Frank E. Kurczewski, Hugh F. Boyle
Northeastern Naturalist 7 (2), 95-112, (1 June 2000) https://doi.org/10.1656/1092-6194(2000)007[0095:HCITPB]2.0.CO;2
Soils, vegetation, fossil pollen and charcoal, disturbance history, early documents and maps, and insects were used to interpret past changes in the central Suffolk County, Long Island, New York pine barrens. Before Euro-American settlement pitch pine-oak-heath woodland, pitch pine-scrub oak barrens, and dwarf pine plains probably covered portions of the broad outwash plain south of the Ronkonkoma Moraine. These communities would have occurred on deep, coarse-textured, excessively drained, nutrient-impoverished, acidic, fire-prone sandy soils. Logging, land clearance, and repeated human-caused fires promoted the expansion of barrens vegetation through much of central Suffolk County during the 17th–19th centuries. Pitch pine became established on the disturbed loamy, sandy, and gravelly soils. Scrub oak sprouted profusely on these soils in response to repeated burning of the undergrowth. The seed for this expansion dispersed from trees and shrubs growing in adjacent oak-pitch pine and pitch pine-oak woodlands. With 20th century fire suppression, pine barrens reverted to oak-hardwood forests in northcentral Suffolk County and oak-pine and pine-oak forests in southcentral Suffolk County. Pine barrens persisted in sections of eastcentral and southcentral Suffolk County in response to periodic burning.