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Drill Cores and Fossils: Was the Atlantic Always There? worksheet preview

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Drill Cores and Fossils: Was the Atlantic Always There?

Grade 7 Earth science: analyze seafloor drill-core ages and fossil locations to argue that South America and Africa have moved apart.

Grade 7ScienceInteractive · Printable

Aligned toMS-ESS2-3

What’s included

  • Single worksheet
  • Auto-graded online
  • 1 NGSS standard
  • Printable answer key
  • 10 questions
  • Classroom-ready

Details

Format
Interactive · Printable
Grade
Grade 7
Subject
Science
Question types
Fill in the blank, Multiple choice, Matching, Short answer

About this worksheet

What students practice

  • Students analyze seafloor age and sediment data to describe how the ocean floor spreads from a ridge.
  • Students use fossil and rock evidence to argue that continents were once joined and have moved apart.

How to use

Read the drilling log together, then have students find the pattern in the drill-site table before they start the questions. Use the last question as an exit ticket.

Curriculum

NGSS standard covered

MS-ESS2-3

Use fossil, rock and seafloor data as evidence of past plate motions.

Preview

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Drill Cores and Fossils: Was the Atlantic Always There?

Use seafloor ages, mud layers and fossil finds as evidence of moving plates.

Drill core data

Read the drilling log and study the table. Then answer the questions.

Drilling Log: Crossing the South Atlantic

1Down the middle of the South Atlantic Ocean runs a long chain of underwater mountains called the Mid-Atlantic Ridge. Along its center, melted rock rises from below, cools and hardens into a dark volcanic rock called basalt. A research drilling ship sailed east from the ridge toward Africa and stopped at six sites, labeled A through F.

2At each site the crew lowered a drill pipe several kilometers to the seafloor. The drill cut through a layer of soft mud and then into the basalt below. Back on deck, scientists studied tiny fossils in the mud resting directly on the basalt. Because that mud began to settle soon after the basalt formed, its age tells roughly how old the basalt is. They also measured how thick the whole mud layer was. Mud on the open seafloor builds up very slowly, from tiny shells and dust sinking through the water.

3Geologist Dr. Nnamdi Eze posted the results in the table below. A second ship drilling west of the ridge, toward South America, reported a matching set of ages on that side. Ages in the table are in millions of years, so a basalt age of 5 means the rock formed about 5 million years ago.

4Evidence also comes from the land. Fossils of Mesosaurus, a reptile about 1 m long, have been found in rocks about 280 million years old in eastern South America and in southern Africa. Scientists think it lived in lakes and shallow, not very salty water, and it was too small to cross thousands of kilometers of open ocean. Fossils of Glossopteris, a seed fern whose seeds were likely too large to blow across an ocean, are found on several southern continents. Geologists have also found that rock formations of the same type and age line up along the coasts of Brazil and West Africa when the two coastlines are fitted together like puzzle pieces.

Drill sites east of the Mid-Atlantic Ridge
SiteDistance from ridge (km)Basalt age (million yr)Mud thickness (m)
A100520
B3001560
C5002595
D70035130
E90045170
F110055205
1.

How many million years older is the basalt at Site E than the basalt at Site B?   million years

2.
Which statement best describes the pattern in the table?
  • A. The basalt is about the same age at every site, but the mud gets thicker.
  • B. The basalt gets older and the mud gets thicker moving away from the ridge.
  • C. The ages go up and down with no clear link to distance from the ridge.
  • D. The basalt gets younger and the mud gets thinner moving away from the ridge.
3.
Use Sites A and B. The seafloor between them is 200 km wide and formed over 10 million years. 200 km is 20,000,000 cm.

On average, this seafloor moved away from the ridge about   cm per year.

4.
The ship plans a seventh site 1,300 km east of the ridge. If the pattern continues, about how old should the basalt there be?
  • A. About 65 million years
  • B. About 55 million years
  • C. About 130 million years
  • D. About 45 million years
5.
Why is the mud layer about ten times thicker at Site F than at Site A?
  • A. Site F was drilled deeper, so the crew reached more mud.
  • B. Mud from the ridge's volcanoes flows downhill and piles up far from the ridge.
  • C. The basalt at Site F has sat on the seafloor much longer, so more mud has settled on it.
  • D. The water near Africa is colder, so mud there grows faster.
6.
Which model fits the drill data from both sides of the ridge?
  • A. The whole ocean floor formed at one time, and only the mud has changed since.
  • B. The seafloor near Africa is sinking, which makes the rock there look older.
  • C. The oldest seafloor formed at the ridge, and younger rock was added near the coasts later.
  • D. New seafloor forms at the ridge and slowly moves away from it on both sides.

Fossil and rock clues

Use the table and the drilling log to answer the questions.

Where four fossils have been found
FossilWhat it wasAge (million yr)Continents found on
MesosaurusSmall water reptileabout 280South America, Africa
GlossopterisSeed fern (plant)about 300 to 250five continents (see note below)
LystrosaurusLand reptileabout 250Africa, India, Antarctica
CynognathusLand reptileabout 240South America, Africa
Note: Glossopteris fossils are found in South America, Africa, India, Antarctica and Australia.
7.
Lystrosaurus lived on land and could not cross a wide ocean. Which landmasses do its fossils suggest were connected about 250 million years ago?
  • A. South America and Australia
  • B. Africa, India and Antarctica
  • C. India and Australia
  • D. North America and Europe
8.
Why are Mesosaurus fossils strong evidence that South America and Africa were once joined?
  • A. It probably could not cross a wide ocean, yet its fossils are found on both coasts.
  • B. Its fossils are found on every southern continent in the table.
  • C. It was a large ocean reptile that swam back and forth across the Atlantic.
  • D. Its fossils are about the same age as the basalt near the ridge.
9.
Match each piece of evidence to the idea it best supports.
  1. Basalt gets older farther from the ridge.
  2. Rocks of the same type and age line up on the coasts of Brazil and West Africa.
  3. Glossopteris fossils appear on five southern continents.
  4. Mud is thicker on basalt far from the ridge.
  1. A. Basalt far from the ridge has been on the seafloor longer.
  2. B. New ocean floor spreads outward from the ridge.
  3. C. Several southern continents were once part of one landmass.
  4. D. Those two coastlines were once side by side.
10.
A classmate says South America and Africa have always been as far apart as they are today. Write a claim about this idea. Support it with evidence from the drill-site table and one fossil or rock clue, and explain your reasoning.

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