Holocene
stability
anthropocene
the modern era, dominated by humans (agriculture began 10 000 years ago when it was warm and stable. people became less nomadic)
1950-present
the great acceleration
people and resource use
7 billion people
1 billion in 1800 (took 100 000 years)
energy usage has increased - fossil fuels (1750-1800)
land usage has increased
ecological footprints
quantification of human claims on the global resources by adding up energy, food, materials and services and estimating land usage
nitrogen
fertiliser usage
140 million tonnes of fixed nitrogen added each year - comparable to microbe fixation
10% in food
rest washes off
denitrifying bacteria return it to atmosphere - some as N2O (greenhouse gas)
eutrophication
added nutrients lead to increase in algae and cyanobacteria - heterotrophic organisms feed on algae and cyanobacteria - aerobic respiration decreases O2 in water creating dead zones
phosphate fertilster
run off - eutrophication
what can be done?
increase yield, not land usage
genetic engineering - increase yield, nutritional value and pest resistance
reduce food spoilage