How Do We Know About Earth's Past Climate?

Earth Holds Multiple Types of Evidence About Its Climate History

The modern thermometer was invented in 1654, and global temperature records began in 1880. So how do scientists know so much about Earth’s climate before then?

The Earth holds climate clues dating back more than 3 billion years; they are contained in rock layers, polar ice sheets, lake beds, and more. Researchers at NASA and elsewhere use these records of Earth’s past climate to help them understand our current and future climate.

This study of past climates is called paleoclimatology. A changing climate triggers many different effects, leaving multiple lines of evidence for scientists to follow. For example, the signs of the ice ages are visible in the features that glaciers carved into the landscape. These climate swings also caused changes in plant communities, sea level, and the composition of Earth’s atmosphere.

Evidence of Earth’s past is all around us. All we need to do is read the signals, such as these below.

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Modern Temp Record
1880 TO PRESENT
Tree Rings
UP TO 9K YEARS AGO
Positions of Glaciers
UP TO 20K YEARS AGO
Lake Sediments
UP TO 1M YEARS AGO
Ice Cores
UP TO 2M YEARS AGO
Ocean Sediments
UP TO 200M YEARS AGO
Landforms
UP TO 500M YEARS AGO
Corals
UP TO 540M YEARS AGO
Sedimentary Rocks
UP TO 3.9B YEARS AGO
CENOZOIC
Quaternary
NEOGENE
2.58 - 23 MYA
(Million Years Ago)
PALEOGENE
23 - 66 MYA
MESOZOIC
CRETACEOUS
66 - 145 MYA
JURASSIC
145 - 201 MYA
TRIASSIC
201 - 252 MYA
PALEOZOIC
PERMIAN
252 - 299 MYA
CARBONIFEROUS
299 - 359 MYA
DEVONIAN
359 - 419 MYA
SILURIAN
419 - 443 MYA
ORDOVICIAN
443 - 485 MYA
CAMBRIAN
485 - 539 MYA
PRECAMBRIAN
PRECAMBRIAN
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