sj-docx-2-anr-10.1177_20530196221147607 – Supplemental material for The San Francisco Estuary, USA as a reference section for an Anthropocene series

Supplemental material, sj-docx-2-anr-10.1177_20530196221147607 for The San Francisco Estuary, USA as a reference section for an Anthropocene series by Stephen Himson, Mark Williams, Jan Zalasiewicz, Colin Waters, Mary McGann, Richard England, Bruce E Jaffe, Arnoud Boom, Rachael Holmes, Sue Sampson, Cerin Pye, Juan Carlos Berrio, Genevieve Tyrrell, Ian P Wilkinson, Neil Rose, Pawel Gaca and Andrew Cundy in The Anthropocene Review</p

sj-docx-3-anr-10.1177_20530196221147607 – Supplemental material for The San Francisco Estuary, USA as a reference section for an Anthropocene series

Supplemental material, sj-docx-3-anr-10.1177_20530196221147607 for The San Francisco Estuary, USA as a reference section for an Anthropocene series by Stephen Himson, Mark Williams, Jan Zalasiewicz, Colin Waters, Mary McGann, Richard England, Bruce E Jaffe, Arnoud Boom, Rachael Holmes, Sue Sampson, Cerin Pye, Juan Carlos Berrio, Genevieve Tyrrell, Ian P Wilkinson, Neil Rose, Pawel Gaca and Andrew Cundy in The Anthropocene Review</p

Palaeontological signatures of the Anthropocene are distinct from those of previous epochs

 The “Great Acceleration” of the mid-20th century provides the causal mechanism of the Anthropocene, which has been proposed as a new epoch of geological time beginning in 1952 CE. Here we identify key parameters and their diagnostic palaeontological signals of the Anthropocene, including the rapid breakdown of discrete biogeographical ranges for marine and terrestrial species, rapid changes to ecologies resulting from climate change and ecological degradation, the spread of exotic foodstuffs beyond their ecological range, and the accumulation of reconfigured forest materials such as medium density fibreboard (MDF) all being symptoms of the Great Acceleration. We show: 1) how Anthropocene successions in North America, South America, Africa, Oceania, Europe, and Asia can be correlated using palaeontological signatures of highly invasive species and changes to ecologies that demonstrate the growing interconnectivity of human systems; 2) how the unique depositional settings of landfills may concentrate the remains of organisms far beyond their geographical range of environmental tolerance; and 3) how a range of settings may preserve a long-lived, unique palaeontological record within post-mid-20th century deposits. Collectively these changes provide a global palaeontological signature that is distinct from all past records of deep-time biotic change, including those of the Holocene. </p