| 0 | PI 548848 | 14161 | Bejaria aestuans Mutis | Ecuador | | | Historic | 1990 | COLLECTED | 11/14/1990 | Cloud forest. Road to Cerro Toledo, 8-10km E of and above Yangana, Loja province | -4.33333333, -79.13333333 | 2460 | | Wild material | Shrub to 1 m tall in burned-over areas, to tree 10m tall x 20cm dbh. in undisturbed cloud forest. Petals pink. Flowers fragrant. Abundant. | 1443784 | PI 548848 |
| 1 | PI 548849 | 14175 | Bejaria aestuans Mutis | Ecuador | | | Historic | 1990 | COLLECTED | 11/14/1990 | Loma de Oro area, approx. 12km N of San Lucas, Lojo province | -3.66666667, -79.25000000 | 2954 | | Wild material | Shrub (on this burned over site), 1.0-1.5m tall. Flower petals light pink to dark rose-red. Capsules tan. Common. B. resinosa also occurs on the site | 1443785 | PI 548849 |
| 2 | PI 548850 | 14133 | Bejaria resinosa Mutis ex L. f. | Ecuador | | | Historic | 1990 | COLLECTED | 11/13/1990 | Shrub paramo with Befaria, Gaultheria, Macleania, Rubus, Vaccinium, Proteaceae and braken fern. Paramo de Tinajillas, approx. 64.7km S of Cuenca, along road to Loja, Azuay province | -3.28333333, -79.16666667 | 3323 | | Wild material | Terrestrial shrub to 3m tall. Inflorescence viscid. Corolla essentially tubular, deep pink to dark rose. Capsule brown. Abundant. Excellent ornamental. | 1443786 | PI 548850 |
| 3 | PI 51786 | No. 488a | Bejaria mathewsii Fielding & Gardner | Cundinamarca, Colombia | | | Historic | 1920 | COLLECTED | 10/14/1920 | | | | | | | 1506069 | PI 51786 |
| 4 | NA 89179 | 2025RJLSEUS-32 | Bejaria racemosa Vent. | Georgia, United States | NA | | Not Available | 2026 | COLLECTED | 10/14/2025 | Ceylon Wildlife Management Area (WMA): The collecting site is along an unnamed south-bound sand road that intersects the WMA road approximately 0.88 kilometers east of the intersection with Lang Lane near the entrance to the WMA. | 30.94310700, -81.66119700 | 9 | Growing in full sun of a managed Pinus taeda forest, largely, though incompletely, logged in the past 1-3 years; it has recently been subjected to a prescribed fire (probably late 2024). This lowland flatwood habitat has a rich assemblage of herbaceous and woody vegetation, both evergreen and deciduous. Slope: 0 percent. Aspect: N/A. Soil: The soils here are classified as Pottsburg Series sand (95 percent) with a small contribution from Rutlege Series loamy sand. The Pottsburg Series consists of very deep, moderately permeable, poorly drained sands with low surface runoff. The typical pedon is nearly flat to less than 1 percent slope unless disturbed; this site has seen considerable logging and is definitely disturbed. Soils are fine grained sand to medium grained sand and friable due to coating with organic matter. Soil reaction ranges from extremely acid to slightly acid. It appears that long-term management of this site has resulted in drainage systems that promote some runoff. Resulting drier surface conditions of this forest seem to have allowed the establishment of odd complexes of species from diverse habitat preferences to form communities. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area originated in the Pleistocene Era area and is characterized as Pamlico shoreline complex - Marsh and Lagoonal Facies. The Pamlico shoreline complex features lagoonal facies of fine silts and clays with organic matter (peat) from low-energy bay/marsh environments, often underlying nearshore marsh/barrier sands, while marsh facies are dominated by dark, organic-rich peats and silty clays deposited in vegetated intertidal zones, showing plant remains, interbedded with fine sands, all reflecting sea-level fluctuations on the Atlantic Coastal Plain. (Source: USGS Georgia Geologic Map Data). | Wild material | | 2193313 | NA 89179 |
| 5 | NA 89177 | 2025RJLSEUS-29 | Bejaria racemosa Vent. | Florida, United States | NA | | Not Available | 2026 | COLLECTED | 10/12/2025 | Crooked Lake Prairie Nature Preserve: accessed by foot along a sugar sand trail approximately 0.48 kilometers from the parking lot at the end of Ohlinger Road. | 27.80656300, -81.56428800 | 38 | Growing on sugar sand in part shade to part sun of a remnant dry, xeric Lake Wales Ridge habitat. The habitat is a mix of "islands" of larger woody vegetation, savannas comprised of more herbaceous flora dominated by grasses, and mixed evergreen and deciduous scrub flora. It seems that small changes in elevation around the edges of Crooked Lake allow for variation in habitats and floristic diversity. Slope: 0 percent. Aspect: N/A. Soil: The soils here are primarily Archbold Series sand, 0 to 5 percent slopes (90 percent) with small contributions from Satellite Series sand, 0 to 2 percent slopes (5 percent) and St. Lucie Series sand, 0 to 8 percent slopes (5 percent). The Archbold Series consists of deep, well drained, very rapidly permeable sandy soils that formed in marine or eolian deposits. These droughty soils are on low ridges in central Florida. Slopes are typically 0 to 5 percent. The soil reaction is slightly to extremely acid. The soil is sand or fine sand throughout. The silt plus clay content in the 25-100 depth is less than 2 percent; even so, they contain slightly more moisture in times of abundant rainfall. The Satellite Series consists of very deep, somewhat poorly drained, rapidly permeable soils on low knolls and ridges of the Southern Florida Flatwoods and less commonly on the South-Central Florida Ridge They formed in thick beds of marine sand. Soil reaction ranges from very strongly acid to slightly alkaline in all horizon. This soil can become saturated 25-100 cm below the surface during the summer rainy season. The St. Lucie Series consists of very deep, excessively drained soils that formed in sandy marine and/or eolian deposits. St. Lucie Series soils are on dunes, ridges, and knolls on marine terraces. Slopes range from linear to convex and range from 0 to 20 percent. This soil is strongly to extremely acid in the upper 200 cm of the horizon but can have neutral to alkaline components as well. The genesis of the St. Lucie Series soil is not clearly understood. No subsurface diagnostic horizons are within depths of 2 meters, but the uncoated sand grains suggest an albic horizon. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The Reworked Cypresshead Sediments is of Pliocene/Pleistocene origin. This unit is the result of post depositional reworking of the Cypresshead siliciclastics. The sediments are fine to coarse quartz sands with scattered quartz gravel and varying percentages of clay matrix that is undifferentiated. (Source: USGS Florida Geologic Map Data). | Wild material | | 2193311 | NA 89177 |
| 6 | NA 89176 | 2025RJLSEUS-26 | Bejaria racemosa Vent. | Florida, United States | NA | | Not Available | 2026 | COLLECTED | 10/10/2025 | Hickory Lake Scrub Preserve, 1658 Scenic Highway Frostproof, FL 33843. The Hickory Lake Scrub Preserve was purchased in August 1997 from the Green Horizon Land Trust, a local nonprofit organization dedicated to preserving environmentally significant land. This property is now managed by Polk County’s Environmental Lands Program. | 27.69781400, -81.53797800 | 32 | Growing on sugar sand in full sun and extremely dry, xeric Lake Wales Ridge habitat comprised of a remarkably rich evergreen and deciduous plant community. The habitat is subjected to periodic prescribed fire (most recent estimated to be 2-3 years ago). Slope: 0 percent. Aspect: N/A. Soil: The soil of this site is characterized as St. Lucie Series fine sand, 0 to 5 percent slopes; with other minor contributions from Archbold, Myakka, and Cassia not described here. The St. Lucie Series consists of very deep, excessively drained soils that formed in sandy marine and/or eolian deposits. St. Lucie soils are on dunes, ridges, and knolls on marine terraces. Slopes range from linear to convex and range from 0 to 20 percent. This soil is strongly to extremely acid in the upper 200 cm of the horizon but can have neutral to alkaline components as well. The genesis of the St. Lucie soils is not clearly understood. No subsurface diagnostic horizons are within depths of 2 meters, but the uncoated sand grains suggest an albic horizon. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). Geology: The underlying geology of this area is characterized as Reworked Cypresshead Sediments from the Pliocene/Pleistocene. This unit is the result of post depositional reworking of the Cypresshead siliciclastics. The sediments are fine to coarse quartz sands with scattered quartz gravel and varying percentages of clay matrix that is undifferentiated. (Source: USGS Florida Geologic Map Data). | Wild material | | 2193310 | NA 89176 |