Archaeological remains of agrarian-based, low-density urbananism1,2,3 have been reported to exist beneath the tropical forests of Southeast Asia, Sri Lanka and Central America4,5,6. However, beyond some large interconnected settlements in southern Amazonia7,8,9, there has been no such evidence for pre-Hispanic Amazonia. Here we present lidar data of sites belonging to the Casarabe culture (around ad 500 to ad 1400)10,11,12,13 in the Llanos de Mojos savannah–forest mosaic, southwest Amazonia, revealing the presence of two remarkably large sites (147 ha and 315 ha) in a dense four-tiered settlement system. The Casarabe culture area, as far as known today, spans approximately 4,500 km2, with one of the large settlement sites controlling an area of approximately 500 km2. The civic-ceremonial architecture of these large settlement sites includes stepped platforms, on top of which lie U-shaped structures, rectangular platform mounds and conical pyramids (which are up to 22 m tall). The large settlement sites are surrounded by ranked concentric polygonal banks and represent central nodes that are connected to lower-ranked sites by straight, raised causeways that stretch over several kilometres. Massive water-management infrastructure, composed of canals and reservoirs, complete the settlement system in an anthropogenically modified landscape. Our results indicate that the Casarabe-culture settlement pattern represents a type of tropical low-density urbanism that has not previously been described in Amazonia.
During the Late Holocene epoch, pre-Hispanic agriculturalists in the Llanos de Mojos, Bolivia, transformed the most-extensive, seasonally flooded, Amazonian savannahs (120,000 km2—roughly the size of England) into productive agricultural and aquacultural landscapes with an apparent diversity in sociopolitical organization, water-control systems and economic bases14,15,16,17. The southeast sector of the Llanos de Mojos (our study region) benefits from soils that have advantageous agricultural properties because of the deposition of a mid-Holocene sedimentary lobe that creates a slightly more elevated topography than the surrounding Llanos de Mojos, which in turn, provides base-rich, Andean-derived, well-drained soils18. The Casarabe culture developed here between around ad 500 and ad 1400, spreading over an area of 4,500 km2 (see ‘Chronology’ in the Supplementary Information, Supplementary Figs. 3–5 and Supplementary Tables 2–4). Previous remote-sensing and field-reconnaissance analyses have revealed the presence of 189 large monumental sites (locally known as ‘lomas’), 273 smaller sites and 957 km of canals and causeways10,19 (Supplementary Table 1). Excavations and bioarchaeology indicate that monumental sites were not unoccupied ceremonial centres but inhabited throughout the year by agriculturalists who cultivated a diversity of crops, with maize (Zea mays) as the primary staple10,11,12,20,21, and who met their protein needs by hunting22 and fishing23.
Despite these important advances in the archaeology of the Casarabe culture, until now, we knew the extent and details of mounded architecture only from less than a handful of isolated sites (Extended Data Figs. 5a, 7) because of the logistical difficulties of mapping sites in tropical forested settings. As a result, our understanding of the civic-ceremonial architecture of the major sites and the regional organization of the Casarabe-culture settlements has remained poorly understood. To remedy this situation, we conducted airborne laser mapping for six areas (10–85 km2) that have known concentrations of major settlements, totalling 204 km2 (Fig. 1).
Lidar (light detection and ranging) documented in detail the two large settlement sites and 24 smaller sites, of which only 15 were previously known to exist. The new data allowed us to define a four-tiered hierarchy classification of sites (Supplementary Table 5) on the basis of (1) the dimensions of human-made base platforms; (2) the elaboration of the civic-ceremonial architecture on top of them; (3) the presence, number and total area enclosed by the outermost polygonal enclosures (Figs. 2, 3 and Extended Data Figs. 1–4); (4) the number of constructed, straight causeways leading to the site (Fig. 3); and (5) the scale of investment in water-management infrastructure, including systems of canals and water reservoirs (see Supplementary Information for a detailed description of the architectural elements and a description of representative sites).
Large settlement sites
Settlements that, at more than 100 ha in size, exceed most other settlements of the same culture many times over, are a very early and worldwide phenomenon2,24,25. A formally agreed term for these sites is still missing26, so in this Article we use the descriptive term ‘large settlement site’ when referring to the two most important sites in the region: Cotoca (147 ha; Figs. 2 and Extended Data Fig. 1) and Landívar (315 ha; Fig. 3 and Extended Data Fig. 2). These two large settlement sites were already known, but their massive size and architectural elaboration became apparent only through the lidar survey.
Both large settlement sites are surrounded by three concentric defensive structures consisting of a moat and rampart (Extended Data Fig. 1), some of which are constituted by double walls (Extended Data Fig. 9a). At the Cotoca site, the inner defensive structures are only preserved in some sections (Extended Data Fig. 1), which may suggest that when the site grew, ramparts were adapted accordingly.
The scale and elaboration of civic-ceremonial architecture are key aspects of the large settlement sites. Massive earthen platform buildings—some of which are U-shaped (Extended Data Fig. 6)—and conical pyramids rise more than 20 m above the surrounding savannah on top of artificial terraces of up to 6 m in height (Fig. 2, Extended Data Figs. 1–3, 4b, 5). The orientation of the buildings that constitute the civic-ceremonial centres of the two large settlement sites is very uniform towards the north-northwest. This probably reflects a cosmological world view, which is also present in the orientation of extended burials of the Casarabe culture (see ‘Funerary patterns’ in Supplementary Information and Supplementary Fig. 1). The core area of Cotoca (22 ha; Figs. 2, 3b and Extended Data Fig. 1)—as defined by the artificial terrace—is more than three times the size of the secondary centres (Supplementary Table 5). Earth to construct the artificial terraces and platform buildings was acquired, at least partially, from areas adjacent to the settlement’s centre. At Cotoca, for example, earth has been removed from a 50- to 80-m wide strip surrounding the central terrace. Today, these lower areas fill with water during the rainy season and are swampy during much of the dry season.
Cotoca and Landívar were the primary centres of a regional settlement network connected by still-visible, straight causeways that radiate from these sites into the landscape for several kilometres (Fig. 3). The presence of platforms (about 20 m by 25 m in size and up to 2 m high) located at strategic points of some of the causeways (Extended Data Fig. 9b, c) and in gaps in the intersection of causeways and polygonal enclosures suggest that access to these large settlement sites may have been restricted and controlled. Labour investment in the construction of the core area of the Landívar site (artificial terraces and platform buildings of the civic-ceremonial centre) is approximately 276,000 m3. The investment in site construction is even more impressive for Cotoca, for which the core area totals 570,690 m3. This latter figure is ten times the amount of earth moved for the construction of the Akapana (53,546 m3)27, the largest structure in Tiwanaku, capital of the eponymous expansive state that developed over several centuries in the Bolivian highlands, simultaneous with the Casarabe culture.
Low-density urbanism of the Casarabe culture
The large settlement sites Cotoca and Landívar were primary centres in the settlement network of the Casarabe culture. Secondary centres (El Cerrito and Salvatierra (sites 106, 186, 193 and 195)) (Supplementary Table 1 and Extended Data Figs. 3, 4, 5, 8) are characterized by base platforms ranging from 2 to 6 ha and one still-visible polygonal enclosure that circumscribes areas between 21 and 41 ha. Civic-ceremonial architecture on top of the base platform consists of one to several platform mounds. Tertiary centres (sites 189 and 192) (Extended Data Fig. 8a, b) comprise a base platform of around 0.5 ha with a single platform situated on it and a circular ditch enclosing a maximum area of 2.5 ha. In addition to these built sites, there is a fourth tier composed of a diversity of small (average 0.34 ha) elevated sites (known as forest islands) that were probably used as temporary campsites or specialized activity sites. A potential fifth tier of small hamlets possibly exists without mounded architecture that cannot be captured by lidar.
Lidar also reveals a clear correlation between the height of civic-ceremonial architecture and the size of the base platform (Supplementary Fig. 2). Within these broad patterns, the civic-ceremonial architecture within each tier is rather variable. This could be related to chronology as well as the function of the sites—a matter that will need to be clarified with future studies.
At the regional level, the lidar data combined with previous archaeological-reconnaissance and remote-sensing data show that the Casarabe culture has a highly integrated, continuous and dense settlement system. Across the 4,500 km2 with documented Casarabe settlement, there are an average of 10 sites (including primary to tertiary centres) within a 10-km radius of each settlement (that is, within a 2-h walk). Density is higher in the eastern sector, with an average distance of 1,800–3,970 m between settlements (Extended Data Fig. 10). Within this distribution, sites tend to be spatially clustered, interconnected by causeways and canals forming clusters encompassing areas ranging from 100 km2 to more than 500 km2 (Extended Data Figs. 3b, 8). Lower-tiered sites typically connect to higher-tier sites, with no formal causeways directly connecting the lower-tiered sites to each other. The large settlement Cotoca is the centre of an area of approximately 500 km2, half forest and half savannah, which includes 18 other monumental sites, which consist of three secondary centres (sites 186, 193 and 195), two tertiary centres (sites 187, 189 and 192), and clusters of small fourth-tier sites to the southeast and the west (Extended Data Figs. 4a, 8). The central role of Cotoca as a primary site is also underlined by the impressive system of canals and causeways that radiate from the base platform in all of the cardinal directions, connecting with lower-tier sites, the Ibare River to the south, and lakes to the east. A 7-km canal brought water from Laguna San José to Cotoca, indicating the scale of landscape management and labour mobilization. Spatial centrality was not a necessity for the location of the principal sites, with primary sites also appearing on the periphery of site clusters (Fig. 1). In the absence of a primary centre, secondary centres could function as the central node for the lower-tiered sites in the region. For example, the secondary centre El Cerrito (site 33) appears to be the centre of an area of around 100 km2 and is surrounded by low-tiered settlements (sites 39, 41 and 106) connected to the core by causeways (Extended Data Fig. 3b).
Our results put to rest arguments that western Amazonia was sparsely populated in pre-Hispanic times28. The architectural layout of large settlement sites of the Casarabe culture indicates that the inhabitants of this region created a new social and public landscape through monumentality. We propose that the Casarabe-culture settlement system is a singular form of tropical agrarian low-density urbanism2—to our knowledge, the first known case for the entire tropical lowlands of South America29,30. The scale, monumentality, labour involved in the construction of the civic-ceremonial architecture and water-management infrastructure, and the spatial extent of settlement dispersal compare favourably to Andean cultures and are of a scale far beyond the sophisticated, interconnected settlements of southern Amazonia31, which lack monumental civic-ceremonial architecture. As such, the data contribute to the discussion of the global wealth of early urban diversity, and will help to redefine the categories used for past and present Amazonian societies.
Lidar technology has revolutionized the documentation of archaeological sites worldwide, especially those hidden under dense forest4,5,6,32,33,34,35,36. In the Amazon lowlands, lidar was first used for archaeological prospection in the Iténez/Guaporé region as part of the 2011 German–Bolivian Project in Mojos (PABAM)9. More recently, lidar has also been used to document archaeological sites in the Amazon regions of Brazil8 and Peru37.
In the present study, we mapped a total of 200 km2 distributed over 6 unconnected areas of varying size of the Casarabe culture area (Fig. 1). The sensor used was a Riegl VUX-1 scanner, with a Trimble APX-15 UAV GNSS, attached to a Eurocopter AS350 helicopter using a custom mount. The laser pulse repetition rate was 200 kHz. Flight altitude was 200 m above ground level, airspeed was 45 knots. Missions were flown in 200-m parallel strips, with 50% overlap. Data post-processing was done by M.S. (ArcTron) using the RIEGL software RiAnalyze. He successfully overcame fundamental problems in the raw data resulting from a time offset of 18 s between raw laser data and trajectory and unusual height differences between point clouds of adjacent tracks. Through mutual manual and partially automated/iterative corrections, at least visually plausible results were achieved after many attempts. The remaining differences of up to 50 cm had to be accepted. Despite these errors, accuracy in the visualization of the archaeological structures is good. Raw point cloud densities varied between 13 million and 20 million points per km2, but generally the density was about 18 million points per km2. The filtering was done automatically taking into account, from the outset, only the last pulses and points with only one reflection. The macros created to pre-classify the point cloud were tested using tiles that best reflected the nature of the terrain. Results were then reviewed and modified until an optimal result with only minor residual errors was achieved. At the end of this process digital elevation model (DEM) LAS files were generated that had a mean point spacing of 0.3 m. From these, DEMs with 50 cm per pixel were generated using the ‘natural neighbours’ method (ArcMap). We used the visualization techniques provided by ArcMap (hillshade, slope) and the relief visualization toolbox (RVT_2.2.1.) developed by the Research Center of the Slovenian Academy of Sciences and Arts38,39,40. Display options were chosen in such a way that they led to an optimal visibility of the archaeological remains.
Volumes were calculated for the built structures of the core area (including the base platform with all platforms and truncated pyramids on it) of the three major monumental sites of our study area (Fig. 2 and Extended Data Figs. 2, 3). At El Cerrito, the built base platform covers 61,970 m2 and has a volume of 323,988 m3. The base platform of Landívar measures 99,795 m2 with a volume of 276,030 m3. The size of the base platform of Cotoca is 159,649 m2 and has a volume of 384,228 m3. Volume calculations were done using ArcGIS by (1) extracting the area of the platforms into a new raster; (2) calculating the ΔZ value of the pixels of that raster; (3) calculating the volume for each pixel; and (4) summing the total volume using the ‘zonal statistics as table’ command.
In total, 144 radiocarbon dates are available for the absolute chronological dating of the Casarabe culture, but these are from a limited number of sites. Stratigraphic information on the dated contexts is available from only four sites (Loma Alta de Casarabe41,42, Mendoza12, Salvatierra11 and Pancho Román43. For the two sites investigated by the PABAM, we have 94 radiocarbon dates (46 from Mendoza and 48 from Salvatierra; Supplementary Figs. 3, 4 and Supplementary Tables 2, 3). Two samples were rejected as outliers. Bayesian analysis of the radiocarbon dates was conducted with OxCal v.4.4.2 and the SHcal20 calibration curve. An additional 50 radiocarbon dates have been published for the sites of Los Aceites, Palmasola, Mary, Kiusíu, Loma Alta de Casarabe, Salvatierra and Pancho Román (Supplementary Fig. 5 and Supplementary Table 4). The 22 radiocarbon dates available for Unit 3 of the Chocolatelito site are unfortunately published in the form of 1α ranges, which prevents their integration into the corresponding list (Supplementary Table 4). Two of the dates fall between ad 0 and 220, which is unusually early and merits closer examination.
Further information on research design is available in the Nature Research Reporting Summary linked to this paper.
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We acknowledge the support of the Departmental Autonomous Government of Beni and of the Bolivian Ministry of Cultures and Tourism. We thank E. Méndez P. and G. Nogales H. from Skyplus in Santa Cruz de la Sierra for their patience and excellent work; R. Torrico, Z. Lehm, H. Salas, M. Gonzalez and S. Tin for their support at different stages of this work; R. Landivar for his explanations of the different names by which Loma Landívar is known. This work was funded by the German Archaeological Institute and supported by Intervenciones Urbanas of the Bolivian Planification Ministry. Lidar data were collected with the VUX-1 lidar sensor acquired by the ERC-PAST project (ERC-CoG 616179) to J.I.
The authors declare no competing interests.
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Extended data figures and tables
a, Lidar image of the central part of the site. Numbered architectural features: 1, principal, U-shaped mound of 22m height; 2-21 smaller platform mounds; 22 and 23, Platforms at the junction of a causeway and the polygonal enclosure. b, Profile cuts of the three enclosures.
a, Location of lidar transect for the Landívar area. b, General plan of the site on which the section shown in c is marked. c, Lidar image of the with profile cuts. Numbered features: 1-5 platform mounds; 6-11, causeways; 12, structure of unknown function. d, Profile cuts A-B and C-D.
a, Location of lidar transect for the El Cerrito area. b, Canals (blue) and causeways (red) found in the area, some of them connecting the pre-Hispanic sites (red triangles). c, Lidar image of El Cerrito. Numbered features: 1, core area platform; 2, truncated pyramid, 3-5, platform mounds. d, Profile cuts A-B and C-D.
a, Layout of Santa María, located in the Cotoca area, is unusual as the site extends on both sides of the paleo-river. Water from the paleo-river was channeled into a circular pond located outside the walled enclosure. Numbered features: 1-4, platform mounds; 5 and 6, reservoir; 7 rampart and moat. b, San Nicolás has twin pyramidal structures, one of which is 17m high.
a, DEM calculated from 20.000 points measured with a total-station (Leica TPS 800) during seven months of surveying (campaigns 2004-2006). b, High-resolution lidar image (DEM; 50cm/pixel).
a, one of the lower platform building at the Cotoca site. b, principal mound at Salvatierra site. Contour lines: 50 cm.
a, site 192. b, site 189. c, site 195. d, site 186 (see Supplementary Table 1).
Extended Data Fig. 9 Examples of (i) openings in enclosures and straight causeways and (ii) platforms at the intersections of causeways and enclosures at the Cotoca site.
a, Opening at the junction of a causeway and the polygonal enclosure. b, Platform at the junction of a causeway and the polygonal enclosure. c, Platform located at the opening of the causeway likely caused by a river. On the opposite shore, the causeway continues in a southeastern direction.
a, 10-km buffer zone map with no buffer boundaries showing how the region was continuously occupied. b, Kernel site density map showing the highest concentration of sites in the eastern portion of the study area.
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Prümers, H., Betancourt, C.J., Iriarte, J. et al. Lidar reveals pre-Hispanic low-density urbanism in the Bolivian Amazon. Nature 606, 325–328 (2022). https://doi.org/10.1038/s41586-022-04780-4