| 0 | PI 102244 | 62174 | Cyrilla racemiflora L. | France | NA | | Not Available | 1993 | COLLECTED | 1957 | | | | | Wild material | Deciduous shrub, up to 12' high with spreading habit. Leaves obovate, dark lustrous green, turning red in autumn. Flower in slender racemes, produced in late June followed by yellow fruit. The habit and profusion of bloom give this species a distinctive quality. Propagation is by root cuttings. | 1492658 | PI 102244 |
| 1 | PI 80049 | | Cyrilla racemiflora L. | Pennsylvania, United States | | | Historic | 1929 | COLLECTED | | | | | | | | 1496258 | PI 80049 |
| 2 | NA 88757 | 2025 TKRM-001 | Cyrilla racemiflora L. | Florida, United States | NA | | | 2025 | COLLECTED | 01/03/2025 | Area on the south side of an unnamed sand road, about 0.54 kilometers south of Florida State Highway 98 and accessed from Walton County Highway 283 S. The collecting site is accessed by going east 0.54 kilometers on the unnamed sand road from the junction with Walton County Highway 283 S. | 30.35374700, -86.15172700 | 12 | Mostly found in moist to dry flatwoods in mixed evergreen and deciduous forest. Slope: N/A. Aspect: various. The underlying geology of this area is characterized as undifferentiated Quaternary Sediments. Much of Florida's surface is covered by a varying thickness of undifferentiated sediments consisting of siliciclastics, organics and freshwater carbonates. Where these sediments exceed 6.1 meters thick, they were mapped as discrete units. In an effort to subdivide the undifferentiated sediments, those sediments occurring in flood plains were mapped as alluvial and flood plain deposits (Qal). Sediments showing surficial expression of beach ridges and dunes were mapped separately (Qbd) as were the sediments composing Trail Ridge (Qtr). Terrace sands were not mapped (refer to Healy [1975] for a discussion of the terraces in Florida). The subdivisions of the Undifferentiated Quaternary Sediments (Qu) are not lithostratigraphic units but are utilized in order to facilitate a better understanding of the State's geology. The siliciclastics are light gray, tan, brown to black, unconsolidated to poorly consolidated, clean to clayey, silty, unfossiliferous, variably organic-bearing sands to blue green to olive green, poorly to moderately consolidated, sandy, silty clays. Gravel is occasionally present in the panhandle. Organics occur as plant debris, roots, disseminated organic matrix and beds of peat. Freshwater carbonates, often referred to as marls in the literature, are scattered over much of the State. In southern Florida, freshwater carbonates are nearly ubiquitous in the Everglades. These sediments are buff colored to tan, unconsolidated to poorly consolidated, fossiliferous carbonate muds. Sand, silt and clay may be present in limited quantities. These carbonates often contain organics. The dominant fossils in the freshwater carbonates are mollusks. (Source: USGS Florida Geologic Map Data). The Hurricane Series consists of very deep, somewhat poorly drained, moderately rapid permeable soils on broad areas that are slightly higher than the adjacent flats in the Southern Coastal Plain (MLRA 133A), the Gulf Coast Flatwoods (MLRA 152A) and the Atlantic Coast Flatwoods (MLRA 153A). They formed in sandy marine sediments. Slopes range from 0 to 5 percent. Solum thickness is 1.5 meters or more. Reaction ranges from extremely acid to moderately acid throughout. (Source: California Soil Resource Lab/NRCS Official Soil Series Descriptions). | Wild material | Received as Cyrilla parvifolia. | 2171019 | NA 88757 |
| 3 | WLP 3411 | TJK2023FL-044 | Cyrilla racemiflora L. | Florida, United States | NA |  | | 2024 | COLLECTED | 12/26/2023 | Forest Hill Cemetery, east fence line, 0.4 mi north of Hwy 98, off Twine Rd. | 29.78030000, -85.27160000 | 7 | Growing on the edge of a wet pine savanna/flatwood. Slope: flat. Aspect: Southeast. Elevation: 23 feet. | Wild material | | 2165704 | WLP 3411 |
| 4 | NA 88823 | TJK2023FL-040 | Cyrilla racemiflora L. | Florida, United States | NA | | | 2023 | COLLECTED | 12/11/2023 | Eglin Air Force Base, Range Road 352, south of Basin Bayou Reservation Area, north of Alaqua Bayou. | 30.48550000, -86.22020000 | 4 | Wet pine flatwoods. Slope: 3%. Aspect: Southeast. Elevation: 14 feet. | Wild material | | 2165652 | NA 88823 |
| 5 | NA 88531 | RJLSEUS2022-002 | Cyrilla racemiflora L. | North Carolina, United States | NA | | | 2023 | COLLECTED | 12/06/2022 | Plants growing around a wetland on both sides of Scotland Lake Road, approximately 1.1 kilometers southwest of the junction with Hoffman Road (Scotland Co. Road 1328) in the Sandhills Game Lands. This plant is a common component of moist to wet areas of the wetland habitats in this area. | 34.98418000, -79.54079800 | 120 | Plants are growing in part-shade to sun in a wetland habitat as well as nearby seasonally drier mesic habitat.
Soils: The underlying geology of this area is of Tertiary origin and characterized as Pinehurst Formation. It is comprised of medium- to coarse-grained sand as well as cross-bedding and rhythmic bands of clayey sand that are unconsolidated.
Source: USGS North Carolina Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=NCTp%3B11)
The primary soil type in the collection area is classified as Johnston Series soils (0 to 2 percent slopes, frequently flooded). The Johnston series consists of very deep, very poorly drained soils that are occasionally to frequently flooded for short to extended periods. Permeability is moderate to rapid. These nearly level soils are alluvial in origin and typical of floodplains and swamp. Slopes range from 0 to 2 percent. Johnston Series soils are comprised of mucky loam that is friable with siliceous elements in the upper 0-75 cm. Lower strata range in percentages of mucky loam and loamy fine sand.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) | Wild material | | 2140760 | NA 88531 |
| 6 | NA 88162 | NCBG-407 | Cyrilla racemiflora L. | North Carolina, United States | NA |  | | 2019 | | | | | | | Wild material | | 2098433 | NA 88162 |
| 7 | WLP 1128 | GF2018-06 | Cyrilla racemiflora L. | Georgia, United States | NA | | | 2018 | COLLECTED | 11/07/2018 | Tattnall County; ; 1.7 miles east of Highway 169 on Mack Phillips Rd, 600 feet southwest of road in Big Hammock WMA. | 31.86714000, -82.05540000 | 28 | Wetland, at the base of sand hammock. | | | 2108888 | WLP 1128 |
| 8 | WLP 1130 | GF2018-09 | Cyrilla racemiflora L. | Florida, United States | NA | | | 2018 | COLLECTED | 11/08/2018 | Liberty County; ; Apalachicola National Forest, 500 feet north of National Forest Rd 112, 0.2 miles west of Hwy 65. | 30.21855000, -84.89692000 | 18 | Swampy area. | | | 2108891 | WLP 1130 |
| 9 | WLP 1084 | NA 81870 | Cyrilla racemiflora L. | Alabama, United States | NA | | | 2009 | COLLECTED | | | 33.05852000, -87.03390000 | 310 | | | | 1923662 | WLP 1084 |
| 10 | NA 78033 | AL #42 | Cyrilla racemiflora L. | Alabama, United States | NA | | | 2008 | COLLECTED | 09/17/2008 | Alabama: Bibb County, just above the Cahaba River, near end of road and Caffee Creek | | | mixed woodland at edge of creek | Wild material | | 1913893 | NA 78033 |
| 11 | NA 56783 | NA 56783 | Cyrilla racemiflora L. | | NA | | Not Available | 1985 | | | | | | | | | 1950768 | NA 56783 |
| 12 | NA 56784 | NA 56784 | Cyrilla racemiflora L. | Alabama, United States | NA | | Not Available | 1985 | COLLECTED | | Mobile County; ; | | | | | | 2108360 | NA 56784 |