Joint 52nd Northeastern Annual Section / 51st North-Central Annual Section Meeting - 2017

Paper No. 69-16
Presentation Time: 1:30 PM-5:30 PM

PREHISTORIC HUMAN CULTURAL SHIFTS IN THE MID-ATLANTIC: EVIDENCE OF CLIMATE INFLUENCE ON ARCHAIC CULTURES IN NEW JERSEY INFRERRED FROM A 15,000-YEAR LAKE SEDIMENT CORE


BROWN, Christopher R.1, GRIFFITHS, Michael L.1, HANSEN, Kyle G.1, GETCH, Seth J.1, GILLIKIN, David P.2, BRACHFELD, Sefanie A.3, DASILVA, Michael1, PARDI, Richard1 and SEBETICH, Michael1, (1)Department of Environmental Science, William Paterson University of New Jersey, 300 Pompton Road, Wayne, NJ 07470, (2)Department of Geology, Union College, 807 Union St, Schenectady, NY 12308, (3)Department of Earth & Environmental Studies, Montclair State University, Montclair, NJ 07043, brownc59@student.wpunj.edu

We present a local lacustrine record from Lake Blauvelt (LB), Franklin Lakes, New Jersey, which records past regional climate variability since ~15,000 years before present (kyr). Several paleoclimate proxies of regional lake recharge, weathering, and vegetation activity were extracted from the core at 3-4 cm increments (~50-100-year temporal resolution) and include analyses of sediment grain size, organic carbon and nitrogen content, nitrogen and carbon isotopes, and paleomagnetism. These proxies reveal similar patterns of variability throughout the record, whereby periods of larger-grained sediment input into the lake were synchronous with higher organic carbon and nitrogen fluxes (and vice versa), indicating both proxies likely reflect changes in lake recharge and weathering rates. These patterns are validated by similar Holocene patterns in C/N, magnetic susceptibility, and sedimentation rates. Together, the data indicate the Younger Dryas epoch (~12.8-11.5 kyr) was characterized by generally dry conditions, which culminated with a rapid transition to increased lake recharge during the early Holocene (~10 kyr). Superimposed upon a general increasing trend in LB lake levels throughout the Holocene is a major step-change at ~4.5-5 kyr, signifying an abrupt transition to higher lake levels that is matched by increased storm frequency in New England and declining regional air temperatures. These patterns are coeval with an abrupt increase in temperatures in the Pacific Northwest and tropical Eastern Pacific, indicating a strong role for the Pacific Decadal Oscillation (PDO) in this shift.

This proxy data when combined and analyzed serves as a context for the study of human culture in the local area from the Paleo-Indian Period to the Late Woodland Period, detailed within. Rather than using only publicly available C14 dates, our study hopes to bring greater light to “gray literature” and collections, at least in northern NJ. The addition of new archaeological data from the region may help in creating a centralized database or foundation for research of settlement patterns as well as the establishment of trade networks and technological shifts in northern New Jersey.