Skip to main content

A New Epoch in the Earth’s Timeline

Throughout the span of Earth's history, the planet has undergone profound transformations in its terrain, climate, and biodiversity, all of which are meticulously preserved beneath the surface.

Layers within the Earth's crust serve as a repository of clues documenting pivotal junctures that have profoundly reshaped the Earth, encompassing episodes like the ice age and impacts by asteroids. Utilizing this geological time scale, scientists have recently designated the Anthropocene as the forthcoming significant epoch.

In this visual representation, the Visual Capitalist team delves into the depths of Earth's geological timeline to unveil the transitions between epochs, shedding light on the specific occurrences that demarcate these distinct eras.

Anthropocene

Earth's geological past is categorized into numerous distinct units, spanning from expansive eons down to specific ages. The duration of each unit varies, shaped by significant occurrences, such as the disappearance and emergence of new species.

Imagine slicing a mountain in half—an intriguing tapestry of layers would come into view, each narrating the progression of time. These strata are distinguished by variations in chemical composition and the sediment amassed over the ages.

Certain divisions are particularly clear and extensively apparent in the geological record, earning them the moniker "golden spikes." These distinctive markers can encompass changes of climatic, magnetic, biological, or isotopic (chemical) characteristics.

The Earth's journey has encompassed numerous epochs, culminating in the contemporary Anthropocene era.

These periods span diverse epochs, such as the Early Devonian, initiating the emergence of initial shell organisms 400 million years ago, and the trio of Jurassic epochs, witnessing the ascendancy of dinosaurs as predominant land vertebrates.

For the past 11,700 years, we've resided in the Holocene epoch, a notably steady phase that facilitated the rise of human civilization. Yet, in the wake of millennia of human influence, this epoch is rapidly yielding to the arrival of the Anthropocene.

The Anthropocene is characterized by a multitude of marks left on the Earth, such as the widespread dispersion of plastic particles and a conspicuous rise in carbon dioxide levels within sediments.

Epoch

Its start (MYA = Million Years Ago)

Anthropocene

70 Years Ago

Holocene

0.01 MYA

Pleistocene

2.58 MYA

Pliocene

5.33 MYA

Miocene

23.04 MYA

Oligocene

33.90 MYA

Eocene

56.00 MYA

Paleocene

66.00 MYA

Cretaceous

145.0 MYA

Jurassic

201.40 MYA

Triassic

251.90 MYA

Lopingian

259.50 MYA

Guadalupian

273.00 MYA

Cisuralian

300.00 MYA

Pennsylvanian

323.40 MYA

Mississippian

359.30 MYA

Devonian

419.00 MYA

Silurian

422.70 MYA

Ludlow

426.70 MYA

Wenlock

432.90 MYA

Llandovery

443.10 MYA

Ordovician

486.90 MYA

Furongian

497.00 MYA

Miaolingian

521.00 MYA

Terreneuvian

538.80 MYA

The most unequivocal indicator of this shift in the geological era, and the designated "golden spike" for the Anthropocene, is the presence of radioactive plutonium resulting from nuclear tests in the 1950s.

The best example has been discovered in the sediment of Ontario's Crawford Lake. This lake features two separate layers of water that remain distinct, causing settling sediments to accumulate in discernible strata at the lakebed across time.

Although the International Commission on Stratigraphy proclaimed the inception of the new epoch in July 2023, Crawford Lake's recognition as the epoch-defining site is still pending. If chosen, our planet will formally enter the Crawfordian Age of the Anthropocene.

To learn more about Anthropocene, have a look at the following books and movies:

This post may contain affiliate links. As an Amazon Associate, I earn from qualifying purchases.


Comments

Popular posts from this blog

Find cities with similar climate

This map has been created using The Global environmental stratification. The Global environmental stratification (GEnS), based on statistical clustering of bioclimate data (WorldClim). GEnS, consists of 125 strata, which have been aggregated into 18 global environmental zones (labeled A to R) based on the dendrogram. Interactive map >> Via www.vividmaps.com Related posts: -  Find cities with similar climate 2050 -  How global warming will impact 6000+ cities around the world?

The Appalachian Mountains, the Scottish Highlands, and the Atlas Mounts in Africa were the same mountain range

The Central Pangean Mountains was a prominent mountain ridge in the central part of the supercontinent Pangaea that extends across the continent from northeast to southwest through the Carboniferous , Permian Triassic periods. The mountains were formed due to a collision within the supercontinents Gondwana and Laurussia during the creation of Pangaea. It was comparable to the present Himalayas at its highest peak during the start of the Permian period. It isn’t easy to assume now that once upon a time that the Scottish Highlands, The Appalachian Mountains, the Ouachita Mountain Range, and the Atlas Mountains in northwestern Africa are the same mountains , once connected as the Central Pangean Mountains.

Moose population in North America

The moose population in North America is shrinking swiftly. This decrease has been correlated to the opening of roadways and landscapes into this animal's north range.   In North America, the moose range includes almost all of Canada and Alaska, the northern part of New England and New York, the upper Rocky Mountains, northern Minnesota and Wisconsin, Michigan's Upper Peninsula, and Isle Royale.    In 2014-2015, the North American moose population was measured at around one million animals. The most abundant moose population (about 700,000) lives in Canada. About 300 000 moose remains in nineteen U.S. states Alaska, Colorado, Connecticut, Idaho, Maine, Massachusetts, Minnesota, Montana, Michigan, Nevada, New Hampshire, New York, North Dakota, Oregon, Utah, Vermont, Washington, Wisconsin, and Wyoming. The largest moose specimens are found in Alaska 200 thousand moose. Below the map shows the size of US states scaled by the moose population.     Via www.vividmaps.com