The stratigraphic record of recent climate change in mid-Atlantic USA
- Johns Hopkins Univ., Baltimore, MD (United States)
The Medieval Warm Period and Little Ice Age recorded in sediments deposited in tributaries and marshes surrounding the Chesapeake and Delaware Bays in the mid-Atlantic region of USA, by changes in pollen and seeds of terrestrial and aquatic plants, and changes in influxes of charcoal, sediment, metals and nutrients. Fossil pollen and seeds portray a regional landscape characterized by conditions drier that present from about 1000 to 1200 AD. During the same period, high charcoal and sediment influxes indicate high fire frequency. This short dry interval was followed by an expansion of submerged aquatic plants, low marsh plants, and terrestrial plants that occupy wet habitats. Charcoal influxes are extremely low during the latter interval, which extended from about 1200 AD to 1500 AD. Plant macrofossil and pollen distributions indicate a second dry period extending from 1550 to 1650 AD, which appears similar to the earlier Medieval Warm interval.
- OSTI ID:
- 7164146
- Report Number(s):
- CONF-940894-; CODEN: BECLAG
- Journal Information:
- Bulletin of the Ecological Society of America; (United States), Vol. 75:2; Conference: Annual Ecological Society of America (ESA) meeting: science and public policy, Knoxville, TN (United States), 7-11 Aug 1994; ISSN 0012-9623
- Country of Publication:
- United States
- Language:
- English
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63 RADIATION, THERMAL, AND OTHER ENVIRON. POLLUTANT EFFECTS ON LIVING ORGS. AND BIOL. MAT.
AQUATIC ECOSYSTEMS
POPULATION DYNAMICS
CHESAPEAKE BAY
SEDIMENTS
TERRESTRIAL ECOSYSTEMS
USA
PALEOCLIMATOLOGY
ATLANTIC OCEAN
BAYS
COASTAL WATERS
DEVELOPED COUNTRIES
ECOSYSTEMS
NORTH AMERICA
PALEONTOLOGY
SEAS
SURFACE WATERS
540110*
560400 - Other Environmental Pollutant Effects