B052-0004
How are anthropogenic influences and climate change expressed by fossil flora and fauna in the last 3,000 years at High Point Cedar Bog, NJ?

Thursday, 10 December 2020
Poster
Sophia E BenJeddi, Barnard College, New York, NY, United States and Dorothy M Peteet, NASA Goddard Institute for Space Studies, New York, NY, United States
Abstract:
Ombrotrophic, high-elevation Chamaecyparis thyoides (Atlantic White Cedar) bogs are severely understudied ecosystems. Their invaluable economic importance in the form of highly durable, fire-retardant, aromatic wood, in addition to their roles in supporting critical wildlife habitats and native vegetation, bring urgency to this study, especially amidst a rapidly changing climate. We investigated Cedar Bog in High Point State Park, NJ, which lies at 457m above sea level, to further understand the implications and influences of natural climate change and anthropogenic impact through the upper 2.5 meters.This site was first studied by William A. Niering in 1953 who conducted a limited pollen analysis of the region and again in 2015 by Bühler and Peteet, who utilized macrofossil analysis and existing pollen records to reconstruct paleoenvironmental history of the lower 4m section of a 6.5m, 13,000yr record. A Dachnowski core was used in 2017 to extract the upper 2.5m of the bog. After sieving 0-20cm at the 4-cm interval, every fifth sample was sieved and macrofossils were picked for analysis. Bryophyte identifications were also performed to estimate moisture and pH. Our preliminary results demonstrate significant shifts in flora and fauna communities through time. At 88cm the site is predominantly composed of charcoal, charred Picea mariana needles, and Carex seeds, while Cenoccocum geophilum sclerotia and root matrices are the main constituents at 68cm depth. Furthermore, 48cm also includes Carex, while 28cm includes high amounts of C. thyoides bracts, Oribatid mites, some Sphagnum, and higher levels of P. mariana needles than C. thyoides needles. Surface centimeters are 85% Sphagnum. These results inform our hypothesis that Cedar Bog transitioned from a drier climate to a wetter, contemporary environment dominated by Sphagnum recurvum and Sphagnum centrale with elevated precipitation levels that concurrently place ecological stress upon C. thyoides stands.