Anthropocene epoch stratotype specimen
c. 0001900 BCE +\- 1ma
​
This is an example of a portrayal of climate change and climate change over time. This review [is] proved to be possible. There are many areas involving agriculture, carbon and widespread destruction, and some historians say that the increase in temperature is increasing. People of the world. Yes, YM [sic] supports the concept of Eocene humans, partly as a biology teacher.
​
Note: The chasm between our lingua franca and the language used by the future curators has become a main obstacle for us to translate and understand the interpretation text they have provided. From our endeavour, though, we may infer that the future curators generally believe the piece of specimen has demonstrated the change of climate.
​
IMoB 6382.9
Curator
human, future
mid-Anthropocene
Anthropocene Stratotype Specimen
0001900 BCE +\- 1ma
Nova Gondwana
Geological epochs are defined in relation to a global stratotype section that identifies a boundary marking a long-term shift in global geological processes. This stratotype section contains evidence of the golden spikes that indicate widespread global changes occurring at the Holocene-
Anthropocene boundary mass extinction, when vertebrate numbers rapidly decline, and mega faunal insects radically increase in ferocity and abundance.
​
IMoB 6382.9-1
Curator
human, 0002035 CE
early-Anthropocene
Anthropocene epoch stratotype specimen
c. 0001900 BCE +\- 1ma
​
This stratotype section contains evidence of the golden spikes that indicate widespread global changes occurring at the Holocene-Anthropocene boundary mass extinction, when terrestrial non-avian vertebrates declined to extinction and mega faunal insects radically increased in variety and abundance.
​
IMoB 6382.9
Curator
non-human, far-future
Novacene
Anthropocene epoch stratotype specimen
c. 0001900 BCE +\- 1ma
​
This Anthropocene ’stratotype’ specimen is evidence of paleogeological fraud in the misrepresentation of geological evidence during the 'Anthropocene Controversy'. This is the misidentification of human-induced global climatic warming effects in the Late Holocene interglacial. This led to the transitory definition of the ‘Anthropocene’ as a new geological epoch, which was later corrected by the Global Union of Geological Sciences, following the designation of the late Quaternary/Quinary boundary. The Quinary Ice Age epoch has been characterised by global cooling, sea level decline, and sustained glaciation, that may have been avoided if our human ancestors had acted more quickly to prevent the inevitable climatic cooling of the Late Quaternary.
​
IMoB 6382.9
Curator
human, far-future
Quinary epoch
_edited.png)
Take a little piece of the future home with you!
Find products related to this exhibit for sale in our museum shop.
.png)
artist/creator
Dean Sully