Group Formation and initial Idea
Over the past couple of days Liam and I have been discussing our ideas together and I have to say I am quite intrigued by his concept. Through some development we decided to work together which could prove quite interesting as neither of us have any background in textiles.
Based on the evidence we leave behind, how will the dominant, intelligent species in a future geological age view anthropogenic humans?
We have no images or videos of real life dinosaurs however we all know what a T-rex looks like. Over the years of discovering fossils we have reconstructed these creatures and imagined what they would have looked like when they were roaming the Earth. The same thing will happen about us in the future. We will leave geological markers (like fossils) which will be preserved for thousands even millions of years and will one day be discovered by the dominant, intelligent species of that era. Liam and I are imagining that these discoveries are made in a world were there is no documentation of modern day humans (books, images, video) and the only way to know we were here would be to look through the Earth’s strata.
The final product will be what we imagine to be their interpretation of what humans would have looked like based on the geological markers we have left behind.
Today was to research what the current key markers of the Anthropocene are and what else could be something that we leave behind. The obvious stand out is the Plastiglomerate I mentioned in my previous post which is rock that has formed with melted plastic in it. This has been the big wake up call that tells us that we have entered this new geological epoch. However, it is thought that the Anthropocene actually began in 1945 after the Trinity test. The first test of a nuclear weapon that left the local area around the test site in New Mexico with radioactive ions and general nuclear fallout. This fallout has since been observed globally after the constant thermonuclear weapon testing that occurred between 1950-1980.
Another anthropogenic marker is black carbon particles found in ice cores and and rock strata which are the result of fossil fuel burning. The black carbon is too small to notice in the air but over time it deposits and is trapped and preserved. On top of that the minerals and rocks in the Earth have changed. Prior to the 19th century, aluminium was very rare in a native form and since then 98% of all of the aluminium we have today has been manufactured by humans. This increase also goes hand in hand with the introduction of concrete to the environment which was first invented by the Romans and is still used today.
Something that is not quite existent but is definitely on its way to happening is the introduction of technofossils to the land. Technofossils are fossilised traces of technologies used over time. The idea was initially proposed when pre-human primate tools were discovered. Developing on from that the technofossils we will leave behind will be a little more advanced (Phones, computers, TV’s, etc...). There are already mass e-waste dumps in Africa which hold thousands of old electrical components which will be preserved over time.
We are not looking at how we will show these markers on a garment yet but we have had a couple of ideas. The next step will be to talk to Miranda and see what the progression to a garment would be but for I now we are happy that we have a solidified pair and an idea that is still quite abstract and provides many creative avenues to take it down.
Black carbon
Novakov, T., Ramanathan, V., Hansen, J. E., Kirchstetter, T. W., Sato, M., Sinton, J. E., & Sathaye, J. A. (2003). Large historical changes of fossil‐fuel black carbon aerosols. Geophysical Research Letters, 30(6).
Radionuclides
Waters, C. N., Syvitski, J. P., Gałuszka, A., Hancock, G. J., Zalasiewicz, J., Cearreta, A., ... & Barnosky, A. (2015). Can nuclear weapons fallout mark the beginning of the Anthropocene Epoch?. Bulletin of the Atomic Scientists, 71(3), 46-57.
Zalasiewicz, J., Waters, C. N., Williams, M., Barnosky, A. D., Cearreta, A., Crutzen, P., ... & Haff, P. K. (2015). When did the Anthropocene begin? A mid-twentieth century boundary level is stratigraphically optimal. Quaternary International, 383, 196-203.
Plastics
Corcoran, P. L. (2015). Benthic plastic debris in marine and fresh water environments. Environmental Science: Processes & Impacts, 17(8), 1363-1369.
Jambeck, J. R., Geyer, R., Wilcox, C., Siegler, T. R., Perryman, M., Andrady, A., ... & Law, K. L. (2015). Plastic waste inputs from land into the ocean. Science, 347(6223), 768-771.
Aluminium & Concrete
Waters, C. N., Zalasiewicz, J., Summerhayes, C., Barnosky, A. D., Poirier, C., Gałuszka, A., ... & Jeandel, C. (2016). The Anthropocene is functionally and stratigraphically distinct from the Holocene. Science, 351(6269), aad2622.
Technofossils
Zalasiewicz, J., Williams, M., Waters, C. N., Barnosky, A. D., & Haff, P. (2014). The technofossil record of humans. The Anthropocene Review, 1(1), 34-43.