Chapter 20: Problem 2
Deposits of shells from ancient \(__________\)are mined as chalk and limestone. a. dinoflagellates c. radiolaria b. diatoms d. foraminifera
Short Answer
Expert verified
Foraminifera (d) are responsible for chalk and limestone deposits.
Step by step solution
01
Understanding the Question
The question asks us to identify which group of organisms deposits shells that are mined as chalk and limestone.
02
Reviewing Options
We are given four options: a. dinoflagellates, b. diatoms, c. radiolaria, d. foraminifera. Each of these is a group of microorganisms known for their different shell types.
03
Identifying Organism with Chalk and Limestone Deposits
Chalk and limestone are primarily composed of calcium carbonate, which is predominantly deposited by foraminifera. Foraminifera are single-celled protists with shells, and their accumulated shells often form limestone and chalk beds over millions of years.
04
Matching to the Correct Option
Having identified that foraminifera are responsible for chalk and limestone deposits, we match this to the corresponding option, which is d. foraminifera.
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Key Concepts
These are the key concepts you need to understand to accurately answer the question.
Chalk
Chalk is a type of soft, white limestone, easily recognizable by its powdery texture. It primarily consists of the mineral calcium carbonate, specifically in the form of calcite. This mineral component originates from the microscopic shells of marine organisms, like foraminifera, that settled to the sea floor over millions of years.
The formation of chalk involves several geological processes:
The formation of chalk involves several geological processes:
- Shell Accumulation: Marine microorganisms, such as foraminifera, live in the ocean. As they die, their shells, which are made of calcium carbonate, accumulate on the sea floor.
- Compaction: Layers of these shells pile up over time, exerting pressure on the lower layers. This compaction results in the transformation of loose shell debris into solid rock.
- Exposure: Geological events such as tectonic uplifting or sea level changes can expose these layers to the earth's surface, where they may be mined as chalk.
Limestone
Limestone is a sedimentary rock known for its abundance and versatility. Like chalk, it is primarily composed of calcium carbonate but differs in density and hardness. Limestone is formed from the remains of marine organisms, including foraminifera and coral.
Here’s a closer look at its formation:
Here’s a closer look at its formation:
- Organic Origin: When marine organisms with calcium carbonate shells die, their remains settle on the ocean floor, contributing to the formation of limestone.
- Chemical Precipitation: Besides biological processes, limestone can also form when calcium carbonate precipitates directly from water, often in warm, shallow marine environments.
- Variety: The presence of other materials, such as clay, sand, or organic remains, can create varied types of limestone, such as fossiliferous limestone, oolitic limestone, and travertine.
Calcium Carbonate
Calcium carbonate is a chemical compound with the formula \( \text{CaCO}_3 \). It is a common substance found in rocks as the minerals calcite and aragonite, and it is the main component of pearls and the shells of marine organisms, snails, and eggs.
The compound is crucial in the formation of sedimentary rocks, such as chalk and limestone. Here are some of its primary characteristics and occurrences:
The compound is crucial in the formation of sedimentary rocks, such as chalk and limestone. Here are some of its primary characteristics and occurrences:
- Natural Form: Calcium carbonate naturally occurs in mineral deposits worldwide, forming structures such as limestone caves and stalactites and stalagmites found within them.
- Biological Function: Many marine organisms rely on calcium carbonate to construct their hard shells and skeletons, contributing significantly to sediment buildup on the ocean floor.
- Industrial Uses: Due to its chemical properties, calcium carbonate is widely used in the manufacturing of cement, the production of lime, and as a dietary calcium supplement.