A question that many wonder about is why is phytoplankton important? Plankton is revealed by ocean color and help show scientists where ocean currents provide nutrients for plant growth. They also help show where pollutants are poisoning the ocean preventing plant growth and where changes in the climate of the ocean are occurring. Plankton is also the foundation of the oceans food chain. As phytoplankton begin to grow and multiply, small fish eat them, then the larger animals begin to eat those smaller animals. The food chain of the ocean begins phytoplankton, then comes zooplankton, next is the predatory zooplankton, fourth is the filter feeders and last is the predatory fish. Phytoplankton is sometimes called the grass of the sea because …show more content…
Researchers that are studying the origins of earth’s first breathable atmosphere have zeroed in on the major role played by the most unassuming creature: plankton. They believed 500 million years ago the earth’s crust contained upheavals [a violent, sudden change or a disruption]. This initiated a strange reverse green house effect, cooling the world’s oceans, spawned giant plankton and sent bursts of oxygen into the atmosphere. This new discovery reveals details of how oxygen came to vanish from the earth’s ancient atmosphere during the Cambrian period and reappeared in higher levels than ever before. Plankton maybe at the bottom of the food chain today but back then they ruled the planet. No life existed on land during that period of time, life in the ocean was not very diverse aside from the abundance of trilobites, an extinct marine arthropod the existed abundantly in the Paleozoic …show more content…
Our understanding of plankton has immensely evolved greatly over time. In the early 1800’s many scientists originally used simple nets and jars to study plankton but quickly after learning how huge their world was scientists strained to learn more. They asked a range of questions, including “where do different types of plankton live?,” “how to plankton populations change over time?,” and “what roles do they play in aquatic food webs?.” Such questions efforts motivated many scientists to create new tools that would help them to view certain aspects of plankton in the ocean. From the original simple net grew a range of new technologies that allowed us to develop a detailed picture of the behavior and habitat of plankton. (how has are knowledge of plankton changed over time ,
Plankton Activity Postlab 1) Apply 2.5: Use mathematical and/or computational representations to support explanations of factors that affect carrying capacity of ecosystems at different scales. Explain how the abundance of phytoplankton in the pond depends on the abundance of an abiotic resource such as nitrogen. - Phytoplankton are the producers in the pond. Species of organisms in ecosystems have their own carrying capacity relative to other species, and carrying capacities are determined by particular abiotic and biotic resources in an ecosystem. An increase in nitrogen levels in the pond (e.g. from fertilizers) will result in a dramatic increase in phytoplankton levels, but once phytoplankton population reaches its carrying capacity (determined by availability of other resources besides nitrogen, [DO] levels, predation etc.),
This had a huge effect on the planktons. Zooplanktons the eat phytoplankton. If there isn’t much phytoplankton for the zooplankton to eat, there numbers will decrease. The article “ The Short‐Term Impact of the Zebra Mussel Invasion,” “phytoplankton fell by 80 percent. Zooplankton (which eat phytoplankton) declined by half.
Some crustaceans have discovered land but they are mainly aquatic arthropods. Crustacean’s use their gills for respiration. Gills are crustacean’s respiratory organs, as the water flows over the gills they oxygen is absorbed from the water (Edney, 1968). Due to the process of respiration with the
The book addresses aquatic and terrestrial ecosystems. At the beginning of the text a vocabulary page outlines the essential words for understanding. Bold faced words highlight the key vocabulary. This text contains many opportunities for students to ask question and respond to their reading. Illustrations cover the page to support the text.
Sedimentary facies changes may show if there was a transgression or regression and can be identified on whether there are coarse-grained sediments such as sand, which indicates they are nearshore, in high energy environments. Or if they are fine-grained sediments like muds and silts, they indicate offshore, deep, low energy environments. List and discuss in detail major problems that had to be overcome by plants and animals in order to live successfully on land. Give examples. Discuss how life has evolved from the ocean during the Paleozoic to move onto
The way they are in general are remarkable animals, they 're so majestic and unique. The sea nettle mostly moves with the ocean 's current because they are weak and can 't go against it but they can move short distances to catch prey, the ocean current is unpredictable so were the current moves they move. The Sea nettles use light sensors to know when it is light out side, so when it it light they migrate up more to the surface and when it becomes dark they move back down at night.
The evolution of advantageous traits in these two taxa would have made it much easier for them to prey on the placoderms. In addition to predation, the new adaptations exhibited by the ray-finned and cartilaginous fishes could have make them more efficient at capturing prey items that the placoderms may have had sole access to in the past (Carr, 1995). Pressure by predators as well as competitive pressure would have made it much harder for the placoderms to deal with other changes in the
Nitrogen has been found to be a limiting factor when referring to plant growth and algae in marine waters (Ryther, Dunstan, “Nitrogen, Phosphorus, and Eutrophication in the Coastal Marine Environment”). A limiting factor is something than is a main factor that affects the population growth of an organism. A 37 year old experiment on a lake
This can begin by considering where the shell-shaped in connection to the life form's condition and part. At first, we confirmed that the shell likely shaped ashore. The explanation behind this is we felt that the early relatives who lived in water required the adaptability to do their lives, and a shell would make that troublesome. A shell can be utilized for insurance so that it might appear like the shell would hinder oceanic exercises. However, it is likewise conceivable that the shell was made to encourage relaxing.
As the temperature was increasing so was the anaerobic respiration. The organism was put under an intense amount of stress causing it to die. There was little to no oxygen on earth in the beginning. However, because there was not much oxygen the cells would have had to learn how to use the anaerobic process without oxygen. To conclude there was more anaerobic respiration occurring due to the lack of oxygen.
Marine organisms are animals, plants, and other living things that live in the ocean. A Marine biologist is a scientist who studies marine organisms and studies the bodies, behavior, and the history of marine organisms. They also study how marine organisms interact with each other and their environment. I have chosen to research about Marine biology because I would like to learn about sea life, the ocean, and its surrounding environment. To start off, a Marine biologist might study coral, crabs, fish, microscopic marine organisms, sea stars, seaweed, squid, or whales.
About 71 percent of our planet Earth is covered by water, and the majority comes from the oceans (about 96.5 percent of all Earth’s water). It remains as the most expansive, diverse, and mysterious places on planet Earth. But it is being threatened by the pollution by people and nature itself. By polluting the habitat of marine organism will indirectly affect the ecosystem of the marine life. Marine life is dying and as the result the oceanic ecosystem is threatened.
The LCHF provides insights into past mantle geochemistry and presents a better understanding of the chemical compositions that existed during the evolutionary transitioning, from geochemical processes to biochemical processes (Baker & German, 2004). However, there is a reason to doubt the origin of life from hydrothermal vents. One of the main arguments against the origin of life from the deep sea, is the fact that so many macromolecules are found in biology. Molecules such as DNA, RNA, proteins and lipids are all polymers and form via condensation reactions – a wet environment is required for molecules to mix, but water then needs to be removed in order to form a polymer (Da Silva,
A major US oceanographic survey has just discovered new forms of life in one of the deep oceanic trenches of the world. Much remains undiscovered in deep ocean trenches and as a result, many scientists are currently researching oceanic trenches, more specifically deep-ocean chemosynthetic research (Vanreusel et al., 2004). The goal for many scientists lies in trying to determine what organisms exist in oceanic trenches, since not nearly all organisms that live down there have been discovered. The discoveries of life that can be made through investigation of the deep oceanic trenches in our seas and thus the discoveries that can be made about deep-sea ecosystems are very important. Research in this particular area is of great importance due
The values of temperature and salinity of the water masses are acquired on the surface and in the mixed layer by heating, cooling, rain, evaporation, wind, waves and currents. Once they sink below the mixed layer, temperature and salinity may be changed only by mixing processes with adjacent water bodies. In these depths the temperature and salinity are conservative properties as there are no significant sources or sinks in the deep ocean. Seen from this perspective the temperature and salinity are not independent variables, and their knowledge allows us to recognize water masses. Oxygen is on the other hand, a non-conservative property, is acquired in surface and and is slowly reduced over time due to oxidation of organic matter and respiration of organisms.