The world's regional climates are determined by the agonisingly slow tectonic movements of continental and oceanic crustal plates.
Plate tectonics set the long-term patterns for the shape of the continents, the seaways, future ocean circulation and cloud albedo, while solar irradiance and orbital cycles are the trigger points.
Atmospheric CO₂ and global surface temperature are not locked together either, a story revealed in the geological record. Far from causing a mass collapse, past high-carbon epochs created the richest expansions of biosphere diversity in Earth’s history.
Atmospheric CO₂ levels were often 10 to 15 times higher than today during the early Paleozoic era (538 to 251 million years ago), starting with the Cambrian explosion. During these evolutionary peaks, atmospheric CO₂ was measured in the thousands of parts per million. Changes did not happen over decades either — they took tens of thousands of years.
A modest rise in CO₂ levels in the modern industrial era is not a sign of runaway warming; it's a recovery during a far longer global decline in atmospheric CO₂. This brief pulse has stimulated global vegetation growth and leaf area expansion, verified by NASA satellite observations.
Our current geological epoch — the Quaternary glaciation — sits near historical low levels for atmospheric CO₂ concentrations. We are in a severely cold epoch that has locked the world in a 2.58-million-year ice age regime. This ice age climate continues today.
During the Last Glacial Maximum 26,000 to 20,000 years ago, ice sheets miles deep blanketed North America, northern Europe, and Siberia. CO₂ fell to approximately 180 ppm, flirting with the 150 ppm threshold where land plants cease photosynthetic activity.
The glaciers began to melt and retreat rapidly 20,000 to 15,000 years ago, with most ice disappearing from major landmasses by 10,000 years ago. Sea levels rose by only 10-13 millimetres a year for around 9,000 years, a measurably slow pace of change, compared with today's 3 mm a year.
By contrast, today's CO₂ hovers around 425 ppm, rising and falling through the years to the rhythms of the seasons. CO₂ does not pose a danger to climate, but it is an essential building block for the biological world.
IMAGE: What 540 million years of geological history says: Willis Eschenbach.
Plate tectonics set the long-term patterns for the shape of the continents, the seaways, future ocean circulation and cloud albedo, while solar irradiance and orbital cycles are the trigger points.
Atmospheric CO₂ and global surface temperature are not locked together either, a story revealed in the geological record. Far from causing a mass collapse, past high-carbon epochs created the richest expansions of biosphere diversity in Earth’s history.
Atmospheric CO₂ levels were often 10 to 15 times higher than today during the early Paleozoic era (538 to 251 million years ago), starting with the Cambrian explosion. During these evolutionary peaks, atmospheric CO₂ was measured in the thousands of parts per million. Changes did not happen over decades either — they took tens of thousands of years.
A modest rise in CO₂ levels in the modern industrial era is not a sign of runaway warming; it's a recovery during a far longer global decline in atmospheric CO₂. This brief pulse has stimulated global vegetation growth and leaf area expansion, verified by NASA satellite observations.
Our current geological epoch — the Quaternary glaciation — sits near historical low levels for atmospheric CO₂ concentrations. We are in a severely cold epoch that has locked the world in a 2.58-million-year ice age regime. This ice age climate continues today.
During the Last Glacial Maximum 26,000 to 20,000 years ago, ice sheets miles deep blanketed North America, northern Europe, and Siberia. CO₂ fell to approximately 180 ppm, flirting with the 150 ppm threshold where land plants cease photosynthetic activity.
The glaciers began to melt and retreat rapidly 20,000 to 15,000 years ago, with most ice disappearing from major landmasses by 10,000 years ago. Sea levels rose by only 10-13 millimetres a year for around 9,000 years, a measurably slow pace of change, compared with today's 3 mm a year.
By contrast, today's CO₂ hovers around 425 ppm, rising and falling through the years to the rhythms of the seasons. CO₂ does not pose a danger to climate, but it is an essential building block for the biological world.
IMAGE: What 540 million years of geological history says: Willis Eschenbach.