The establishment of farming is a pivotal moment in human history, setting the stage for the development of class-based society and urbanization. Determining the nature of early farming and how farming practices evolved with increased societal complexity is therefore key to understanding the development of early urban civilizations.
Our research takes a new interdisciplinary approach, combining archaeobotany, plant stable isotope chemistry and functional plant ecology, to reconstruct not only what crops were grown, but also how farming was practiced.
Our recent paper (Bogaard et al. 2015) provides a worked example of combining plant stable isotope chemistry and functional plant ecology, to characterise a series of modern extensive (low input) and intensive (high input) farming regimes.
Carbon and nitrogen stable isotope analysis of archaeobotanical crop remains can be used to infer agricultural intensity in two complementary ways. First, there is a clear impact of animal manure application on crop stable nitrogen isotope ratios; the volatization of the lighter 14N isotope in ammonia results in soil nitrates and plants enriched in the heavier 15N isotope. Secondly, carbon stable isotope analysis can be used to infer crop water status and hence potentially irrigation in arid climates.
These newly established ‘tools’ for inferring central aspects of agricultural practice can be combined to infer labour inputs through manuring and/or watering. These inferences are highly complementary. For example, manuring has a ‘slow-release’ effect on soils—only c. 5-25% of nitrogen being mobilized in the first year after application—and so provides an index of intensity as a long-term investment in land. Watering, by contrast, is required at regular intervals through the growing season in arid climates. Moreover, distinct regimes can be differentiated through variability in the intensity of inputs; thus, for example, hand-watering of pulses in a small-scale ‘garden’ setting is characterized by more variable watering levels and hence carbon isotope values than large-scale gravity-flow systems.
Functional plant ecology
Functional plant ecology infers the ecological potential of plant (here, weed) species on the basis of morphological and behavioural attributes that have an explicit functional significance. Thus, for example, weed species, which can develop large leafy canopies, are able to compete successfully for nutrients and light and so to dominate fertile situations. Measuring the canopy dimensions of established specimens of a species at a number of locations makes it possible to assess their maximum canopy size and hence this functional aspect of their competitive ability. Species adapted to conditions that are both fertile and highly disturbed, however, tend to have smaller canopies but a distinct ability to grow rapidly, a characteristic that is correlated with a set of leaf characteristics, such as the ratio of leaf area to dry weight (specific leaf area). Yet another set of functional attributes (e.g. small canopy size, low specific leaf area) characterize plants that are successful in nutrient-limited habitats. By measuring the functional attributes of weed species represented as seeds accompanying crops in archaeobotanical assemblages, it is possible to compare them with a series of modern analogue weed floras developed under known conditions to infer the nature of the farming regime.