Greater effective soil age in little-eroded uplands soils means a longer time for the accumulation of recalcitrant organic matter in older soils—and probably more importantly, it allows the accumulation of noncrystalline minerals that stabilize soil organic matter.We further suggest that the patterns for total P are more complex because its pools reflect both weathering and loss and retention by both organic matter and mineral adsorption, which are greater in the upland slope positions.Overall, these results illustrate that erosion and deposition have a rejuvenating effect on the supply of rock-derived nutrients in these valley landscapes —one that suffices to make both lower slope and alluvial soils fertile enough to support intensive pre-contact agricultural systems in both valleys despite the infertility of the upland soils surrounding them.However,differences in the structures of the valleys influenced their ability to support intensive agriculture prior to European contact.Halawa Valley and other large valleys on older islands have well-developed colluvial aprons surrounding their alluvial floors.In contrast, Pololu¯ Valley lacked the potential for lower-slope rainfed agriculture because the high subsidence rate of Hawai’i Island causes a sharp transition between slopes too steep to cultivate and the nearly flat valley floor —a process that is accentuated by the rapid glacial-melt-driven sea level rise of the past approximately 20 ky.Other major valleys on Kohala Volcano have similar structures—including the largest, Waipi’o Valley, which was a major center of precontact Hawaiian settlement.Considering only the area bounded by the cliff tops on the valley sides and waterfalls at the head of the valleys,flood and drain table differences in subsidence rates and corresponding in-fill histories cause large differences in the distribution of slopes suitable for agriculture within Pololu¯ and Halawa.
Assuming that slopes of less than 5 could have been made suitable for intensive pond field systems, 17% of the 423 ha surface of Pololu¯ Valley could support pond fields ; only 6% of the 692 ha surface of Halawa Valley had slopes less than 5.Further, assuming that 12 represents an upper threshold for intensive rainfed agriculture, 16% of Halawa Valley has slopes between 5 and 12 , as opposed to only 5% of Pololu¯ Valley.Available archaeological evidence for pre-contact agricultural systems in Pololu¯ and Halawa is consistent with our findings on valley topography and soil fertility.Tuggle and Tomonari-Tuggle found evidence for both irrigated and rainfed fields on the flat alluvial floor of Pololu¯.They attribute the fact that not all the Pololu¯ alluvium was irrigated to the valley’s hydrologic conditions; the valley floor is so large relative to its watershed area that stream flow was inadequate to have watered the entire valley floor.In Halawa Valley, the entire area of alluvium was converted to irrigated pond fields, which also extended onto the lower colluvial slopes.More importantly, well-defined rainfed cultivation plots with stone-faced terraces and walls extend well up the colluvial slopes in Halawa, encompassing an area greater than the total area of irrigated pond fields there.Rosendahl mapped the Kapana area of Halawa Valley, providing a detailed example of intensive rainfed agricultural terraces, integrated with habitation sites and small temples.Significantly, mid-nineteenth century land records from Halawa demonstrate that most claimants included both irrigated as well as rainfed areas in their claims , showing that the two kinds of agriculture were integral parts of the overall production system at the household level.The broader implications of this potential for intensive rainfed agriculture on colluvial slopes of the valleys on the older islands in the Hawaiian Archipelago are substantial.Analyses of the distribution of intensive agricultural systems and their consequences for the dynamics of Hawaiian society have considered irrigated and rainfed systems to have been spatially separated, due to the very different ecosystem and landscape properties that favor their development.
Because these types of agricultural systems differ both in their ability to produce a surplus over agricultural labor and in their vulnerability to drought—with both comparisons favoring the irrigated pond field systems—these contrasting systems could have contributed to the development of rather different societies, in areas or on islands dominated by one system or the other.The islands of Hawai’i and to a lesser extent Maui were based largely upon intensive rainfed systems, with only a few well-watered irrigated valleys.In contrast, the older islands in the archipelago have been thought to be based mostly upon irrigated pond field systems.However, the evidence here suggests that the older islands likely maintained integrated pond- field/rainfed systems and that, as in Halawa Valley, the peripheral rainfed systems could have covered a larger area than did irrigated pond fields.A similar pattern has been suggested in the leeward Makaha Valley of O’ahu, where archaeological survey confirmed the presence of extensive areas of dryland gardening on colluvial slopes, but where irrigation was confined to smaller areas in the valley interior.The potential for developing integrated pond- field/rainfed systems on colluvial slopes on the older islands strengthens the contrast between the agricultural production potential of Hawai’i Island versus the older islands.It has been suggested that pressures to maintain surplus production in rainfed, drought-prone agricultural areas could have driven the elites of Hawai’i Island towards marriage alliances with elites of the older islands, and/or towards conquest of those islands —and the development of integrated pond field/rainfed systems on the older islands would only have increased their attractiveness as potential acquisitions.Moreover, integrated systems on the older islands could have boosted their potential agricultural yields, and the diversity of foods they could produce, to levels approaching the total productivity of the much larger island of Hawai’i.These dynamics should be incorporated into our understanding of the dynamics of Hawaiian society, and those of other indigenous societies in which similar dynamics could occur.For the vast majority of our evolutionary history, humans subsisted by hunting animals and gathering plants.
Around 12,000 years ago, we began to take a more direct role in the process of food production, domesticating animals and cultivating crops in order to meet our nutritional requirements.This subsistence revolution is thought to have occurred independently in a limited number of places.This new way of life is arguably the most important process in human history, and its dramatic consequences have set the scene for the world we live in today.Agricultural productivity, and its variation in space and time, plays a fundamental role in many theories of human social evolution, yet we often lack systematic information about the productivity of past agricultural systems on a scale large enough to test these theories properly.Here, we outline how explicit crop yield models can be combined with high quality historical and archaeological information about past societies in order to infer how agricultural productivity and potential have changed temporally and geographically.The paper has the following structure: First, we introduce the ways in which agriculture is involved in theories about human social evolution, and stress the need to scientifically test between competing hypotheses.Second, we outline what information we need to model about past agricultural systems and how potential agricultural productivity and carrying capacity can provide a useful way of comparing societies in different regions and time periods.Third, we discuss the need for a systematic, comparative framework for collecting data about past societies.We introduce a new databank initiative we have developed for collating the best available historical and archaeological evidence.We discuss the kinds of coded information we are collecting about agricultural techniques and practices in order to inform our modelling efforts.We illustrate this task by presenting three short case studies summarizing what is known about agricultural systems in three different regions at various time periods.We discuss the challenges confronting this approach, and the various limitations and caveats that apply to the task at hand.Fourth, we outline how we can combine a statistical approach of modelling past crop productivity based on climate inputs with the kind of historical information we are collecting.The development of agriculture and the ways it has spread and intensified are fundamental to our understanding of the human past.For example, authors such as Renfrew, Bellwood, and Diamond argue that early agricultural societies enjoyed a demographic advantage over hunter-gatherers, which fueled a series of population expansions resulting in agriculturalists spreading out to cover much of the world, taking their culture and languages along with them.At the beginning of the European age of exploration, agricultural societies had pushed the distribution of forager populations in the Old World to only those places that were marginal for agriculture.
Widespread forager populations were present in the Americas and Australia, but these too eventually gave way to agricultural populations of European origin.Agriculture raised the carrying capacity of the regions in which it developed and spread,rolling bench leading to people living at higher densities with a more sedentary way-of-life than was previously possible.However, the development of agriculture did not stop there.Further improvements in agricultural technologies and techniques, and processes such as artificial selection further raised the productivity of agriculture and the size of the population that could be supported in any one region.These improvements ultimately enabled humans to live in large urban conglomerations with extremely high population densities.Influential models of agricultural innovation, starting with the work of Esther Boserup , argue that advances occur in response to increases in population, and the subsequent decreasing availability of land.This drives farmers to invest more labor in producing food.In other words, there is feedback in the system that leads to the increasing intensification of agriculture.These processes of intensification, whatever their cause, can occur in a number of different ways and have had important consequences.From the fields and hedgerows of Northern Europe to the mountainside rice terraces of the Ifugao of the Philippines , through to the deforested slopes of Easter Island , agricultural populations have dramatically altered the landscapes around them.Agriculture is central to many theories about how larger-scale complex societies evolved.Under functionalist views of social complexity more productive agricultural systems allowed for ‘surplus’ production, and enabled a more extensive division of labor.This surplus production allowed for individuals who did not grow their own food, enabling the creation of specialized managers and rulers, and occupational artists and artisans.It is argued that this division of labor increases efficiency and coordination, enabling more complex societies to out-compete less complex societies either directly or indirectly.Under this view, not only is a rich resource base a necessary condition for the emergence of complex societies, but it is also a sufficient one.If this is correct, it follows that differences in agricultural productivity can explain why some regions developed more complex societies than others.Changes in agricultural intensity have also been linked to changes in the ritual and religious life of human groups.It is argued that hunter-gathers and early agriculturalists, who lived in small groups and faced high risks from hunting of large animals, tended to participate in dysphoric, “imagistic” rituals that, although rarely experienced, are typically emotionally intense.Such rituals act as a mechanism for creating social cohesion via ‘identity fusion’.A greater dependence on agriculture led to increased group sizes, and required different forms of cooperation and coordination in order to successfully produce food.New ritual forms developed that were organized around daily or weekly cycles but with less intense emotional experiences.It is argued that this ‘routinization’ enabled strangers to recognize and identify with others as members of a common in-group, enabling trust and cooperation on a hitherto unknown scale.It is clear that agriculture is of fundamental importance to studies of the human past.The ideas outlined above represent just a flavor of the ways agriculture and agricultural productivity enter into our understanding of the long-term patterns and processes of human history.
Importantly, these ideas are hypotheses that require testing against other plausible narratives.For example, it has been argued that an important factor driving the evolution of complex societies was intensive forms of conflict between nomadic pastoralists and settled agrarian societies that selected for increasingly larger and more cohesive societies.Thus, complex societies tended to emerge on the border of the Eurasian Steppe and spread out from there.Under this view, agriculture is seen as necessary but not sufficient to explain the observed variation about where and when such societies developed.When attempting to understand the past we should seek to test between competing hypotheses, rather than simply focusing on a single favored idea.In order to do this, it is important to have relevant data on past agricultural systems and their productivity and potential.These systems exhibit a great deal of variation, and are of varying levels of intensity.To enable more direct comparisons across different regions and time periods, it will be important to have explicit models that translate different agricultural systems across space and time into a common currency.This will allow us to perform statistical analyses so that we can directly test alternative hypotheses.