(Lamb. ex D. Don) Endl.
Identity
Unique IDELEMENT_GLOBAL.2.140518
Element CodePGTXO02010
Record TypeSPECIES
ClassificationSpecies
Classification StatusStandard
Name CategoryVascular Plant
IUCNEndangered
Endemicendemic to a single nation
KingdomPlantae
PhylumConiferophyta
ClassPinopsida
OrderPinales
FamilyCupressaceae
GenusSequoia
Other Common Namesredwood (EN)
Concept ReferenceKartesz, J.T. 1994. A synonymized checklist of the vascular flora of the United States, Canada, and Greenland. 2nd edition. 2 vols. Timber Press, Portland, OR.
Conservation Status
Rank MethodLegacy Rank calculation - Excel v3.1x
Review Date2020-04-30
Change Date1996-11-21
Edition Date2020-04-30
Edition AuthorsMorse, Larry E. (1996); rev. R. Bittman (2013), rev. Treher (2020)
Threat ImpactLow
Range Extent20,000-200,000 square km (about 8000-80,000 square miles)
Number of Occurrences81 - 300
Rank ReasonsSequoia sempervirens occurs on the pacific slope from southwestern Oregon to Monterey County, California. It is abundant, even dominant, in a substantial but not large geographic range. Mature trees in areas not protected as conservation lands are subject to substantial demand for timber. A large portion of the species range is on protected lands.
Range Extent CommentsSequoia sempervirens occurs on the pacific slope of the northern half of the Coast Range of California (from Monterey Co. northward), and adjacent southwestern-most Oregon. It is generally found within 5-35 miles of the ocean, and apparently dependent on coastal humidity and fog (Griffith 1992).
Occurrences CommentsThe species is frequent within its geographic range, which extends from southwestern Oregon to Monterey County, California.
Threat Impact CommentsDemand for timber on remaining private forest lands remains strong, with the wood having unique properties that make substitution difficult. Climate change is changing the environment of the north coast to be less foggy, and perhaps more prone to catastrophic fires. However, there is some evidence that there is increased tree growth (from core studies) in the past few decades, due to increased precipitation, which is also attributed to climate change.