A radiocarbon chronology of Holocene climate change and sea-level rise at the Delmarva Peninsula, US Mid-Atlantic Coast

被引:5
作者
Ramsey, Kelvin W. [1 ]
Tomlinson, Jaime L. [1 ]
Mattheus, C. Robin [2 ]
机构
[1] Univ Delaware, Delaware Geol Survey, 257 Acad St, Newark, DE 19711 USA
[2] Univ Illinois, Prairie Res Inst, Illinois State Geol Survey, Champaign, IL USA
关键词
climate; Delmarva Peninsula; Holocene; radiocarbon; sea-level rise; CHESAPEAKE BAY; DELAWARE BAY; CONTINENTAL-SHELF; EASTERN SHORE; RIVER VALLEY; HISTORY; EVOLUTION; ESTUARY; RECORD; ACCUMULATION;
D O I
10.1177/09596836211048282
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Radiocarbon dates from 176 sites along the Delmarva Peninsula record the timing of deposition and sea-level rise, and non-marine wetland deposition. The dates provide confirmation of the boundaries of the Holocene subepochs (e.g. "early-middle-late" of Walker et al.) in the mid-Atlantic of eastern North America. These data record initial sea-level rise in the early Holocene, followed by a high rate of rise at the transition to the middle Holocene at 8.2 ka, and a leveling off and decrease in the late-Holocene. The dates, coupled to local and regional climate (pollen) records and fluvial activity, allow regional subdivision of the Holocene into six depositional and climate phases. Phase A (>10 ka) is the end of periglacial activity and transition of cold/cool climate to a warmer early Holocene. Phase B (10.2-8.2 ka) records rise of sea level in the region, a transition to Pinus-dominated forest, and decreased non-marine deposition on the uplands. Phase C (8.2-5.6 ka) shows rapid rates of sea-level rise, expansion of estuaries, and a decrease in non-marine deposition with cool and dry climate. Phase D (5.6-4.2 ka) is a time of high rates of sea-level rise, expanding estuaries, and dry and cool climate; the Atlantic shoreline transgressed rapidly and there was little to no deposition on the uplands. Phase E (4.2-1.1 ka) is a time of lowering sea-level rise rates, Atlantic shorelines nearing their present position, and marine shoal deposition; widespread non-marine deposition resumed with a wetter and warmer climate. Phase F (1.1 ka-present) incorporates the Medieval Climate Anomaly and European settlement on the Delmarva Peninsula. Chronology of depositional phases and coastal changes related to sea-level rise is useful for archeological studies of human occupation in relation to climate change in eastern North America, and provides an important dataset for future regional and global sea-level reconstructions.
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页码:3 / 16
页数:14
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