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An international team of scientists has identified pivotal parameters that signify the onset of the Anthropocene epoch, which is proposed to have begun in 1952 CE. This epoch, marked by profound human impact on on the Earth's geology and ecosystems, is defined by the "Great Acceleration" that began in the mid-20th century.

The "Great Acceleration" has led to significant changes in biogeographical ranges for both marine and terrestrial species, rapid ecological shifts due to climate change and environmental degradation, and the widespread dissemination of exotic species beyond their native habitats. Additionally, the accumulation of human-made materials such as medium density fiberboard is highlighted as a hallmark of this new epoch. 

The study, published in Earth-Science Reviews, outlines several critical paleontological signals that characterize this period of rapid environmental change.

Key findings from the study include: 

  1. Global Paleontological Signatures: The researchers demonstrated how paleontological records from continents including North America, South America, Africa, Oceania, Europe, and Asia can be correlated to ecological shifts and the spread of highly invasive species, underscoring the increasing interconnectivity of human systems and their lasting impacts. 

  1. Unique Depositional Settings of Landfills: The study highlights how landfills, as unique depositional environments, can concentrate the remains of organisms far beyond their natural geographical and environmental ranges. 

  1. Preservation of Anthropocene Records: Various settings, from urban landscapes to remote areas, are identified as potential sites for preserving long-lived, unique paleontological records. These records within post-mid-20th century deposits are distinct from all past records of biotic change, including those from the Holocene epoch.

Photo collage of examples of invasive species likely to leave a fossil record

The study provides compelling evidence that the Anthropocene epoch is marked by a global paleontological signature unlike any other in Earth's history. This signature includes the breakdown of discrete biogeographical ranges, rapid ecological changes, the spread of non-native species, and the accumulation of human-made materials.

As scientists continue to study and debate the formal recognition of the Anthropocene as a distinct geological epoch, this research offers crucial insights into the defining characteristics and global reach of human influence on the Earth's systems. 

Diagram showing late 20th and 21st century production of cultivated fruits and vegetables and fiberboard
Late 20th and 21st century production of avocados, coconuts, mangos, peach, walnut, palm kernels, snails and medium-density fiberboard.

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