R. R. Reynolds

Status
Established
Year Established
1943

Location

State
Arkansas
National Forest Regions
Southern Region (R8)
Forest at R. R. Reynolds Research Natural Area

The R.R. Reynolds RNA is a closed-canopy, mature loblolly pine-hardwood forest that has had little human intervention for 65 years. One of the most distinctive features of the RNA is its large trees. Some of the loblolly pines approach 40 inches (101 cm) in diameter at breast height (DBH) and are nearly 140 feet (43 m) tall. In the 1993 inventory, the largest diameter tree in the RNA was a white oak (Quercus alba) that measured 44 inches (112 cm) in diameter. Shelton and Cain (1999) reported that the oldest trees in the RNA approach 150 years for both pines and oaks. Such trees are living representatives of the virgin forest.

County: Ashley

Forest: Crossett Experimental Forest, Ouachita National Forest

View a searchable map for the R.R. Reynolds RNA.

SAF Cover Types (list acres):

  • Loblolly pine–hardwood–82
  • Loblolly pine–81
  • Loblolly–shortleaf pine–80

Kuchler Types (list acres):

  • Oak–hickory–pine, 51 ac (20.6 ha)
  • Oak–hickory–pine, 15 ac (6.1 ha)
  • Oak–hickory–pine, 14 ac (5.7 ha)

Ecological and Physical Description

Size
80ac (32ha)
Elevation Range
125' (38m) - 134' (41m)
Temperature Range
52°F (11°C) - 76°F (24°C)
Primary Features

Closed canopy mature loblolly pine hardwood forest that has had little human interventIon. Area established to provide baseline contrast to typical managed cutover stand. Entirely within Crossett Experimental Forest.

Annual Precipitation

55.49 in, (140.9 ha)

Nearest Weather Station

A weather station is maintained at the Crossett Experimental Forest headquarters located 1.0 mile (1.7 km) to the west of the RNA.

Geology and Soils

The RNA is located in the West Gulf Coastal Plain, with elevations ranging from 125 to 134 feet (38 to 41 m) above sea level. Typical sedimentary deposits consist of unconsolidated clay, sand, and gravel of Quaternary age. Along broad upland flats, there is a significant deposit of loess of up to a foot (25 cm) thick that was deposited during the Quaternary. The youngest rocks that underlie the RNA belong to the Claiborne Group, which is of Tertiary age. The Claiborne Group is chiefly non-marine in origin, but does contain some marine intervals (Howard et al. 1997). The Claiborne Group, which may be up to 1,500 feet (457 m) thick, has been subdivided into the Carrizo Sand, Cane River Formations, Sparta Sand, Cook Mountain Formation, and Cockfield Formation. Fossils include fish and reptile bones and teeth, leaf impressions, and trace fossils.

Aquatic Features

The area is dissected by several intermittent drainages.

Flora and Fauna

Common Plant Species

Common Animal Species

Last updated June 6, 2023