Ocean Acidification Effects and Calcium Carbonate
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Questions and Answers

What happens to the majority of CaCO₃ in shallow water depths?

  • It is buried in the sediment (correct)
  • It dissolves immediately
  • It floats away
  • It remains on the surface

The increase in atmospheric CO₂ leads to a deeper carbonate compensation depth (CCD).

False (B)

What effect does ocean acidification have on marine phytoplankton and plant species?

It can have negative, neutral, or positive effects.

The depth at which all carbonate is dissolved is known as the __________.

<p>carbonate compensation depth (CCD)</p> Signup and view all the answers

Match the following outcomes to marine species based on CO₂ levels:

<p>Certain marine phytoplankton = May increase in photosynthesis Other plant species = May experience negative effects Some marine plants = May show no signs of change Overall biodiversity = Inevitably affected by changes</p> Signup and view all the answers

What is ocean acidification primarily caused by?

<p>Uptake of atmospheric carbon dioxide (A)</p> Signup and view all the answers

Coral reefs benefit from ocean acidification.

<p>False (B)</p> Signup and view all the answers

What is the current approximate pH of the ocean?

<p>8.0</p> Signup and view all the answers

The two forms of calcium carbonate mentioned are _______ and _______.

<p>calcite and aragonite</p> Signup and view all the answers

Which factor has a major local effect on ocean acidification?

<p>Eutrophication (C)</p> Signup and view all the answers

Match the following forms of calcium carbonate with their characteristics:

<p>Calcite = Less soluble form found in some marine organisms Aragonite = More soluble form found in most corals and mollusks</p> Signup and view all the answers

Ocean acidification refers to the ocean becoming acidic with a pH less than 7.0.

<p>False (B)</p> Signup and view all the answers

What is the impact of acid rain on ocean chemistry?

<p>It can decrease the pH of surface ocean waters.</p> Signup and view all the answers

What process leads to a decrease in seawater oxygen levels during eutrophication?

<p>Decomposition of algae by bacteria (A)</p> Signup and view all the answers

Ocean acidification decreases the availability of carbonate ions.

<p>True (A)</p> Signup and view all the answers

What are the products formed when CO₂ reacts with seawater?

<p>Carbonic acid, bicarbonate ions, and hydrogen ions.</p> Signup and view all the answers

The saturation horizon is the level below which calcium carbonate minerals undergo _____ .

<p>dissolution</p> Signup and view all the answers

Match the terms with their corresponding effects:

<p>Increased CO₂ = Decreased pH level Carbonic acid = Increased acidity Bicarbonate ions = Lower availability of carbonate ions Dissolution = Destruction of shells</p> Signup and view all the answers

Which of the following is NOT a suggested mitigation strategy for ocean acidification?

<p>Increasing offshore drilling (D)</p> Signup and view all the answers

Name one marine organism mentioned that relies on carbonate ions for calcification.

<p>Coral</p> Signup and view all the answers

Surface waters are under saturated with carbonate ions.

<p>False (B)</p> Signup and view all the answers

What happens to calcifying organisms due to ocean acidification?

<p>They become vulnerable to dissolution of their shells (B)</p> Signup and view all the answers

The saturation horizon for aragonite is found at a greater ocean depth than that for calcite.

<p>False (B)</p> Signup and view all the answers

What is the primary natural source of CO₂ on Earth?

<p>Volcanoes</p> Signup and view all the answers

The depth at which dissolution strongly increases in the deep ocean is known as the ______.

<p>lysocline</p> Signup and view all the answers

How does upwelling affect coastal regions?

<p>It circulates deeper ocean water, bringing more nutrients. (B)</p> Signup and view all the answers

Rock weathering can quickly reduce the anthropogenic input of CO₂ to the atmosphere.

<p>False (B)</p> Signup and view all the answers

What do the upper layers of the ocean tend to be supersaturated with?

<p>Calcium carbonate (CaCO₃)</p> Signup and view all the answers

Match the following terms with their definitions:

<p>Ocean Acidification = The decrease in pH levels of ocean water Upwelling = The upward movement of deeper ocean water Saturation Horizon = The depth at which calcium carbonate remains stable Lysocline = The depth where dissolution of carbonate increases sharply</p> Signup and view all the answers

Flashcards

Ocean Acidification

The decrease in ocean pH caused by the absorption of excess carbon dioxide from the atmosphere.

Ocean pH

A measure of the acidity or basicity of seawater. Lower pH means more acidity.

Carbon Dioxide (CO2) Absorption by Oceans

Oceans absorb a significant amount of CO2 produced by human activities, impacting ocean chemistry.

Calcite

A mineral form of calcium carbonate, found in some marine organisms. Relatively less soluble.

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Aragonite

A mineral form of calcium carbonate, found in many marine organisms. More soluble than calcite.

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Acid Rain

Rain with a low pH, which can affect surface ocean chemistry locally.

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Eutrophication

Excess nutrients (mostly nitrogen) in coastal waters, potentially affecting ocean chemistry.

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Coral Reef Impact

Ocean acidification negatively impacts coral reef growth and health.

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Saturation Horizon

The depth in the ocean where the concentration of calcium carbonate is sufficient to prevent dissolution.

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Ocean Acidification & Saturation Horizon

Acidification causes the Saturation Horizon to rise, exposing more organisms to undersaturated waters increasing dissolution risk.

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Lysocline

Boundary between the supersaturated upper and undersaturated lower parts of the ocean, Where dissolution strongly increases.

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Upwelling Events

Periodic movement of deeper ocean water to the surface, bringing nutrients and CO₂.

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Ocean Acidification Effect on Upwelling

As ocean acidification shallows the supersaturated layer, upwelling events more frequently expose organisms to undersaturated water.

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Calcite Saturation Horizon

The depth at which calcite will not dissolve, and is deeper than the aragonite horizon.

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Aragonite Saturation Horizon

The depth in the ocean where aragonite solubility is balanced (prevented from dissolving).

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Carbon Cycle Imbalance

Human activity is adding CO2 faster than the natural processes of the Carbon Cycle can absorb it.

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Carbonate ions

Essential ions for calcification, vital for marine organisms to build shells; decreased by increased CO₂

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Calcification

The process of building hard parts (shells, skeletons) from calcium carbonate in marine organisms

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CO₂ absorption in seawater

Increased CO₂ in the atmosphere leads to more CO₂ dissolving in the ocean, forming carbonic acid, decreasing ocean pH

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Carbonic acid formation

The reaction where CO₂ dissolves in water to produce carbonic acid, a key part of ocean acidification.

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Mitigation of ocean acidification

Methods to reduce CO₂ emissions and other impacts of ocean acidification through various means.

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pH decrease in seawater

The lowering of ocean water's pH due to increased CO₂ levels, causing a more acidic environment.

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Carbonate Compensation Depth (CCD)

The ocean depth at which all carbonate minerals dissolve due to pressure and acidity.

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Ocean Acidification Effect on CCD

As ocean pH decreases, the CCD shallows, exposing more shells in sediment to dissolving conditions.

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Winners and Losers in Ocean Acidification

Some marine organisms may benefit from higher CO₂ levels, while others are negatively affected, showing the variability of responses to ocean acidification.

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Why Reduce CO₂ Levels?

Reducing atmospheric CO₂ levels is crucial to halt ocean acidification and protect marine ecosystems.

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Study Notes

Ocean Acidification

  • Oceans absorb a significant amount of CO₂, acting as a buffer against climate change.
  • Ocean acidification is a decrease in ocean pH (increase in hydrogen ions) due to CO₂ uptake from the atmosphere.
  • This leads to a decrease in carbonate ions and less alkalinity.
  • The uptake of atmospheric CO₂ is exceeding the ocean's natural buffering capacity.
  • Ocean pH has decreased by 0.1 units since the industrial revolution.
  • Current ocean pH is around 8.0, remaining basic but susceptible to further decrease.

Forms of Calcium Carbonate

  • Calcite and aragonite are two forms of calcium carbonate.
  • Calcite is a relatively less soluble form, found in some shells, corals, and mollusks (oysters).
  • Aragonite is a more soluble form, present in most corals, mollusks, and some algae.

CO₂ Effect on Ocean Acidification

  • The increasing uptake of atmospheric CO₂ causes an increase in hydrogen ions.
  • This decrease in carbonate ions and the resulting decrease in alkalinity are known as ocean acidification.

Other Factors Influencing Ocean Acidification

  • Acid Rain: Has a pH between 1 and 6, impacting local ocean chemistry, but has a minimal global effect.
  • Eutrophication: Excess nutrients (mostly nitrogen) from agriculture, fertilizers, and sewage lead to plankton blooms. Decomposition of these blooms consumes oxygen and increases CO₂, decreasing pH.

Ocean Acidification Effects

  • Coral reefs struggle to grow in increasingly acidic waters.
  • Reduced plankton production affects fisheries.
  • Shells and skeletons of marine organisms are compromised due to reduced carbonate ion availability for calcification.

Ocean Acidification and Calcification

  • Seawater absorbs CO₂, creating carbonic acid, bicarbonate, and carbonate ions.
  • Carbonate ions are crucial for calcification (shell and skeleton formation) in many marine organisms.
  • Increased CO₂ lowers carbonate ion concentration, which hinders calcification.

Mitigation Strategies

  • Reduce CO₂ emissions.
  • Promote energy efficiency and alternative energy sources (wind & solar).
  • Eliminate offshore drilling.
  • Implement government policies to cap CO₂ emissions.

Saturation Horizons

  • The saturation horizon is the depth at which calcium carbonate is under-saturated.
  • Ocean acidification raises this horizon, leading more marine organisms facing conditions where their shells/skeletons dissolve.

Ocean Acidification and Long-Term Carbon Fate

  • Over long timescales, a natural balance exists between CO₂ uptake and release at Earth's surface.
  • Processes like rock weathering and organic matter production help regulate this balance.

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Ocean Acidification PDF

Description

Explore the impact of ocean acidification on marine life and the chemistry of calcium carbonate. Understand how increased CO₂ affects ocean pH and the forms of calcium carbonate present in different organisms. This quiz addresses key concepts crucial for grasping environmental science and marine biology.

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