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Your query included: All accessions taxonomy genus name like Lyonia

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ACCESSIONPLANT NAMETAXONOMYORIGINGENEBANKIMAGEAVAILABILITYRECEIVEDSOURCE TYPESOURCE DATECOLLECTION SITECOORDINATESELEVATIONHABITATIMPROVEMENT LEVELNARRATIVE
0PI 287724Lyonia nezikii Nakai & H. Hara Japan Historic1963COLLECTED1689786PI 287724
1PI 285379Col. No. 1167Lyonia ovalifolia (Wall.) Drude Nepal Historic1962COLLECTEDOpen fields on Mt. Furkai33111688831PI 285379
2PI 139242No. 5280Lyonia lucida (Lam.) K. Koch Georgia, United States Historic1940COLLECTED08/24/19409.6km north of Fargo1862469PI 139242
3PI 130434No. 7963Lyonia sp.Yunnan Sheng, China Historic1938COLLECTEDDokerla, Atuntze28001846368PI 130434
4PI 130435No. 10896Lyonia sp.Yunnan Sheng, China Historic1938COLLECTEDBaimashan, Atuntze32001846369PI 130435
5PI 130436No. 13884Lyonia sp.Yunnan Sheng, China Historic1938COLLECTEDTehgoh, Chungtien33001846370PI 130436
6PI 130438No. 15045Lyonia sp.Yunnan Sheng, China Historic1938COLLECTEDLikiang Snow Range30001846372PI 130438
7PI 130439No. 15322Lyonia sp.Yunnan Sheng, China Historic1938COLLECTEDLikiang Snow Range28001846373PI 130439
8PI 130437No. 14702Lyonia sp.Yunnan Sheng, China Historic1938COLLECTEDWati, Muli29001846371PI 130437
9PI 128984Lyonia ovalifolia (Wall.) Drude India Historic1938COLLECTED1845155PI 128984
10PI 105927Lyonia sp.Himachal Pradesh, India Historic1934COLLECTEDBangar1793849PI 105927
11PI 103262No. 24279Lyonia ovalifolia (Wall.) Drude Yunnan Sheng, China Historic1933COLLECTEDMiturong Muli Territory34621791583PI 103262
12PI 103263No. 24400Lyonia ovalifolia (Wall.) Drude Sichuan Sheng, China Historic1933COLLECTEDMount Siga, west of the Yalung River37631791584PI 103263
13PI 100103F. 30437Lyonia ovalifolia (Wall.) Drude China Historic1932COLLECTED1787466PI 100103
14PI 99759Lyonia ovalifolia (Wall.) Drude India Historic1932COLLECTED1787086PI 99759
15PI 68341Lyonia ovalifolia (Wall.) Drude West Bengal, India Historic1926COLLECTED1721053PI 68341
16PI 64121Lyonia ovalifolia (Wall.) Drude West Bengal, India Historic1925COLLECTED1665468PI 64121
17PI 60653Lyonia ovalifolia (Wall.) Drude West Bengal, India Historic1924COLLECTED1662258PI 60653
18PI 47755Lyonia ovalifolia (Wall.) Drude West Bengal, India Historic1919COLLECTED1613377PI 47755
19PI 39127Lyonia villosa (Hook. f. ex C. B. Clarke) Hand.-Mazz. West Bengal, India Historic1914COLLECTED1604008PI 39127
20PI 4785Lyonia ligustrina (L.) DC. United States Historic1900COLLECTED1540205PI 4785
21PI 1562'Andromeda japonica'Lyonia ovalifolia (Wall.) Drude France Historic1898COLLECTED1534016PI 1562
22NA 885892024RM-002Lyonia ferruginea (Walter) Nutt. Florida, United StatesNA2024COLLECTED11/21/2024Eglin Air Force Base: collected along an unnamed sand road that leads to the former Flowers Boat Landing (now permanently closed) along the Yellow River. Accessed by boat.30.60823600, -86.835955006Mixed evergreen and deciduous open habitat in part shade to full sun. Slope: 0 to 1 percent. Aspect: N/A. The underlying geology of this area is characterized as Alluvium from 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 20 feet (6.1 meters) thick, they were mapped as discrete units. 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 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 soils of this are characterized as Dorovan-Pamlico Series association. The Dorovan Series consists of very deep, very poorly drained, moderately permeable soils on densely forested flood plains, hardwood swamps, and depressions in the Atlantic Coast Flatwoods (153A), Eastern Gulf Coast Flatwoods (152A), and Southern Coastal Plain Major (133A) Land Resource Areas. They formed in highly decomposed acid-organic materials. Slopes are less than 1 percent. The organic material ranges from 1.3 to 2 meters or more thick. Reaction is extremely acid to very strongly acid in the organic layers and very strongly acid or strongly acid in the mineral layers. The Pamlico Series consists of very poorly drained soils that formed in decomposed organic material underlain by dominantly sandy sediment. The soils are on nearly level flood plains, bays, and depressions of the Coastal Plain. Slopes are less than 1 percent. Pamlico soils have 0.4 to 1.3 meters of organic material over dominantly sandy sediments. Reaction is extremely acid (less than 4.5 in 0.01 M calcium chloride) in the organic layers, and ranges from extremely acid to strongly acid in the underlying mineral layers.Wild material2169926NA 88589
23NA 88853TJK2023FL-048Lyonia ferruginea (Walter) Nutt. Florida, United StatesNA2024COLLECTED12/26/2023South of Highway 98, west of Twine Road. Track has a very large powerline right-of-way to the east, and George Washington Swamp bottom to the west.29.77560000, -85.274000006Longleaf Pine-Saw Palmetto. This area appears to be declining in quality, as witnessed by the declining in Rhododendron stem/plant density. Possible contributing issues: lacking necessary fire regime, has not seen fire in 8-10 years, encroaching woody shrub layer, accumulating organic matter (pine needle), expanding tree canopy, Hurricane Michael. Slope: less than 2%. Aspect: Northeast. Elevation: 20 feet.Wild material2165708NA 88853
24WLP 3412TJK2023FL-045Lyonia lucida (Lam.) K. Koch Florida, United StatesNA2024COLLECTED12/26/2023East backwoods adjacent to Forest Hill Cemetery, 0.4 mi north of Hwy 98, off Twine Rd.29.78030000, -85.271600007Edge of a wet pine savanna/flatwood. Slope: flat. Aspect: Southeast. Elevation: 23 feet.Wild material2165705WLP 3412
25NA 88699RJL2023NCSC-004Lyonia ligustrina (L.) DC. North Carolina, United StatesNA2023COLLECTED11/13/2023Sandhills Game Land: north side of Pulpwood Road approximately 0.11 km southwest of the junction with Tyner Road.34.95949000, -79.48665600107Plants growing in part-shade to sun on the moist margins of a spring fed wetland that is a mixed evergreen and deciduous woodland habitat. The underlying soils are moist even during dry periods due to seepage from the wetland. Slope: 3 to 10 percent. Aspect: Northeast. The underlying geology of this area is of Tertiary origin and characterized as Pinehurst Formation. It is comprised of sand that is medium- to coarse-grained, cross-bedding and rhythmic bands of clayey sand common, unconsolidated. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in the area of this collection is classified as Pelion loamy sand, 6 to 10 percent slopes. Pelion Series soils are very deep, moderately well-drained soils with moderately slow to slow permeability. The upper 30 cm of the strata is sandy loam to sandy clay loam ranging from grayish brown to reddish yellow. This stratum has a weak fine granular structure and is very friable. It contains many fine roots and is moderately acid. Deeper strata to 2 m range from yellow to yellowish red sandy clay, often with masses of oxidized iron and few fine prominent light gray iron depletions; they are strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159127NA 88699
26NA 88703RJL2023NCSC-008Lyonia lucida (Lam.) K. Koch North Carolina, United StatesNA2023COLLECTED11/13/2023Sandhills Game Land: north side of Pulpwood Road approximately 0.11 km southwest of the junction with Tyner Road.34.95848900, -79.48618700101Plants growing in moist-mesic to seasonally saturated soils in shade to part-shade of a spring fed wetland that is a mixed evergreen and deciduous woodland habitat. Slope: 0 to 5 percent. Aspect: Various. The underlying geology of this area is of Tertiary origin and characterized as Pinehurst Formation. It is comprised of sand that is medium- to coarse-grained, cross-bedding and rhythmic bands of clayey sand common, unconsolidated. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in the area of this collection is classified as Pelion loamy sand, 6 to 10 percent slopes. Pelion Series soils are very deep, moderately well-drained soils with moderately slow to slow permeability. The upper 30 cm of the strata is sandy loam to sandy clay loam ranging from grayish brown to reddish yellow. This stratum has a weak fine granular structure and is very friable. It contains many fine roots and is moderately acid. Deeper strata to 2 m range from yellow to yellowish red sandy clay, often with masses of oxidized iron and few fine prominent light gray iron depletions; they are strongly acid. (Source: NRCS Web Soil Survey.)Wild material2159131NA 88703
27NA 88685TJK2023FL-032Lyonia ligustrina (L.) DC. Florida, United StatesNA2023COLLECTED11/18/2023Blackwater State Forest: Wolfe Creek.30.80844000, -86.9624300055Drier ridge above seepage slope. Slope: less than 2%. Aspect: South. Elevation: 180 feet.Wild material2159097NA 88685
28NA 88639KY23-042Lyonia ligustrina (L.) DC. Kentucky, United StatesNA2023COLLECTED09/11/2023Daniel Boone National Forest: Bee Rock Loop Trail along Rockcastle River.37.04179000, -84.31805000233Riverscour grassland. Elevation: 765 feet. Aspect: East.Wild material2158731NA 88639
29WLP 3213TXWL2023-001Lyonia mariana (L.) D. Don Texas, United StatesNA2023COLLECTED08/22/2023Angelina National Forest.31.05522100, -94.26205200Baygall below longleaf [pine] stand.Wild material2158757WLP 3213
30WLP 3090RM2023-008Lyonia lucida (Lam.) K. Koch Alabama, United StatesNA2023COLLECTED12/29/2022This plant is growing along the steep edges of Gantt Lake, accessed by boat. Occasional in shaded areas around Gantt Lake.31.40780000, -86.4677000068The plants were growing in open conditions on a steep north-facing bluff above Gantt Lake.
Soils: The underlying geology of this area is Claiborne Group, Tallahatta Formation, of Eocene origin, with white to very light-greenish-gray thin-bedded to massive siliceous claystone; interbedded with thin layers of fossiliferous clay, sandy clay, and glauconitic sand and sandstone.
Source: USGS Alabama Geological Map Data (https://mrdata.usgs.gov/geology/state/state.php?state=AL)
The surface soil profile of this area is primarily Bibb-Kinston Series Association. Bibb Series soils are coarse-loamy, sandy, acid soils that are poorly drained. They are soils of flood plains and streams subject to frequent flooding. These are found in association with Kinston Series soils that are fine-loamy, sandy, acid soils of flood plains and stream subject to frequent flooding. The Bibb-Kinston association ranges from 1-1.5 meters thick and is strongly acid.
Source: Soil Survey of Santa Rosa County and NRCS Web Soil Survey (https://www.nrcs.usda.gov/Internet/FSE_MANUSCRIPTS/florida/FL113/0/SantaRosa.pdf and https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2141444WLP 3090
31WLP 2677RJL2022NJ-008Lyonia ligustrina (L.) DC. New Jersey, United StatesNA2022COLLECTED10/24/2022Plants growing along Burlington County Road 563, Green Bank Chatsworth Road, on the west side of the road, 16.22 kilometers south of the intersection with New Jersey Hwy 72. Plants are common at this location. 39.73274000, -74.5344900015Plants growing in a depression wetland habitat in full sun. This location seems somewhat historically disturbed by development of cranberry bogs surrounding the wet site.
Soils: The underlying geology of this area is the Cohansey Formation of middle Miocene origin and comprised of sand, white to yellow with local gravel and clay. It is sometimes locally stained red or orange brown by iron oxides and (or) cemented into large blocks of ironstone. Unweathered clay is typically dark gray, but commonly weathers white where it is interbedded with thin beds of ironstone. Sand is typically medium grained and moderately sorted although it ranges from fine to very coarse grained and from poorly to well sorted. Sand consists of quartz and siliceous rock fragments. Some beds are locally micaceous. Maximum thickness in the map area is about 60 meters; however, thickness is difficult to determine because of the irregular basal contact and extensive post-depositional erosion.
Source: USGS New Jersey Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=NJTch%3B1)
The primary soil type in the area of this collection is classified as Atsion sand, 0 to 2 percent slopes, Northern Tidewater Area. The area is close and probably overlapping with Lakehurst sand series soil. Atsion series soil is poor to slowly draining and comprised primarily of sandy marine sediments. Surface runoff is slow to very slow. This soil is strongly to extremely acid throughout the profile. This soil is generally 50-100 cm deep.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139668WLP 2677
32WLP 2673RJL2022NJ-004Lyonia mariana (L.) D. Don New Jersey, United StatesNA2022COLLECTED10/24/2022Plants growing on both sides of Duerer Street approximately 0.37 kilometers southeast of 4th Avenue, Mullica Township, New Jersey. Plants are common but scattered on both sides of the road at this site. 39.55730700, -74.6637610022Plants grow from part shade to full sun throughout the habit from the upper edges of the ditches through the herbaceous grass dominant buffer and all the way to the part shade of the woodland edge. Plants transition through moist/wet conditions in full sun to quite dry conditions in part shade and seem equally adapted.
Soils: The underlying geology of this area is the Cohansey Formation of middle Miocene origin and comprised of sand, white to yellow with local gravel and clay. It is sometimes locally stained red or orange brown by iron oxides and (or) cemented into large blocks of ironstone. Unweathered clay is typically dark gray, but commonly weathers white where it is interbedded with thin beds of ironstone. Sand is typically medium grained and moderately sorted although it ranges from fine to very coarse grained and from poorly to well sorted. Sand consists of quartz and siliceous rock fragments. Some beds are locally micaceous. Maximum thickness in the map area is about 60 meters; however, thickness is difficult to determine because of the irregular basal contact and extensive post-depositional erosion.
Source: USGS New Jersey Geologic Map Data (https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=NJTch%3B1)
The primary soil type in the area of this collection is classified as Mullica sandy loam, 0 to 2 percent slopes. These soils are typically coarse-loamy, siliceous, semiactive, and mesic typic humaquepts that are strongly to extremely acidic throughout the profile. The typical solum thickness ranges from 50-150+ cm. These soils are generally considered to be poorly drained.
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139664WLP 2673
33NA 89041RJL2022MD-015Lyonia ligustrina (L.) DC. Maryland, United StatesNA2022COLLECTED10/05/2022Plants growing at Elkton State Forest along road and in wet woodlands near the Elk Neck State Forest Shooting Range labelled as the address of 717 Irishtown Rd, North East, MD 21901. Plants are common but scattered on the edges and in the understory of low-lying wet woodlands. 39.58716100, -75.9141900055Plants are growing in part-shade to shade of deciduous forests on moist slopes and on hummocks in very moist to wet low-lying areas along seasonal or year-round flowing seeps.
Soils: The underlying geology of this area is of Cretaceous origin and comprised of Potomac Group, including Raritan and Patapsco Formations, and Patuxent Formation. The Potomac Group includes: interbedded quartzose gravels; proto-quartzitic to orthoquartzitic argillaceous sands; and white, dark gray, and multicolored silts and clays. Included withing this zone are Raritan and Patapsco Formations comprised of gray, brown, and red variegated silts and clays; lenticular, cross-bedded, argillaceous, subrounded sands; minor gravels; thickness. The Patuxent Formation is also interbedded in this zone and comprised of white or light gray to orange-brown, moderately sorted, cross-bedded, argillaceous, angular sands and subrounded quartz gravels; silts and clays subordinate that are predominantly pale gray.
Source: USGS Maryland Geologic Map Data https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=MDKp%3B5
The primary soil types in the collection area are classified as Russett-Christiana-Hambrook Complex and/or Sassafras and Croom Soils; though, others may intersect and overlay in specific areas. The soils in the collecting area are generally described as a complex series of fluviomarine deposits. The soils range from a thin loam layer at the surface to varying levels of loam to sandy loam and/or extremely gravelly sandy clay loam strata, depending upon geographical location (ie. Hillslope summits, slopes, footslopes, swales, etc.).
Source: NRCS Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)		Wild material2139606NA 89041
34NA 88402NCBG-633Lyonia ligustrina (L.) DC. Maryland, United StatesNA2021Wild material2116359NA 88402
35NA 88403MARSB-542Lyonia mariana (L.) D. Don New Jersey, United StatesNA2021Wild materialGrowth formûthe plant is a shrub (i.e., a woody plant with several stems growing from the base)ûLeaf typeûthe leaf blade is simple (i.e., lobed or unlobed but not separated into leaflets)ûLeaves per nodeûthere is one leaf per node along the stemûLeaf blade edgesûthe edge of the leaf blade has no teeth or lobesûLeaf durationûthe leaves drop off in winter (or they wither but persist on the plant)ûarmature on plantûthe plant does not have spines, prickles, or thornsûLeaf blade lengthû25–105 mmûLeaf blade widthû10–50 mmûLeaf stalkûthe leaves have leaf stalksûFruit type (general)ûthe fruit is dry and splits open when ripeûBark textureûthe bark of an adult plant is thin and smoothûthe bark of an adult plant peels off easily or hangs offûTwig winter colorûgrayûBud scale numberûthere are two scales on the winter bud, and their edges meet2113554NA 88403
36NA 88136NEWFS-627Lyonia ligustrina (L.) DC. Maine, United StatesNASEED2019Wild material2098239NA 88136
37NA 88094MARSB-241Lyonia mariana (L.) D. Don New York, United StatesNASEED2019Wild material2097533NA 88094
38NA 88098MARSB-294Lyonia mariana (L.) D. Don New Jersey, United StatesNASEED2019Wild material2097561NA 88098
39NA 88099MARSB-295Lyonia mariana (L.) D. Don New Jersey, United StatesNASEED2019Wild material2097562NA 88099
40NA 88100MARSB-303Lyonia mariana (L.) D. Don New Jersey, United StatesNASEED2019Wild material2097564NA 88100
41NA 88104MARSB-398Lyonia mariana (L.) D. Don New York, United StatesNASEED2019Wild material2097612NA 88104
42NA 88111MARSB-428Lyonia ligustrina (L.) DC. New Jersey, United StatesNASEED2019Wild material2097629NA 88111
43WLP 1381PCC18-HON-006Lyonia ovalifolia (Wall.) Drude var. elliptica (Siebold & Zucc.) Hand.-Mazz. Honshu, JapanNA2018COLLECTED09/14/2018Tochigi Prefecture, Shioya-gun; Shioya-machi; Funyu Forest - Utsunomiya University Forest.36.78213000, 139.82423000400Mesic forest dominated by Pinus densiflora, Tsuga sieboldii, and occasional deciduous trees; top of north-south ridge above a hinoki (Chamaecyparis obtusa) plantation; south edge of collecting site with a large canopy gap. Soil A horizon light tan, clayey; lots of organic matter.Seed collected from two plants; three herbarium vouchers collected; photographed.2108911WLP 1381
44WLP 1382NACPEC18-097Lyonia ovalifolia (Wall.) Drude var. elliptica (Siebold & Zucc.) Hand.-Mazz. Hubei Sheng, ChinaNA2018COLLECTED09/21/2018Shennongjia Forest District; Muyuping; Shennongjia National Park, Guanmenshan.31.43431000, 110.357580001535Rich deciduous forest in narrow valley along tributary of river. Growing in humus over rocks.Seeds and four herbarium specimens collected from one plant. Photographed.2108991WLP 1382
45NA 81714NA 81714Lyonia ligustrina (L.) DC. Maryland, United StatesNANot Available2013COLLECTED12/05/2013Cedarville State Forest near Brandywine/Waldorf, MD, Cedarville Pond.49Along northeast and southeast sides of pond and in swampy areas under deciduous canopy.1951926NA 81714
46WLP 1357MDPO 2012-012Lyonia mariana (L.) D. Don Maryland, United StatesNA2012COLLECTED10/17/201238.35340000, -75.41360000471922750WLP 1357
47WLP 2212LBJWC-MLE-19Lyonia mariana (L.) D. Don Texas, United StatesNASEED2012COLLECTED07/24/2006Sandyland Sanctuary, north of railroad, adjacent to lily pond30.38656000, -94.2567300014Longleaf pine woodlands; land form: sandy highlands, lower boggy/wet areas. Land used for conservation. Soil sand, white.Wild material1902490WLP 2212
48WLP 1341RL 07023Lyonia lucida (Lam.) K. Koch Florida, United StatesNA2007COLLECTEDFlorida: Orange County, North of Apopka, in longleaf pine-oak scrub lands of Wekiwa Springs Park.1925086WLP 1341
49NA 71249NA 71249Lyonia ligustrina (L.) DC. New York, United StatesNANot Available2000COLLECTED10/199941.00000000, -72.0833300051950977NA 71249
50NA 64840NA 64840Lyonia ovalifolia (Wall.) Drude var. elliptica (Siebold & Zucc.) Hand.-Mazz. Hubei Sheng, China Historic1994COLLECTED09/20/1994Wudang Shan.32.39527778, 111.01638889Moist slopes with Pinus tabuliformis, Quercus aliena, Ilex pernyi.Wild material1511670NA 64840
51Ames 10170Ames 10170Lyonia ligustrina (L.) DC. Michigan, United States Historic1989DEVELOPEDSeed received from W.J. Beal Botanical Garden, M.S.U.1051823Ames 10170
52NA 56800NA 56800Lyonia mariana (L.) D. Don Texas, United StatesNANot Available1985COLLECTEDHardin County; Village Mills; Original propagation from the wild.2108361NA 56800
53NA 55839NA 55839Lyonia lucida (Lam.) K. Koch North Carolina, United StatesNANot Available1985COLLECTEDOrange County; ; Originally from: Orange Co. NC2108357NA 55839
54NA 45360NA 45360Lyonia ovalifolia (Wall.) Drude var. elliptica (Siebold & Zucc.) Hand.-Mazz. Kyushu, JapanNANot Available1978COLLECTED11/21/1978Seidagawa (river).Wild material1952374NA 45360