needed oxygen, these animals must swim fast and move large volumes of water past their gills. One adaptation for fast swimming in some tuna species is a body temperature 8 to 10 C higher than the surrounding water.

Tuna Fisheries Tuna species are found throughout the world's oceans. Atlantic, Pacific, and southern bluefin tuna are prized for the sushi and sashimi market. Skipjack, yellowfin, and bigeye tunas are found mainly in the tropics, while albacore, like bluefin, are also found in temperate waters. These species are used for a mixture of canned and fresh products.

Purse-Seine Fishing

Longline Fishing

Longline Fishing

Pole-and-Line

Tuna Consumption Globally

Ecology of the Open Sea The open sea represents a pelagic ecosystem, one in which the inhabitants live in the water column. In a pelagic ecosystem, the basis of food chains is the many species of small phytoplankton. These organisms derive the nutrients that they need from the seawater that surrounds them. The smaller the organism, the greater the relative surface area that is exposed for the absorption of nutrients and sunlight and the lesser the amount of nutrients needed to sustain the body. The major herbivores in the open ocean are zooplankton, and these supply food for the nekton.

Productivity Although surface waters of the open ocean receive large amounts of sunlight, they do not receive any of the nutrients that wash to sea from the land. This results in low levels of nutrients, such as nitrogen and phosphorus, that are necessary to support the life of phytoplankton. The low level of nutrients in the open ocean is most pronounced in tropical waters. Phytoplankton production in the central South Pacific Ocean is only about half as much as the productivity off the California coast and only about one sixth as much as in some coastal areas off Saudi Arabia or western Africa, where coastal upwelling brings nutrients to the surface.

Food Webs in the Open Sea

Food Webs in the Open Sea The base of food webs in the open sea is formed by the phytoplankton and heterotrophic bacteria. Phytoplankton release some of their photosynthetic products into the surrounding seawater as dissolved organic matter (DOM). Bacteria can also metabolize some of the DOM and return it to the water in inorganic form, making the mineral nutrients again available to the phytoplankton.

Efficiency of Open-Ocean Food Webs

Food Webs in the Open Sea The food webs in nutrient-poor open seas may have food chains with 5~6 links, leading to the nektonic top carnivores among the whales and sharks. The base of the food chain in plankton communities is formed by microbes with short life cycles, and 100% of each day s production may be grazed entirely by zooplankton. A pyramid of production is a pyramidshaped diagram that indicates the rate at which new biomass is produced at successive trophic levels. A standing crop is the amount of biomass of organisms in a given area at a given time. GLOSSARY

Summary The primary producers of the open sea are mainly phytoplankton. Even though the open sea receives large amounts of sunlight, it lacks the supply of nutrients that makes coastal seas so productive. The low level of nutrients is most pronounced in tropical oceans, where the water forms more or less permanent layers that are separated by thermoclines. Bacteria are important in the ability of the community to cycle nutrients efficiently. The open sea does not support many large animals because of limited primary production and food webs involving several energy-wasting steps between primary producers and final consumers.

Research in the Open Ocean

Key Concepts The open sea is a pelagic ecosystem, in which the living components are plankton and nekton. Plankton range widely in size, taxonomic diversity, and lifestyle. Phytoplankton are the primary producers in open-ocean food webs, and their productivity is limited by the scarcity of nutrients. Bacteria provide a second base to open-ocean food webs, and they allow the scarce nutrients to be efficiently recycled.

Key Concepts Limited primary production and food webs with several energy wasting steps limit the number of large animals the open ocean can support. Gelatinous plankton such as salps and ctenophores play significant roles in open-ocean ecosystems because of their efficient feeding mechanisms, reduction of nutritional quality, and provision as prey for specialist carnivores. Large zooplankton include jellyfish, gastropod molluscs, and colonial pelagic tunicates. Fish, squid, and mammals make up most of the nekton in the open sea.

Further Readings http://www.biosci.ohiou.edu/faculty/currie/ocean An academic site with many links to pelagic organisms and the scientists who study them. http://jellieszone.com/index.html Information on jellyfish and other gelatinous zooplankton.