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Pyrocene

Pyrocene is a earth science topic covered in the lgStudy science library. This page brings together a partial reference excerpt, illustrations, worked examples, real-world applications and a short study plan, so you can understand Pyrocene rather than just read about it. In short: Pyrocene is a proposed term for a new geologic epoch or age characterized by the influence of human-caused fire activity on Earth. The concept focuses on the many ways humans have applied and removed fire from the Earth, including the burning of fossil fuels and the technologies that have enabled people to leverage their influence and become the dominant species on the planet.

Key takeaways

  • Pyrocene belongs to earth science; place it in that map before memorising details.
  • Learn the definition first, then one example that makes the definition concrete.
  • Connect Pyrocene to a quantity you can measure, compute or draw — that is where exam questions come from.
  • Reproduce the core statement of Pyrocene from memory before moving on to harder problems.

Reference excerpt

Pyrocene is a proposed term for a new geologic epoch or age characterized by the influence of human-caused fire activity on Earth. The concept focuses on the many ways humans have applied and removed fire from the Earth, including the burning of fossil fuels and the technologies that have enabled people to leverage their influence and become the dominant species on the planet. The Pyrocene offers a fire-centric perspective on human history that is an alternative to or complementary term for the Anthropocene. Like the Anthropocene, the concept suggests that human activity has shaped the Earth's geology and identifies fire as humanity's primary tool for shaping the planet and its environment. Pyrocene was first proposed by environmental historian Stephen J. Pyne in 2015. Since that time, it has been adopted by journalists and scholars in the fields of wildland fire, ecology, and environmental policy focused on the impacts of climate change and increased risk of wildfires around the globe. This research has focused on extreme wildfires in Hawaii, California, Spain, Portugal, Romania, Australia, and Canada. It has relied on the concept of Pyrocene to highlight how climate change, land-use changes, and direct human ignition have increased the frequency and intensity of these conflagrations.

Etymology The word Pyrocene is formed from two Ancient Greek words. Pyros (Ancient Greek: πυρά, romanized: purá; from πῦρ (pûr) 'fire') is the Greek word for fire while "Cene" coming from the word kainós (καινός) means "new". The concept is that this epoch is "entirely new". The suffix '-cene' is used in several epochs of geologic Era.

Overview of the concept The concept of the Pyrocene argues that humanity's collective fire practices have become an informing presence and a geological force on Earth. Fire practices include all those activities that start and stop fires among living biomass, but also those that involve fossil biomass and those pyrotechnologies that enable people to leverage their influence. The foundational premise suggests that humanity and fire formed an alliance that increased the range and power of each. While fire has been on Earth for over 420 million years, as long as terrestrial plants (Silurian-Devonian terrestrial revolution), humanity has altered its regimes and expanded it into a planetary presence. In return, fire has enabled and accompanied humans to every landscape on Earth and even the Moon. Humanity enjoys a species monopoly over fire's manipulation, establishing it as the keystone species for fire on Earth and making fire its unique ecological signature. Together, humans and fire have upset biogeochemical cycles, including carbon, rewired energy flows, and, through the accumulation of emitted greenhouse gases into the atmosphere, perturbed global climate to such an extent that climate history has become a subnarrative of fire history. According to Pyne's concept of the Pyrocene, there have been three kinds of fire. The first kind of fire was natural fire, which began with the evolution of plants. The second kind of fire was human fire, which the species domesticated for heat, light, cooking, and the control of landscapes. The third kind of fire involves extracting and burning fossil fuels through chemical combustion and industrial machinery. This third kind of fire has created by-products in the form of pollution and greenhouse gasses on a scale that have overwhelmed the atmosphere and the planet's capacity to cope with the accelerated rate with which humans burn these fuel sources.

History of the concept Fire historian Stephen Pyne first used the term in an article, "Fire Age," published by Aeon in 2015, then announced in the more fully developed form in 2019, again in Aeon. In 2019, Pyne used the concept to frame the September fire-focused issue of Natural History magazine and to provide a coda to a revision of Fire: A Brief History. In 2021 he condensed his notions into a small book,The Pyrocene: How We Created a Fire Age, and What Happens Next. The book was translated into Italian, Portuguese, Chinese, and Danish, and reviewed by both Nature and Science. The Pyrocene has been frequently invoked in news articles about catastrophic wildfires in places like California, Hawaii, and Australia and the growing impact of wildfire smoke. Journalists in outlets including the New York Times, New York Magazine, Wired, and Los Angeles Times. The New Yorker has included it a review of recent books with a fire theme. An overview has appeared in Scientific American. In his original conception, Pyne imagined the Pyrocene as coextensive with the Holocene (current geological epoch, beginning approximately 11,700 years ago), commencing as a fire-wielding species that interacted more widely with a fire-warming Earth. He introduced the term "pyric transition" to describe the subsequent phase change that occurred when humans began to burn fossil biomass (or what he calls "lithic landscapes") in place of surface biomass ("living landscapes"). Burning in living landscapes has a long evolutionary ecological checks and balances history. Burning fossil biomass lacks those baffles and barriers; the available sources overwhelm the sinks, unhinging air, seas, and terrestrial biotas. Both realms of combustion share an unbroken narrative of humanity's relationship to fire. Pyne has proposed the metaphor of a fire age – the fire-informed equivalent of an ice age to suggest the cumulative magnitude of these effects. The Pyrocene is thus a successor epoch to the Pleistocene.

… excerpt ends here. Continue reading the full article.

Worked examples

Example 1 — a first encounter with Pyrocene

Start with the simplest possible case. Write down what Pyrocene claims or describes in one sentence, then invent the smallest concrete situation in which that sentence is true. In earth science, the smallest case is usually a single object, a single equation or a single measurement. Check that every symbol or term in your sentence has a meaning in that case.

Example 2 — changing one variable

Take the situation from Example 1 and change exactly one quantity: double it, halve it, or set it to zero. Predict what should happen to Pyrocene before you calculate. Comparing your prediction with the result is the fastest way to find out whether you understand the idea or only the words.

Example 3 — an exam-style question

Typical questions about Pyrocene ask you to (a) state it precisely, (b) apply it to given data, and (c) explain a limitation. Practise writing all three answers in under five minutes; the third part is what separates a full-mark answer from an average one.

Applications of Pyrocene

In research
Pyrocene appears in earth science research whenever the underlying quantities have to be modelled precisely. Papers usually cite it as a starting assumption and then explore where it breaks down.
In technology and industry
Engineering practice reuses Pyrocene in design rules, simulations and safety margins. Knowing the idea lets you read a specification sheet and understand why the numbers look the way they do.
In the classroom
Pyrocene is common in secondary-school and first-year university syllabi. It links to neighbouring topics Fire, Geologic time scales, so understanding it makes those chapters shorter.
In everyday life
Look for Pyrocene outside the textbook — in sport, cooking, traffic, electronics or the sky above you. An example you found yourself is remembered far longer than one you were given.

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How to study Pyrocene in 20 minutes

  1. Read the reference excerpt below once, without taking notes.
  2. Close the page and write down what Pyrocene means in your own words.
  3. Compare your version with the excerpt and mark what you missed.
  4. Work through the three examples above with pen and paper.
  5. Explain Pyrocene out loud to somebody else — or to Teacher Smith in the lgStudy chat.

Frequently asked questions

What is Pyrocene in simple terms?

Pyrocene is a proposed term for a new geologic epoch or age characterized by the influence of human-caused fire activity on Earth. The concept focuses on the many ways humans have applied and removed fire from the Earth, including the burning of fossil fuels and the technologies that have enabled p…

Why does Pyrocene matter?

Because it connects several earth science ideas at once: it gives you a definition you can apply, a quantity you can calculate, and a way to check whether a result is plausible.

How should I study Pyrocene?

Read the excerpt, restate it from memory, then work through the examples and applications listed on this page. The five-step study plan above takes about twenty minutes.

What does this page cover?

It gives you a compact reference excerpt plus original lgStudy explanations, examples, applications and study material on Pyrocene.

Tags

  • Fire
  • Geologic time scales

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