What Is: The Anthropocene

Image Credit: Scientific Frontline / stock image

The Definition of a New Reality

The term "Anthropocene" has transcended its origins in the quiet corridors of stratigraphy to become the defining cultural, philosophical, and scientific concept of the twenty-first century. It proposes a fundamental rupture in Earth history; the moment when human activity ceased to be a mere biological presence on the surface of the planet and became a geological force capable of determining the trajectory of the Earth system itself. This concept suggests that the Holocene—the geological epoch that began approximately 11,700 years ago at the end of the last Ice Age and provided the stable climatic conditions necessary for the development of agriculture and human civilization—has ended. In its place, we have entered a new, volatile interval characterized by the pervasive alteration of the atmosphere, hydrosphere, cryosphere, and biosphere by a single species.  

While the term implies a new geological "epoch" following the Holocene, its formal status remains a subject of intense scientific adjudication and controversy. In March 2024, the International Union of Geological Sciences (IUGS) officially rejected the proposal to formalize the Anthropocene as a chronostratigraphic unit within the Geological Time Scale. However, this rejection has not diminished the concept's utility or its permeation into global discourse; rather, it has reoriented the scientific community toward viewing the Anthropocene as a diachronous, unfolding geological "Event" rather than a strictly defined epoch with a singular start date. This distinction is profound, shifting the focus from a search for a "golden spike" on a timeline to a broader recognition of a transformation comparable to the Great Oxidation Event of deep time.  

Growth of coral reefs likely cannot keep pace with rising sea level

The upper panel shows a coral reef margin in Belize with living branched Acropora (elkhorn) and platy Millepora (fire) corals, which are both competitive and fast-growing. The lower panel shows broken branches of dead Acropora corals overgrown by weedy, fertile hill and finger corals (Porites) as well as fleshy algae.
Photo Credit: E. Gischler.

In identifying and dating coral remains in drill cores taken from Belize reefs, a team of experts from Goethe University Frankfurt and partners from Germany, the USA and Canada has shown the importance of specific types of coral for reef-building during the current Holocene geological epoch, dating back some 12,000 years. The scientists found that certain coral species disappeared for longer periods in the past due to climate changes, and identified another climate-related threat to coral reefs: In addition to warming and ocean acidification, among others, the rising sea level also threatens coral reefs, whose growth rates cannot keep up. 

Tropical coral reefs could end up being one of the first victims of climate change. The marine diversity hotspots are threatened by and declining as a result of global warming, ocean acidification, a deterioration of water quality, as well as diseases of reef-building organisms, and their growth is unable to keep up with the projected rise in sea levels. These are some of the conclusions drawn by an interdisciplinary team of scientists from Goethe University Frankfurt's Institute of Geosciences, the company ReefTech Inc., the GEOMAR Helmholtz Center of Ocean Research, the University of Ottawa's Department of Earth and Environmental Sciences, and the GSI Helmholtz Center of Heavy Ion Research. Their findings are based on an examination of 22 drill cores collected from the Belize barrier reef and atolls, the largest reef system in the Atlantic Ocean, which focused on identifying and dating coral growth and accretion rates over the past 9,000 years. 

What Is: An Ecosystem

The Holocoenotic Nature of the Biosphere
Image Credit: Scientific Frontline / stock image

The Genesis of a Paradigm 

The concept of the ecosystem represents one of the most significant intellectual leaps in the history of biological science. It is not merely a label for a collection of living things, but a sophisticated framework that integrates the chaotic multiplicity of the natural world into a coherent, functional unit. To understand the ecosystem is to understand the fundamental architecture of life on Earth. This report provides an exhaustive analysis of the ecosystem concept, tracing its historical lineage, dissecting its thermodynamic and biogeochemical engines, exploring its diverse manifestations across the globe, and evaluating its resilience in the face of unprecedented anthropogenic pressure. 

Climate catastrophe produced instantaneous evolutionary change

A geocolor enhanced image captured by weather satellite GOES-16 shows Hurricane Harvey in the Gulf of Mexico as daylight approached Aug. 24, 2017, with nighttime features to the storm’s left and daytime features to its right.
Photo Credit: NOAA/NASA GOES Project

With species the world over on the move due to climate change, a unique experiment in the wake of 2017’s Hurricane Harvey has revealed a way that species can instantly evolve when they move in response to a climate catastrophe.

“With the profound and rapid changes, we’re seeing with the environment, movement is becoming critical for species’ survival,” said Rice University evolutionary biologist Scott Egan, senior author of a study published this week in Nature Ecology and Evolution. “The takeaway from this study is that while natural selection is still incredibly important, there’s another form of evolutionary change that’s directly related to movement, and it could make a huge difference in the evolution of organisms.”

Harvey, the most intense rainfall event in U.S. history, stalled over southeast Texas and dropped more than three feet of rain over thousands of square miles in a matter of days. Record flooding in and around Houston produced “mini extinctions” of insects and other species in areas that remained inundated for 10 or more days.

Farmers boosted Europe's biodiversity over the last 12,000 years

Standing stones in Carnac, France. Built between 6,500 - 5,300 years ago by Europe's first farmers.
 Photo Credit: Jonny Gordon.

Although humans are to blame for nature’s recent decline, a new study shows that for millennia, European farming practices drove biodiversity gains, not losses. 

Standing stones in Carnac, France. Built between 6,500 - 5,300 years ago by Europe's first farmers. Picture by Jonny Gordon. 

A team of researchers at the University of York analyzed fossil pollen records from Europe to track vegetation changes stretching back 12,000 years. They discovered that as new populations of farmers from Turkey moved into Europe 9,000 years ago, far from destroying plant diversity, they enriched it. 

Dr Jonny Gordon is a Postdoctoral Research Associate in the Leverhulme Centre for Anthropocene Biodiversity and lead author of the new paper, Increased Holocene diversity in Europe linked to human-associated vegetation change, which has been published in Global Ecology and Biogeography. 

What Is: Extinction Level Events

A Chronicle of Earth's Biotic Crises and an Assessment of Future Threats
Image Credit: Scientific Frontline

Defining Biotic Catastrophe

The history of life on Earth is a story of breathtaking diversification and innovation, but it is punctuated by chapters of profound crisis. These are the extinction level events—catastrophes of such magnitude that they fundamentally reset the planet's biological clock. Popular imagination often pictures a single, sudden event, like the asteroid that sealed the fate of the dinosaurs. The geological reality, however, is more complex and, in many ways, more instructive for our current era. Understanding these events requires a rigorous scientific framework that moves beyond simple notions of species loss to appreciate the systemic collapse of entire global ecosystems.

What Is: The Phanerozoic Eon

Defining the Eon of Complex Life
Image Credit: Scientific Frontline / AI generated

The Phanerozoic Eon constitutes the current and most biologically dynamic division of the geological time scale. Spanning the interval from approximately 538.8 million years ago (Ma) to the present day, it represents roughly the last 12% of Earth's 4.54-billion-year history. Despite its relatively short duration compared to the preceding Precambrian supereon—which encompasses the Hadean, Archean, and Proterozoic eons—the Phanerozoic contains the overwhelming majority of the known fossil record and the entirety of the history of complex, macroscopic animal life.  

Boreal forest and tundra regions worst hit over next 500 years of climate change, study shows

The boreal forest is the Earth's most significant provider of carbon storage and clean water
Photo Credit: Landon Parenteau

The boreal forest, covering much of Canada and Alaska, and the treeless shrublands to the north of the forest region, may be among the worst impacted by climate change over the next 500 years, according to a new study.

The study, led by researchers at the White Rose universities of York and Leeds, as well as Oxford and Montreal, and ETH, Switzerland, ran a widely-used climate model with different atmospheric concentrations of carbon dioxide to assess the impact climate change could have on the distribution of ecosystems across the planet up to the year 2500.

Most climate prediction models run to the year 2100, but researchers are keen to explore longer-term projections that give a global picture of how much humans, animals and plant-life may need to adapt to climate change beyond the next century, which is important as long-lived trees adapt at scales of centuries rather than decades.

Biological crusts influence the climate

Biological soil crusts strengthen the soil and ensure that less sand is stirred up and thus fewer dust particles are released into the atmosphere.
Credit: Emilio Rodriguez-Caballero

A surface layer of bacteria, fungi and lichen amongst others reduces the amount of dust stirred up into the atmosphere

When bacteria, fungi, mosses, lichens and algae combine on dry land, they form so-called biological soil crusts. These cover about twelve percent of the total global land surface, and up to one third of the surface in dry areas. Biological soil crusts play an important role in consolidating soils, making them more stable and less likely to be stirred up by the wind. Since dust particles in the atmosphere have an impact on the climate, soil crusts fulfil an important function in several respects. An international team of researchers around biologist Bettina Weber of the University of Graz and research associate of the Max Planck Institute for Chemistry provide, for the first time, comprehensive facts and figures on the importance of biological soil crusts for the regional and global dust cycle, both under current and future conditions.

Archaeology and ecology combined sketch a fuller picture of past human-nature relationships

Hunting of a deer. Wall painting, 6th millennium BC. Museum of Anatolian Civilizations, Ankara.
 Image source: Wikimedia Commons

For decades now, archaeologists wielded the tools of their trade to unearth clues about past peoples, while ecologists have sought to understand current ecosystems. But these well-established scientific disciplines tend to neglect the important question of how humans and nature interacted and shaped each other across different places and through time. An emerging field called archaeoecology can fill that knowledge gap and offer insights into how to solve today’s sustainability challenges, but first, it must be clearly defined. A new paper by SFI Complexity Fellow Stefani Crabtree and Jennifer Dunne, SFI’s Vice President for Science, lays out the first comprehensive definition of archaeoecology and calls for more research in this nascent but important field.

While an archaeology or palaeobiology study might examine a particular relationship, such as how humans in New Guinea raised cassowaries during the Late Pleistocene, archaeoecology takes a much broader view. “It’s about understanding the whole ecological context, rather than focusing on one or two species,” Dunne explains.

What Is: Biological Plasticity

Image Credit: Scientific Frontline

The Paradigm of the Reactive Genome 

The history of biological thought has long been dominated by a tension between the deterministic rigidity of the genotype and the fluid adaptability of the phenotype. For much of the 20th century, the Modern Synthesis emphasized the primacy of genetic mutation and natural selection, often relegating environmental influence to a mere background filter against which genes were selected. In this view, the organism was a fixed readout of a genetic program, stable and unwavering until a random mutation altered the code. However, a profound paradigm shift has occurred, repositioning the organism not as a static entity but as a dynamic system capable of producing distinct, often dramatically different phenotypes from a single genotype in response to environmental variation. This capacity, known as biological or phenotypic plasticity, is now recognized as a fundamental property of life, permeating every level of biological organization—from the epigenetic modification of chromatin in a stem cell nucleus to the behavioral phase transitions of swarming locusts, and ultimately to the structural rewiring of the mammalian cortex following injury. 

Wolf protection downgrade highlights need for adaptive conservation frameworks

The protected category means greater flexibility in managing wolf populations
Photo Credit: Marcel Langthim

Following the European Parliament’s historic vote to move wolves from the strictly protected to protected category, experts are calling on policymakers to ensure the change becomes a catalyst for fairer, more adaptive and transparent wildlife management to meet the challenges of successful species recovery.

The protected category means greater flexibility in managing wolf populations

The reclassification reflects a remarkable recovery of the wolf population, having increased by 58% in a decade, with populations of brown bears, lynxes and wolverines also on the rise. 

The protected category affords member states greater flexibility in managing expanding wolf populations, but although protections remain in place, the move has raised fears among conservation groups of widespread culling. 

At the same time, farming and hunting communities and landowner associations see it as necessary to regulate the population and enable management that is adapted to local conditions.