Next Article in Journal
Climate Change and Adaptive Management: Case Study in Agriculture, Forestry and Pastoral Areas
Previous Article in Journal
The Role of Urban Agriculture Technologies in Transformation toward Participatory Local Urban Planning in Rafsanjan
 
 
Font Type:
Arial Georgia Verdana
Font Size:
Aa Aa Aa
Line Spacing:
Column Width:
Background:
Article

Mapping Antebellum Rice Fields as a Basis for Understanding Human and Ecological Consequences of the Era of Slavery

1
Department of Forestry and Environmental Conservation, 261 Lehotsky Hall, Clemson University, Clemson, SC 29634, USA
2
Folk Land Management, 3515 White Hall Road, Green Pond, SC 29446, USA
3
Nemours Wildlife Foundation, 161 Nemours Plantation Drive, Yemassee, SC 29945, USA
4
New South and Associates, Inc., 6150 E. Ponce De Leon Avenue, Stone Mountain, GA 30083, USA
5
Levine Science Research Center, Nicholas School of Environment, Duke University, Durham, NC 90328, USA
6
Department of History, Carnegie Mellon University, 5000 Forbes Avenue, Pittsburgh, PA 15213, USA
*
Author to whom correspondence should be addressed.
Land 2021, 10(8), 831; https://doi.org/10.3390/land10080831
Submission received: 22 June 2021 / Revised: 30 July 2021 / Accepted: 31 July 2021 / Published: 8 August 2021
(This article belongs to the Section Land Systems and Global Change)

Abstract

:
Model systems enlightened by history that provide understanding and inform contemporary and future landscapes are needed. Through transdisciplinary collaboration, historic rice fields of the southeastern United States can be such models, providing insight into how human–ecological systems work. Rice culture in the United States began in the 1670s; was primarily successfully developed, managed, and driven by the labor of enslaved persons; and ended with the U.S. Civil War. During this time, wetlands were transformed into highly managed farming systems that left behind a system of land use legacies when abandoned after slavery. Historically accepted estimates range from 29,950 to 60,703 ha; however, using remotely sensed data (e.g., LiDAR) and expert opinion, we mapped 95,551 ha of historic rice fields in South Carolina, USA. After mapping, the rice fields’ current wetland and land cover characteristics were assessed. Understanding the geographic distribution and characteristics allows insight into the overall human and ecological costs of forced land use change that can inform future landscapes.

1. Introduction

Humans have altered ecosystems on Earth to the point that scientists have dubbed our current era the Anthropocene [1]. Despite the staggering global scale of our recent influence on ecosystem patterns and processes, some of the most profound changes to particular regions and landscapes happened during historical periods [2,3]. Agricultural influences were widespread and transformational, often geographically specific, and technical peaks of exploitation were followed by collapse and reorganization as new socio-ecological pathways emerged [4,5]. Today, features created by humans for agricultural uses and the environments that accompanied them are frequently not counted in current models of ecosystem function and constitute missing sources of variation [2]. Studies attempting to explain current distributions of species are improved by knowing the extent of anthropogenic landscape features, as historically modified ecosystems may influence what is currently observed [6,7]. Wetlands are important ecosystems globally for ecosystem function and are incompletely mapped; little is known about how and where they were modified historically, and such information, when available, can inform present-day ecological analyses and management [8,9].
Globally, millions of acres of wetlands have been modified through time to grow rice for human consumption. Rice is a nutritious food that can be grown by managing the timing and duration of water in naturally occurring wetlands and other low-lying areas. In North America, rice was the original cash crop for which imported enslaved persons were used, beginning in the 1670s. First instituted in South Carolina, rice culture expanded throughout the lower Atlantic coastal plain in subsequent decades and reached an apex just before the American Civil War between 1850 and 1860 [10]. During this peak period, 5,000,000 bushels of rice were produced in the United States, and 70% (3,500,000 bushels) were produced in South Carolina [10,11]. Rice cultivation collapsed after the Civil War due to three interacting factors: (1) without free labor (i.e., enslaved persons’ labor) the enterprise was no longer profitable, (2) a series of large storms damaged water control devices (e.g., dikes, levees, and trunks) and the planters did not have the capital nor the labor to recover from this series of devastating events, and (3) while rice farming in the Mississippi Delta was able to mechanize, planters along the Atlantic Coast (Georgia, Florida, North Carolina, and South Carolina) were unable to transition from human labor to machinery due in large part to the soft, alluvial soils [12,13].
Along the south Atlantic Coast, two economically successful methods for rice cultivation were used; both were derived from West African methods, and it is likely that enslaved persons were specifically sought who had this knowledge. Inland fields were the first to be developed. They were established in linear, gravity-fed, freshwater systems, which were likely ancient cypress–tupelo systems and surrounded by uplands. The inland rice cultivation system took advantage of the occurrence of distinct microenvironments that were a product of minor elevational changes along the landscape gradient from lowlands to uplands, allowing for rice to be cultivated in a variety of hydrologic conditions [14,15]. This system largely depended on precipitation to provide water, and to store water during periods of water scarcity and manage water flow through rice fields, dikes upstream and downstream of rice fields were constructed. These dikes today may be recognized on the ground and through remote sensing as identifiable indicators of historic and abandoned fields. The second method, tidal cultivation, came after the American Revolution and took advantage of the narrow coastal band where predictable tides and the associated freshwater wedge existed [16]. The flow of freshwater into and out of tidal rice fields was controlled by water management devices called trunks. Tidal rice fields can be recognized today by many geomorphological indicators.
While it is known that Antebellum planters first used inland, freshwater systems and eventually moved to tidal cultivation, little is known about the extensiveness of their operations or the particular wetland types and settings they may have selected. Travelers noted wetlands that occurred in the region, but such areas were considered unsafe and sources of disease and were avoided [17,18]. Ecological studies in relatively undisturbed contemporary wetlands in the region allow inference about what species and environments were likely encountered by builders of rice fields in the 17th–19th centuries; there are approximately 18 wetland types that are extant and were likely represented in the pre-settlement era [19].
Wetlands are valued for their high biological diversity and productivity, their ability to filter and transform nutrients and pollutants, and their capacity to buffer the impact of human activities on downstream aquatic systems [20]. Wetlands provide critical habitat for a variety of wildlife, including waterfowl, wading birds, reptiles and amphibians, and invertebrates [21]. Moreover, they contribute to enhanced water quality due to filtering and create recreational opportunities (e.g., hunting and fishing). While many historic rice fields have been lost with the passage of time, many remain and provide some level of wetland function [22]. Some that remain are maintained in their “rice field” state with traditional and modified technologies, and others have partially “naturalized” following their release over a century ago from being human controlled systems.
The current ecological state of Antebellum rice fields has been the focus of restoration, management, and conservation questions. Rice fields along the coast act as core habitat and maintain connectivity for a variety of avian species (e.g., waterfowl, shorebirds, and warblers) [22]. Many of the desired outcomes from management have been directed towards waterfowl [12]. Emphasis on waterfowl management is understandable, where in South Carolina alone, trip and equipment expenditures from waterfowl hunting in 2001 provided nearly $10 million and the total economic impact was more than $14 million [23]. In recent years management of historic rice fields has become more diverse in the set of objectives that now includes ecosystem services beyond supporting services such as waterfowl hunting and management to include such services as provisioning services for wildlife habitat (e.g., black rail, wood storks, roseate spoonbill, American alligator), regulating services for water quality and storm protection, and cultural services for tourism and recreation.
A conservation conundrum is how to prioritize places for action, when so many have been fundamentally altered by our own species [24]. The first step in any conservation planning project is to acquire spatial data representing the extent and conditions of conservation-relevant habitats. Historic rice fields in the Americas represent an illustration of the complexity of conservation planning. Should they be conserved for their current, wetland-related ecological values? Should they be conserved for their historical, cultural meaning? Should they be restored to a pre-agriculture, “wild” state? The first step in answering these questions is to know “where, how much, and what”, in other words, to know the extent of these features, where they are, and something of their characteristics.
Until now, the extent of Antebellum rice culture on the landscape in South Carolina has been estimated only from archival historical sources, and there has been no published empirical approach. The areal coverage of historic rice fields in South Carolina has been estimated from historical records to range from 29,950 to 60,703 ha (100,000 to 150,000 acres) [12,25], yet casual inspection of the landscape would suggest this coverage may be far greater. Further, there are no analyses of their current wetland classifications and land cover, which can serve as indications of potential function. Without a more complete understanding of their extent and location, and potential types, it is impossible to grasp their cultural, ecological, and historical value or to effectively manage them.
LiDAR provides a remotely sensed data source that can penetrate tree canopy cover and provide elevation data to model terrain structure, which is an advantage over other remotely sensed data sources that are unable to penetrate the forest canopy and provide ground-level data [26,27,28]. LiDAR was used to evaluate the legacy effects of ancient Mayan land use on canopy structure, where it was found that canopy height was more homogeneous on the terraced landscape formed by Mayans than the surrounding unterraced landscape [29]. In the landscape where the current work was performed, LiDAR was used to identify shell ring deposits by Native Americans prior to the arrival of Europeans, allowing for a more complete understanding of the distribution of these settlements [30].
Unlike work by Doar [25] and Gresham and Hook [12], our use of LiDAR allowed us to identify previously unknown historic rice fields (i.e., inland rice fields). Using a variety of remotely sensed data, which included aerial photography, historic aerial photography, near-infrared images, and LiDAR, we sought to map the extent of Antebellum rice fields in the region where rice culture was most dominant to serve as an initial understanding of the extent and types of wetlands modified in past centuries and their current functions. Due to the lack of inclusion of inland rice fields, now largely forested, in previous estimates of the areal extent of historic rice fields, we hypothesized that, in addition to the traditional methods used to identify these landscape features, our use of LiDAR imagery would result in an increase of 50% in the total area of historic rice fields. We provide these maps freely to researchers in the fields of history, geography, anthropology, historical ecology, and other disciplines concerned with piecing together the ecological and social consequences of the enslavement of humans for rice culture. Further, we estimate and discuss the current land cover contexts and wetland characteristics of historic rice fields to aid in management, research, and conservation planning.

2. Materials and Methods

We sought to remotely sense, digitize, and categorize historic rice fields in eight coastal counties of South Carolina, USA. South Carolina was chosen because it was the epicenter of rice culture in the southeastern United States during the Antebellum period and there has been work to identify historic rice fields there previously that can serve as a benchmark for comparison (see Doar et al., 1936 [10], Gresham and Hook 1982 [12]); LiDAR was readily available for the study area; and there has been and continues to be high interest in historic rice fields for social, cultural, and conservation reasons in South Carolina. We restricted our analysis to coastal counties because historical work showed this is where the vast majority of rice fields were located; however, there are documented rice fields outside of this area within South Carolina. Remotely sensed data sources included satellite imagery [31], aerial photographs [32], National Wetlands Inventory (NWI) [33], USGS topographic maps [34], and LiDAR [32] generated hillshaded bare earth digital elevation models (DEMs) and intensity models. LiDAR data were collected by the South Carolina Department of Natural Resources between 2007 and 2010, where there was a mean of two ground points per square meter with an average spacing of 0.7 m. Once obtained from the South Carolina Department of Natural Resources, the Clemson Center for Geospatial Technologies (CCGT) used high-throughput computing on Clemson University’s GIS cluster, which comprises 30 Windows computers with 740 cores for the distribution of GIS jobs for parallel processing. CCGT created hillshaded bare earth DEMs and intensity models from individual LiDAR files for eight coastal South Carolina counties. LiDAR files were processed at the county level using RapidLasso LASTools [35] in a three-step process. LiDAR point cloud data were split with neighboring files for buffered input, data were then distributed to CCGT’s GalaxyGIS cluster for parallel processing to calculate bare earth DEMs, and then DEMs were mosaiced back together and sent to the original workstation as a single file [36].
Using ArcGIS Online (AGOL), we developed an application where all remotely sensed data (i.e., aerial photographs, LiDAR DEMs and intensity models, NWI, satellite imagery, and USGS topographic maps), were accessible to use as a workspace for heads-up digitizing of rice fields. The application allowed us to identify potential rice fields using a combination of remotely sensed data sources. Rice fields were identified by the visual presence in remotely sensed data of canals, dikes, and quarter drains, which are the main features associated with historic rice fields. The authors (R. Coen and D. Hanks) performed all identification and digitization of the rice fields. The main features of the rice fields were particularly evident with hillshaded LiDAR (Figure 1C,D). The linear nature of these features associated with rice fields is in sharp contrast to the more typical dendritic branching associated with natural drainage patterns and was the primary factor used to identify landscape features as rice fields (Figure 1). In conjunction with hillshaded bare earth DEMs, LiDAR intensity models were also useful in identifying wetland areas below the forest canopy (i.e., rice fields) [37]. Because water shows high absorption for near-infrared wavelengths, LiDAR intensity is well suited to identify inundated or saturated ground surfaces [38].
Once a rice field was identified, using available remotely sensed data sources, we manually digitized the field using the AGOL application. Other landscape features with similar linearity are present on the landscape (e.g., mines, pine plantations); therefore, during heads-up digitizing, using the AGOL application, a mapper’s confidence in whether an area identified as a rice field was or was not a rice field was indicated by scoring the field as a 1 (low confidence), 2 (moderate confidence), or 3 (high confidence). The identification, digitization, and confidence quantification processes were performed at least twice by two different mappers (i.e., R. Coen and D. Hanks) across all eight coastal counties of South Carolina. Fields were also classified as either tidal (those influenced by coastal tides) or inland (those too far inland to be influenced by coastal tides). Tidal rice fields were further classified as functional or broken. The ability to manage water levels is maintained in functional tidal fields by intact dikes and water control features (i.e., trunks), whereas the dikes in broken tidal fields have been breached or broken, thereby eliminating the ability of managers to control water levels and movement of water into and out of the rice fields, resulting in these tidal fields resembling natural tidal marshes. Inland rice fields were not delineated as broken or functional primarily because it is difficult to distinguish if their dikes are broken or intact, even with LiDAR data.
Once the digitization process was complete, we developed a procedure for in-person visits to field validate areas identified as rice fields. To ensure a robust method of selecting a representative subset of rice fields to field validate, we developed a concept model (Figure 2) and protocol that is systematic and reproducible. This methodology allowed for a randomly selected subset of rice fields for in-person visits and field validation. Accessibility was a major concern for field validation due to private ownership of rice fields or fields being located great distances from roads or navigable waters. Therefore, to be included in our subset of rice fields for validation, we first filtered rice fields based on accessibility. Rice fields were considered accessible if they were within 200 m of a public road or navigable waters. This step ensured ease of access and reduced the amount of time required to validate a rice field, thereby allowing for more fields to be assessed, resulting in improved spatial distribution and increased coverage. Many of the accessible rice fields were either adjacent to or within the same rice field complex as those that were not easily accessed; therefore, we believe the available rice fields that were accessible were representative of the entire system. Next, we randomly selected a percentage of the rice fields that met the accessibility requirement within each confidence category (i.e., high, medium, low). Due to the variability in our confidence of identifying areas from our remotely sensed data as rice fields, we elected to field validate more of the areas identified as rice fields but with low confidence and fewer of the areas identified with high confidence as rice fields during the digitization and classification process. There were 3014 rice fields identified, of which 65.2% (1964) were accessible (i.e., within 200 m of a road or navigable waters). From the subset of accessible rice fields, we randomly selected 325 (10.8% of all identified fields) to field validate. Of the 325 randomly selected fields, 20.3% were classified as low confidence, 12.6% were classified as medium confidence, and 9.9% were classified as high confidence. To further ensure we accurately identified historic rice fields using remote sensing, we engaged local experts. The local experts we engaged with had both a geographic knowledge of the region and an understanding of the nature of historic rice fields. In fact, many of these individuals own and manage historic rice fields in the region. Local experts were asked to identify areas that were either errors of commission or errors of omission in our remotely sensed identification of historic rice fields [39]. Often the areas they focused on were their property, areas adjacent to their property, or areas which they had intimate knowledge of.
Field validation was accomplished by in-person visits to the randomly selected sites where identification and confirmation of dikes, canals, and other key identifying features were conducted. Fields were identified as either being rice fields or not (i.e., yes or no). Fields that were identified as rice fields (i.e., yes) were included in our final map and summary statistics of the rice fields, and those that were identified as not being rice fields were removed from the data set. Additionally, photographs were taken of at least one of the identifying features at each site. These images were added to the AGOL application for further confirmation (if in question) (Figure 3).
Using the National Land Cover Data 2016 (NLCD), the National Wetlands Inventory (NWI), and zonal statistics (ESRI ArcGIS Pro) we identified land cover types and wetland classes that were geographically coincident with rice fields. To gain further understanding of contemporary land cover and wetland classes geographically coincident with rice fields, fields were separated into tidal and inland rice fields, and zonal statistics were calculated again.

3. Results

3.1. Geographic and Areal Extent of Historic Rice Fields

Based on our analysis using remote sensing, there is an average of 52.3% more rice fields that were built using labor of enslaved persons in the heart of Antebellum-era rice culture than previously known. Historic rice fields that we detected spanned a distance of ~258 km (160 miles) along the South Carolina coast, were found as far inland as ~72 km (45 miles), and represented cumulatively 111,005 ha (274,301 acres) (Figure 4). We field validated 359 (10.7% of the total) randomly selected rice fields. Our error of commission was 6.1%. Therefore, using a variety of remotely sensed data sources, we accurately identified landscape features as rice fields 93.9% of the time. However, local experts identified 15,453 ha (38,185 acres) that our remote sensing efforts misclassified as rice fields but were in fact not historic rice fields, resulting in a total of 95,551 ha (236,112 acres) of historic rice fields in South Carolina, which is an increase of 157–236% over previous estimates of 29,950 to 60,703 ha (100,000 to 150,000 acres) [12,25]. The use of LiDAR allowed for differentiation and delineation of inland and tidal rice fields, for which previous work was unable to account [12,25]. Inland rice fields comprised 49.1% (47,032 ha) of the total area of historic rice fields in South Carolina, while tidal rice fields comprised 50.9% (48,624 ha). Of the 48,624 ha of tidal rice fields, 72.4% (35,184 ha) were identified as broken, while the remaining 27.6% (13,440 ha) were identified as functional.

3.2. Evaluation of Historic Rice Fields and Contemporary Land Cover and Wetland Type

The mapped historic rice fields were geographically coincident with the NLCD in the following manner: woody wetlands (56.3%, 53,903.8 ha) and emergent herbaceous wetlands (31.06%, 29,706.9 ha) were the two landcover types with the highest representation. High and medium developed lands had the least representation (0.05%, 49.5 ha; 0.10%, 90.1 ha, respectively). When considering inland and tidal rice fields separately, inland fields were dominated by woody wetlands (80.4%, 38,031.3 ha) and emergent herbaceous wetlands (6.81%, 3219.9 ha). Conversely, tidal fields were dominated by emergent herbaceous wetlands (56.17%, 27,310.2 ha) and woody wetlands (31.59%, 15,359.5 ha). Functional tidal fields were dominated by emergent herbaceous wetlands (58.36%, 7843.5 ha), open water (20.87%, 2805.3 ha), and woody wetlands (17.11%, 2300.0 ha), yet broken tidal fields were dominated by emergent herbaceous wetlands (55.33%, 19,466.7 ha) and woody wetlands (37.12%, 13,059.5 ha). Overall, the landcover types least represented in the mapped historic rice fields were high- and medium-intensity development, cultivated crops, and mixed forests. Landcover types least represented in inland fields were barren land, high-intensity development, cultivated crops, and medium-intensity development. In tidal fields, 12 of the 15 landcover types cumulatively represented only 2.04% areal coverage and included mixed forest, high-intensity development, cultivated crops, medium-intensity development, deciduous forests, pasture/hay, low-intensity development, shrub/scrub, barren land, open space development, grassland/herbaceous, and evergreen forests. These same 12 land cover classes represented 1.42% of areal coverage for the broken tidal fields and 3.65% for the functional tidal fields (Figure 5A, Table 1).
Based on the NWI, overall, the rice fields are currently geographically coincident mostly in palustrine wetlands (75.3%, 72,058 ha), followed by estuarine habitats (11.7%, 11,168 ha), with only upland habitats (9.9%, 9429 ha) representing >5%. Inland and tidal rice fields exhibit a similar distribution of NWI wetland systems where palustrine wetlands represent most rice fields (79.6%, 37,415 ha; 71.3%, 34,668 ha, respectively), followed by upland habitats in inland fields and estuarine wetlands in tidal fields (17.6%, 8282 ha; 21.5%, 10,438 ha) (Figure 5B, Table 2). The majority of both broken and functional tidal rice fields comprised palustrine wetlands (67.6%, 23,764 ha; 81.1%, 10,904 ha); however, the majority of the remaining broken tidal fields comprised estuarine wetlands (26.4%, 9286 ha), while the remaining functional tidal fields comprised somewhat evenly both estuarine and lacustrine wetlands (8.6%, 1152 ha and 6.5%, 877 ha).

4. Discussion

The human condition, past, present, and future, cannot be fully understood until it is embedded in its ecological condition [40]. Here, by delineating the full extent of historic rice fields in South Carolina, we provide the physical boundaries of these landscape legacies, which is the basis for beginning the process of embedding the human condition of the past and present within the ecological condition of the rice fields. We propose that this understanding may help inform the ecological and human conditions of the future. Historic rice fields from the Antebellum era are a landscape legacy of past land cover transformation that extends across the South Atlantic Coastal Plains from northern Florida to southern Virginia. Based on our estimates from South Carolina, where the practice was most extensive, we can assume that more than 95,000 hectares of wetlands and associated landscapes were transformed and impacted by slavery-driven rice culture, an increase in the area of known historic rice fields in South Carolina by as much as 68% over previous estimates [12,25]. Not only did the work of the enslaved and their planter owners influence the landscape, but the construction and maintenance of the fields also impacted the humans who were forced to do it. The hand labor involved with moving so much earth, as well as working in disease-ridden wetlands, in extreme temperatures, is thought to have caused the deaths of many enslaved children, men, and women. Whereas death rates for enslaved persons on cotton and tobacco plantations dropped to approximately 33% by the 1780s, double the number, approximately two-thirds, of enslaved persons still died on Lowcountry rice plantations up until the Civil War from chronic malaria, pneumonia, gastrointestinal and bowel diseases, overwork, and attacks by wild animals. Along the Savannah River, 90% of children enslaved on rice plantations died before 15 years of age, particularly from consecutive epidemics of Asiatic cholera [41]. After the wetlands were released from human control primarily due to the end of slavery in the United States, they took various ecological trajectories. Our mapping project cataloged current wetland characteristics of these anthropogenic features, showing that many, while retaining the signatures of their former uses, have reverted to some form of natural land cover.
Surprisingly, developed lands, while representing a very small percentage (0.05%) of the total areal coverage, were geographically coincident with historic rice fields. Despite the grading and earth moving associated with development, historic rice field signatures were present to some degree. Even after these land modifications, the ability of LiDAR to detect subtle elevational changes was visible to the individuals manually digitizing the rice fields. The ability of LiDAR to detect subtle changes is a valuable feature for similar projects where historic land uses may have transitioned to a contemporary use. Of the inland rice fields identified, nearly 6.8% were evergreen forests, which are primarily plantation pine stands, thus representing another land use transition to a contemporary use. Unsurprisingly, woody wetlands comprised more than 80% of the tidal rice fields; however, and somewhat surprisingly, woody wetlands represented 31.6% of the tidal rice fields in our study. Encroachment of woody vegetation into the tidal rice fields through successional creep along the margins was evident in this circumstance. Considering we do not know the ecological status of these areas as a pre-rice landscape, it is plausible that they were forested wetlands that are reverting to their former condition [42].
Rice cultivation in the pre-Antebellum south was a product of the slave economy that existed during this period and allowed for a landscape transformation from, most likely, forested wetlands to an agrarian landscape, providing evidence not only that the physical environment is often a product of the socio-political environment [43] but also that the physical environment is instrumental in structuring the socio-political environment. In the case presented here, the socio-political–environmental complex that existed between the 1670s and the 1860s resulted in a series of alternate stable states, which are still today going through various trajectories of ecological, political, and sociological change.
The coupling of human and natural systems (Figure 6A) has become extensive and has led to an understanding of the Earth within a new geological epoch termed the Anthropocene. During the pre-EuroAfro period (1540s to 1670) the landscape of the southeastern plains, while going through anthropogenic disturbance due to the development of cities such as Charleston, South Carolina, and Savannah, Georgia, was still in a somewhat “natural” condition. However, once the pre-EuroAfro natural landscape (Figure 6B) was anthropogenically modified to the EuroAfro rice culture state (Figure 6C), the interdependence of the system as a coupled human–natural system became even more evident and increasingly tightly coupled. Thereafter (Figure 6D,E, the contemporary and future states, respectively), the evolution of the historic rice fields has been due to both natural and human-management phenomena.
Societal and cultural norms of a given period resulted in the landscape being in various local and regional alternate stable states (Figure 6B–E). After emancipation, and without enslaved persons’ labor, the alternate stable state that was the rice enterprise was no longer profitable due to a state shift in the socio-ecological system that persisted for more than 150 years (Figure 6D,E). During these transitional periods, rice fields took varying trajectories that were largely dependent on the new socio-ecological system that developed, which could vary spatially depending on a variety of factors. Some fields were allowed to transition towards an unmanaged “natural” state, while others were managed in large part for waterfowl. Even today, some fields continue to be managed primarily for waterfowl and recreation but also for non-game species such as wood storks and songbirds, while yet others continue along the path towards some unmanaged “natural” ecological state. While it is theoretically possible the ecosystem could return to a state similar to that of the pre-EuroAfro condition at various periods after the anthropogenic EuroAfro rice culture state shift (e.g., transitions from Figure 6C,D to Figure 6B), it is unlikely, if not impossible, and potentially even undesirable for the system to return to the exact pre-EuroAfro ecosystem due to additional changes across the socio-political–ecological landscape.
All but 9.9% of the identified rice fields (inland and tidal) were geographically coincident with a wetland type as described by the NWI. Historic rice fields represent more than 6% of the remaining wetlands in South Carolina. As wetland ecosystems, historic rice fields are valuable resources for their many and varied conservation and ecological functions; however, wetlands have been viewed as a hindrance to productive land use. Due to this view of wetlands, many have been modified to provide non-natural land uses (e.g., many wetlands have been ditched and drained for agricultural production). In fact, between the 1780s and the 1980s, wetland loss in the lower 48 states of the United States exceeded 50%. South Carolina, the extent of this study, lost an estimated 305,537 ha (755,000 acres) or 27% of its wetlands during this 200-year period [19]. Wetlands continue to be converted to other uses; for example, during a nine-year span (1980–1989), 8274 ha (20,440 acres) of wetlands was lost in South Carolina [44]. Once converted to other land uses, the historical and cultural values of historic rice fields, as well as the ecological value, will be lost without a clear path back to their former wetland condition.
Historic rice fields along the Atlantic coastal plain are land use legacies that no longer function as working rice fields but instead provide a variety of other functions in this regional landscape. Threats to their continued function are many and will likely interact in a synergistic manner that is difficult to predict. Threats include land use change [45,46], climate change (e.g., increased tropical storms and hurricanes [47]), and sea level rise [48]. Of these threats, some may be chronic (e.g., land use change, climate change, sea level rise), while others may be episodic (e.g., tropical storms and hurricanes). Leonard et al. [48] found that in coastal areas of the southeastern U.S., there is likely to be decreased habitat connectivity for wildlife due to the combination of sea level rise and urban sprawl. Moreover, recent tropical storms and hurricanes (e.g., hurricanes Matthew (2016) and Florence (2018)) have damaged the structural integrity of rice field dikes to the point that they must be rebuilt if the landscape is to continue to be managed as a historic rice field. Reconstitution of these breached structures results in thousands of dollars of costs to private landowners, who are the primary owners of historic rice fields. As the breaches continue in the future, potentially more regularly, there may be a point where landowners can no longer afford the costs of reconstruction of the historic structures, thereby resulting in loss of these important features. As episodic and chronic stressors continue to increase in intensity and/or frequency, the structure and function of historic rice fields will be threatened and increasingly lost.
With increasing pressure from land use change across much of the Earth, further understanding of how conservation features may be embedded in the matrix of land use is needed. Historical rice fields then represent an intensive example of what conservation biologists routinely confront worldwide, which is how to restore, protect, and maintain biodiversity in a changing world, given vast and increasing human influence. Some landscapes, as a result of land use legacies, have valuable biotic assemblages, while also having value as cultural and historical sites. These values are in constant flux as the dynamics of ecology, politics, and culture evolve. Historic rice fields represent a prime case in point. This may present a conundrum to traditional conservation motives, where it is seen as desirable and attempts are made to return a system to its pre-anthropogenic state. Furthermore, to maintain the stable state that exists due in large part to the land use legacy will require the continuation or reintroduction of management activities that originally helped create that legacy [2]. To further complicate attempts to return the landscape to a pre-rice-cultivation ecosystem assumes an understanding of the structure and function of the system prior to the early 1670s as a sort of reference system, a knowledge which does not currently exist. Given there was an understanding of the pre-rice ecosystem structure which could be restored, there is no guarantee that the historic ecosystem function would also be restored [49].
This study expanded the known extent of Antebellum rice fields created by enslaved persons by 1.57–3.19 times (36.4–68.2% increase). This research focused on South Carolina, which was the epicenter of historic rice culture prior to the Civil War, and provides an index upon which to consider the extensiveness of this type of wetland transformation, knowledge that it happened at the landscape scale, and the types of wetland that may have been favored and their current characteristics. Yet still, there is much to be learned about the values these land use legacies provide, and the current study provides the underpinning to consider future work such as defining the stable states that existed before rice culture, understanding better the historical conditions under which enslaved persons worked during their cultivated states, and understanding what functions and values the legacy wetlands may have today. In addition to waterfowl hunting, which has been and continues to be the driving force behind the continued management of the rice fields, there are many unstudied values and services that these land use legacies provide (e.g., tourism-related activities such as bird and wildlife watching). The maps and data we have produced can form the foundation for a series of hypotheses on which many future investigations can be developed, and they can be input into conservation planning and design projects that wish to incorporate both cultural and natural values.

Author Contributions

Conceptualization, R.D.H., R.F.B., T.H.F., M.L.G. and E.P.W.; methodology, R.D.H., R.F.B., T.H.F., M.L.G. and R.H.C.; formal analysis, R.D.H., M.L.G., R.H.C. and T.H.F.; writing, R.D.H.; writing—review and editing, R.D.H., R.F.B., T.H.F., E.P.W., A.A., D.D.R. and E.L.F.-B.; visualization, R.D.H. All authors have read and agreed to the published version of the manuscript.

Funding

This research received no external funding.

Data Availability Statement

Mapped historic rice fields of South Carolina can be found on ArcGIS Online online: https://services1.arcgis.com/x5wCko8UnSi4h0CB/arcgis/rest/services/Rice_fields/FeatureServer (accessed on 25 July 2021).

Acknowledgments

We would like to thank the following entities: Nemours Wildlife Foundation, Folk Land Management, Margaret H. Lloyd Endowment, Carnegie Mellon University, Duke University, University of South Carolina, Clemson University, and the Clemson University Department of Forestry and Environmental Sciences. The Clemson Center for Geospatial Technologies was particularly helpful with the processing of LiDAR files, and we owe them a great deal of gratitude.

Conflicts of Interest

The authors declare no conflict of interest.

Dedication

This paper is dedicated to Michael L. Gouin (1970–2021), U.S. Navy veteran, Clemson graduate, and the first intern for the rice field mapping project. His enthusiasm and hard work in the early phases were a primary factor in our success in mapping rice fields of South Carolina. He will be remembered as a conservationist, aficionado of South Carolina history, and a gentleman.

References

  1. Waters, C.N.; Zalasiewicz, J.; Summerhayes, C.; Barnosky, A.D.; Poirier, C.; Gałuszka, A.; Cearreta, A.; Edgeworth, M.; Ellis, E.C.; Ellis, M.; et al. The Anthropocene is functionally and stratigraphically distinct from the Holocene. Science 2016, 351, aad2622. [Google Scholar] [CrossRef] [PubMed]
  2. Foster, D.; Swanson, F.; Aber, J.; Burke, I.; Brokaw, N.; Tilman, D.; Knapp, A. The Importance of Land-Use Legacies to Ecology and Conservation. Bioscience 2003, 53, 77–88. [Google Scholar] [CrossRef] [Green Version]
  3. Richter, D.D.; Markewitz, D.; Heine, P.R.; Jin, V.; Raikes, J.; Tian, K.; Wells, C.G. Legacies of agriculture and forest regrowth in the nitrogen of old-Field soils. For. Ecol. Manag. 2000, 138, 233–248. [Google Scholar] [CrossRef]
  4. Gunderson, L.H. Ecological resilience-in theory and application. Annu. Rev. Ecol. Syst. 2000, 31, 425–439. [Google Scholar] [CrossRef] [Green Version]
  5. Richter, D.D.; Markewitz, D.; Trumbore, S.E.; Wells, C.G. Rapid accumulation and turnover of soil carbon in a re-establishing forest. Nature 1999, 400, 56–58. [Google Scholar] [CrossRef] [Green Version]
  6. Scott, M.C. Winners and losers among stream fishes in relation to land use legacies and urban development in the southeastern US. Biol. Conserv. 2005, 127, 301–309. [Google Scholar] [CrossRef]
  7. Baldwin, R.F.; Surasinghe, T. Ghost of land use past in the context of current land cover: Evidence from salamander communities in streams of Blue Ridge and Piedmont ecoregions. Artic. Can. J. Zool. 2014, 92, 527–536. [Google Scholar]
  8. De Steven, D.; Gramling, J.M. Diverse Characteristics of Wetlands Restored under the Wetlands Reserve Program in the Southeastern United States. Wetlands 2012, 32, 593–604. [Google Scholar] [CrossRef]
  9. Pitt, A.L.; Baldwin, R.F.; Lipscomb, J.D.; Brown, B.L.; Hawley, J.E.; Allard-Keese, C.M.; Leonard, P.B. The missing wetlands: Using local ecological knowledge to find cryptic ecosystems. Biodivers. Conserv. 2012, 21, 51–63. [Google Scholar] [CrossRef]
  10. Doar, D.; Salley, A.S.; Ravenel, T.D. Rice and rice Planting in the South Carolina low Country; The Charleston Museum: Charleston, SC, USA, 1936. [Google Scholar]
  11. Coclanis, P.A. The Shadow of a Dream: Economic Life and Death in the South Carolina Low Country, 1670–1920; Oxford University Press: Oxford, UK, 1989; ISBN 0198021356. [Google Scholar]
  12. Gresham, C.A.; Hook, D.D. Rice fields of South Carolina: A resource inventory and management policy evaluation. Coast. Manag. 1982, 9, 183–203. [Google Scholar] [CrossRef]
  13. Tuten, J.H. Lowcountry Time and Tide: The Fall of the South Carolina Rice Kingdom; University of South Carolina Press: Columbia, SC, USA, 2012; ISBN 1611172160. [Google Scholar]
  14. Carney, J. Landscapes of Technology Transfer: Rice Cultivation and African Continuities. Technol. Cult. 1996, 37, 5–35. [Google Scholar] [CrossRef]
  15. Carney, J.; Porcher, R. Geographies of the past. Southeast. Geogr. 1993, 33, 127–147. [Google Scholar] [CrossRef]
  16. Porcher, R.D.; Judd, W.R. The market preparation of Carolina Rice: An Illustrated History of Innovations in the Lowcountry Rice Kingdom; University of South Carolina Press: Columbia, SC, USA, 2014; ISBN 1611173515. [Google Scholar]
  17. Nairne, T. Nairne’s Muskhogean Journals: The 1708 Expedition to the Mississippi River; Univ. Press of Mississippi: Jackson, MS, USA, 1988; ISBN 1604736445. [Google Scholar]
  18. Dallmeyer, D.G. Bartram’s Living Legacy: The Travels and the Nature of the South; Mercer University Press: Macon, GA, USA, 2010. [Google Scholar]
  19. Dahl, T.E. Wetlands Losses in the United States, 1780’s to 1980’s: Report to the Congress 1990; U.S. Department of the Interior, Fish and Wildlife Service: Washington, DC, USA, 1990. [Google Scholar]
  20. Hook, D.D. Wetlands: History, current status, and future. Environ. Toxicol. Chem. 1993, 12, 2157–2166. [Google Scholar] [CrossRef]
  21. Mitsch, W.J.; Gossilink, J.G. The value of wetlands: Importance of scale and landscape setting. Ecol. Econ. 2000, 35, 25–33. [Google Scholar] [CrossRef]
  22. Williams, R.K.; Perry, R.D.; Prevost, M.B.; Adair, S.E.; McKnight, S.K. Management of South Atlantic Coastal Wetlands for Waterfowl and Other Wildlife; Ducks Unlimited: Memphis, TN, USA, 2002. [Google Scholar]
  23. U.S. Fish and Wildlife Service. Economic Impact of Waterfowl Hunting in the United States; U.S. Fish and Wildlife Service: Washington, DC, USA, 2008. [Google Scholar]
  24. Margules, C.R.; Pressey, R.L. Systematic Conservation Planning. Nature 2000, 405, 243–253. [Google Scholar] [CrossRef] [PubMed]
  25. Doar, D. Rice and Rice Planting in the South Carolina Low Country. 1936; Charlest. Museum: Charleston, SC, USA, 1970. [Google Scholar]
  26. Sittler, B. Revealing historical landscapes by using airborne laser scanning. Int. Arch. Photogramm. Remote Sens. Spat. Inf. Sci. 2004, 26, 258–261. [Google Scholar]
  27. James, L.A.; Watson, D.G.; Hansen, W.F. Using LiDAR data to map gullies and headwater streams under forest canopy: South Carolina, USA. Catena 2007, 71, 132–144. [Google Scholar] [CrossRef]
  28. Lang, M.W.; McCarty, G.W. Lidar intensity for improved detection of inundation below the forest canopy. Wetlands 2009, 29, 1166–1178. [Google Scholar] [CrossRef]
  29. Hightower, J.N.; Butterfield, A.C.; Weishampel, J.F. Quantifying ancient maya land use legacy effects on contemporary rainforest canopy structure. Remote Sens. 2014, 6, 10716–10732. [Google Scholar] [CrossRef]
  30. Davis, D.S.; Dinapoli, R.J.; Sanger, M.C.; Lipo, C.P. The Integration of Lidar and Legacy Datasets Provides Improved Explanations for the Spatial Patterning of Shell Rings in the American Southeast. Adv. Archaeol. Pract. 2020, 8, 361–375. [Google Scholar] [CrossRef]
  31. Esri ArcGIS World Imagery 2015. Available online: https://www.arcgis.com/home/group.html?id=0f3189e1d1414edfad860b697b7d8311#overview (accessed on 25 July 2021).
  32. Resources, S.C.D. of N. GIS data Clearinghouse. Available online: www.dnr.sc.gov/gis.html (accessed on 20 July 2008).
  33. Wilen, B.O.; Bates, M.K. The US fish and wildlife service’s national wetlands inventory project. In Classification and Inventory of the World’s Wetlands; Springer: Berlin/Heidelberg, Germany, 1995; pp. 153–169. [Google Scholar]
  34. Esri, H.; DeLorme, I.; Increment, P.; Gebco, U.; Fao, N.P.S. World Topographic Map. 2013. Available online: https://www.arcgis.com/home/item.html?id=7dc6cea0b1764a1f9af2e679f642f0f5 (accessed on 21 July 2021).
  35. LAStools. Available online: http://rapidlasso.com/LAStools (accessed on 25 July 2021).
  36. TigersGIS Elevation Models from LiDAR. Available online: https://www.clemsongis.org/elevation-models-lidar (accessed on 25 July 2021).
  37. Lang, M.; Mccarty, G.; Oesterling, R. Topographic Metrics for Improved Mapping of Forested Wetlands. Wetlands 2013, 33, 141–155. [Google Scholar] [CrossRef]
  38. Lang, M.W.; McCarty, G. United States, Natural Resources Conservation Service, Conservation Effects Assessment Project. Light Detection and Ranging (LiDAR) for Improved Mapping of Wetland Resources and Assessment of Wetland Conservation Practices. Available online: https://naldc.nal.usda.gov/catalog/60811 (accessed on 25 July 2021).
  39. ESRI. ESRI ArcGIS Desktop: Release 10 2011; ESRI: Redlands, CA, USA, 2011. [Google Scholar]
  40. Cronon, W. Changes in the Land: Indians, Colonists, and the Ecology of New England; Hill and Wang: New York, NY, USA, 2011; ISBN 142992828X. [Google Scholar]
  41. Dusinberre, W. Them Dark Days: Slavery in the American Rice Swamps; Oxford University Press on Demand: Oxford, UK, 1996; ISBN 0195090217. [Google Scholar]
  42. Kovacik, C.F.; Winberry, J.J. South Carolina: The Making of a Landscape; University of South Carolina Press: Columbia, SC, USA, 1987; ISBN 0872496848. [Google Scholar]
  43. Mitchell, D. Cultural landscapes: Just landscapes or landscapes of justice? Prog. Hum. Geogr. 2003, 27, 787–796. [Google Scholar] [CrossRef]
  44. Dahl, T.E. South Carolina’s Wetlands: Status and Trends 1982–1989; DAHL: Washington, DC, USA, 1999. [Google Scholar]
  45. Terando, A.J.; Costanza, J.; Belyea, C.; Dunn, R.R.; McKerrow, A.; Collazo, J.A. The Southern Megalopolis: Using the Past to Predict the Future of Urban Sprawl in the Southeast U.S. PLoS ONE 2014, 9, e102261. [Google Scholar] [CrossRef] [Green Version]
  46. Brown, D.G.; Johnson, K.M.; Loveland, T.R.; Theobald, D.M. Rural land-use trends in the conterminous United States, 1950–2000. Ecol. Appl. 2005, 15, 1851–1863. [Google Scholar] [CrossRef] [Green Version]
  47. Woodruff, J.D.; Irish, J.L.; Camargo, S.J. Coastal flooding by tropical cyclones and sea-level rise. Nature 2013, 504, 44–52. [Google Scholar] [CrossRef] [Green Version]
  48. Leonard, P.B.; Sutherland, R.W.; Baldwin, R.F.; Fedak, D.A.; Carnes, R.G.; Montgomery, A.P. Landscape connectivity losses due to sea level rise and land use change. Anim. Conserv. 2017, 20, 80–90. [Google Scholar] [CrossRef]
  49. Stephenson, N.L. Reference Conditions for Giant Sequoia Forest Restoration: Structure, Process, and Precision. Ecol. Appl. 2011, 9, 1253–1265. [Google Scholar] [CrossRef]
Figure 1. Comparison of aerial (A,B) and LiDAR (C,D) imagery in both tidal (A,C) and inland (B,D) rice fields to exemplify how LiDAR digital elevation model hillshades were particularly useful in identifying dikes and canals in inland fields and the margins of tidal rice fields where they were adjacent to forested lands. Shaded polygons show digitized tidal (blue) and inland (yellow) rice fields.
Figure 1. Comparison of aerial (A,B) and LiDAR (C,D) imagery in both tidal (A,C) and inland (B,D) rice fields to exemplify how LiDAR digital elevation model hillshades were particularly useful in identifying dikes and canals in inland fields and the margins of tidal rice fields where they were adjacent to forested lands. Shaded polygons show digitized tidal (blue) and inland (yellow) rice fields.
Land 10 00831 g001
Figure 2. A systematic and reproducible conceptual model was developed to ensure a robust subset of rice fields were selected for field validation.
Figure 2. A systematic and reproducible conceptual model was developed to ensure a robust subset of rice fields were selected for field validation.
Land 10 00831 g002
Figure 3. A subset of rice fields was selected to be field validated. (A) The AGOL application allowed for georeferenced field validation. A channel of an inland rice field is shown with the AGOL application in panel (A). Panel (B) demonstrates the dense overstory in many inland rice fields, where LiDAR-derived bare ground DEMs proved to be an invaluable data source. Panel (C) shows a dike of a tidal rice field. The wooden structure on the left side of the picture is a rice field trunk used as a water control feature. Panel (D) shows a quarter drain in a tidal rice field that is fully inundated. Photo credits: A, B, and D to D. Hanks. C to T. Folk.
Figure 3. A subset of rice fields was selected to be field validated. (A) The AGOL application allowed for georeferenced field validation. A channel of an inland rice field is shown with the AGOL application in panel (A). Panel (B) demonstrates the dense overstory in many inland rice fields, where LiDAR-derived bare ground DEMs proved to be an invaluable data source. Panel (C) shows a dike of a tidal rice field. The wooden structure on the left side of the picture is a rice field trunk used as a water control feature. Panel (D) shows a quarter drain in a tidal rice field that is fully inundated. Photo credits: A, B, and D to D. Hanks. C to T. Folk.
Land 10 00831 g003
Figure 4. Map of the South Carolina “Rice Kingdom” showing the location and geographic extent of historic rice fields in South Carolina. Green polygons represent broken tidal fields and purple polygons represent functional tidal fields, whereas orange polygons represent inland fields.
Figure 4. Map of the South Carolina “Rice Kingdom” showing the location and geographic extent of historic rice fields in South Carolina. Green polygons represent broken tidal fields and purple polygons represent functional tidal fields, whereas orange polygons represent inland fields.
Land 10 00831 g004
Figure 5. Area in hectares is given for where historic rice fields are geographically coincident with the National Land Cover Dataset (NLCD) and the National Wetlands Inventory (NWI). NLCD land cover types (A), NWI System type (B), NWI Subsystem/Class type (C), and NWI Upland Land Cover/Land Use (D). (B) National Wetland Inventory System type: E—Estuarine, L—Lacustrine, P—Palustrine, R—Riverine, and U—Upland. (C) National Wetlands Inventory Subsystem/Class type: E1—Estuarine Subtidal, E2—Estuarine Intertidal, L1—Lacustrine Limnetic, L2—Lacustrine Littoral, PAB—Palustrine Aquatic Bed, PEM—Palustrine Emergent, PFO—Palustrine Forested, PSS—Palustrine Scrub–Shrub, PUB—Palustrine Unconsolidated Bottom, R1—Riverine Tidal, R2—Riverine Lower Perennial, and U—Uplands.
Figure 5. Area in hectares is given for where historic rice fields are geographically coincident with the National Land Cover Dataset (NLCD) and the National Wetlands Inventory (NWI). NLCD land cover types (A), NWI System type (B), NWI Subsystem/Class type (C), and NWI Upland Land Cover/Land Use (D). (B) National Wetland Inventory System type: E—Estuarine, L—Lacustrine, P—Palustrine, R—Riverine, and U—Upland. (C) National Wetlands Inventory Subsystem/Class type: E1—Estuarine Subtidal, E2—Estuarine Intertidal, L1—Lacustrine Limnetic, L2—Lacustrine Littoral, PAB—Palustrine Aquatic Bed, PEM—Palustrine Emergent, PFO—Palustrine Forested, PSS—Palustrine Scrub–Shrub, PUB—Palustrine Unconsolidated Bottom, R1—Riverine Tidal, R2—Riverine Lower Perennial, and U—Uplands.
Land 10 00831 g005
Figure 6. (A) Coupling of natural–human systems; (BE) controls within and between coupled human and natural systems provide feedback mechanisms that maintain a stable state, but transitions to alternate stable states can occur given system disruptions (e.g., energy inputs). Coupled human–natural systems interact with one another and are controlled by parameters that influence their resilience and stability.
Figure 6. (A) Coupling of natural–human systems; (BE) controls within and between coupled human and natural systems provide feedback mechanisms that maintain a stable state, but transitions to alternate stable states can occur given system disruptions (e.g., energy inputs). Coupled human–natural systems interact with one another and are controlled by parameters that influence their resilience and stability.
Land 10 00831 g006
Table 1. Distribution of historic rice fields within the various National Land Cover Data (NLCD) categories for the total area, as well as for both inland and tidal fields.
Table 1. Distribution of historic rice fields within the various National Land Cover Data (NLCD) categories for the total area, as well as for both inland and tidal fields.
Land CoverTotalInlandTidalTidal BrokenTidal Functional
Area (ha)% of TotalArea (ha)% of TotalArea (ha)% of TotalArea (ha)% of TotalArea (ha)% of Total
Open Water6013.56.291109.52.354962.110.212156.86.132805.320.87
Developed, Open Space739.90.77558.41.18187.60.3977.20.22110.30.82
Developed, Low Intensity179.50.19134.60.2843.60.0925.30.0718.30.14
Developed, Medium Intensity90.90.1074.30.1614.80.0311.60.033.20.02
Developed, High Intensity49.50.0543.30.095.60.015.30.010.30.00
Barren Land (Rock/Sand/Clay)111.70.1224.80.0590.60.1973.70.2116.80.13
Deciduous Forest433.10.45399.10.8420.60.047.10.0213.50.10
Evergreen Forest3629.63.793204.36.77337.70.69191.10.54146.61.09
Mixed Forest91.10.1087.20.180.80.000.30.000.50.00
Shrub/Scrub175.70.18121.80.2652.40.115.00.0147.40.35
Grassland/Herbaceous361.50.38153.20.32209.70.4390.80.26118.90.88
Pasture/Hay108.50.1186.80.1821.70.047.20.0214.50.11
Cultivated Crops60.90.0653.90.117.20.016.40.020.80.01
Woody Wetlands53,903.856.3538,031.380.4015,359.531.5913,059.537.122300.017.11
Emergent Herbaceous Wetlands29,706.931.063219.96.8127,310.256.1719,466.755.337843.558.36
Total95,655.9 47,302.3 48,623.9 35,184.0 13,439.9
Table 2. Distribution of historic rice fields within the various system categories of the National Wetlands Inventory.
Table 2. Distribution of historic rice fields within the various system categories of the National Wetlands Inventory.
SYSTEMTotalInlandTidal TotalTidal BrokenTidal Functional
Area (ha)% TotalArea (ha)% TotalArea (ha)% TotalArea (ha)% TotalArea (ha)% Total
Estuarine11,168.411.68730.51.5510,438.021.479285.626.391152.48.57
Lacustrine2702.42.83571.11.212131.24.381254.43.57876.86.52
Palustrine72,082.675.3737,414.679.5734,668.071.3023,764.067.5510,904.081.14
Riverine259.00.2723.30.05235.70.48225.70.6410.00.07
Upland9429.29.868282.317.611146.92.36651.11.85495.83.69
Publisher’s Note: MDPI stays neutral with regard to jurisdictional claims in published maps and institutional affiliations.

Share and Cite

MDPI and ACS Style

Hanks, R.D.; Baldwin, R.F.; Folk, T.H.; Wiggers, E.P.; Coen, R.H.; Gouin, M.L.; Agha, A.; Richter, D.D.; Fields-Black, E.L. Mapping Antebellum Rice Fields as a Basis for Understanding Human and Ecological Consequences of the Era of Slavery. Land 2021, 10, 831. https://doi.org/10.3390/land10080831

AMA Style

Hanks RD, Baldwin RF, Folk TH, Wiggers EP, Coen RH, Gouin ML, Agha A, Richter DD, Fields-Black EL. Mapping Antebellum Rice Fields as a Basis for Understanding Human and Ecological Consequences of the Era of Slavery. Land. 2021; 10(8):831. https://doi.org/10.3390/land10080831

Chicago/Turabian Style

Hanks, R. Daniel, Robert F. Baldwin, Travis H. Folk, Ernie P. Wiggers, Richard H. Coen, Michael L. Gouin, Andrew Agha, Daniel D. Richter, and Edda L. Fields-Black. 2021. "Mapping Antebellum Rice Fields as a Basis for Understanding Human and Ecological Consequences of the Era of Slavery" Land 10, no. 8: 831. https://doi.org/10.3390/land10080831

APA Style

Hanks, R. D., Baldwin, R. F., Folk, T. H., Wiggers, E. P., Coen, R. H., Gouin, M. L., Agha, A., Richter, D. D., & Fields-Black, E. L. (2021). Mapping Antebellum Rice Fields as a Basis for Understanding Human and Ecological Consequences of the Era of Slavery. Land, 10(8), 831. https://doi.org/10.3390/land10080831

Note that from the first issue of 2016, this journal uses article numbers instead of page numbers. See further details here.

Article Metrics

Back to TopTop