Calcareous Pavement Barrens |
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| Upland White Goldenrod (Oligoneuron album) in bloom in calcareous pavement barrens with at The Nature Conservancy's Chaumont Barrens |
Gregory J. Edinger |
System: Terrestrial
SubSystem: Barrens And Woodlands
State Protection:
Not Listed
Federal Protection:
Not Listed
State Rarity Rank:
S1
Global Rarity Rank:
G3
Did you know?
These calcareous pavement landforms originated from sedimentary deposits in a vast, shallow inland sea that covered much of New York approximately 450 million years ago. Many of these deposits are rich in fossils (Isachsen et. al 2000). Cracks in the pavement bedrock are called "grykes." They are formed when rain water dissolves the limestone producing solution fissures that often collect leaves and debris, so take care when walking in a calcareous pavent barrens and avoid stepping into the grykes.
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| State Ranking Justification |
[-] |
There are probably much less than 50 occurrences statewide. A few documented occurrences have good viability and several are protected on public land or private conservation land. This community is limited to the calcareous regions of the state, and there are only a few high quality examples. The current trend of this community is probably stable for occurrences on public land and private conservation land, or declining slightly elsewhere due to moderate threats that include conversion to pastureland, development, trampling by visitors, ATVs, and invasive species.
The number and acreage of calcareous pavement barrens in New York have probably declined slightly in recent decades as a result of development, conversion to pastureland, recreational ATVs, and invasive species.
The number and acreage of calcareous pavement barrens in New York have probably declined moderately to substantially from historical numbers likely correlated with past conversion to pastureland.
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