noaa-lake-22586 Abbott Lake, California 1,400 Year Sediment Physical Properties Data Hiner, C.A.; Kirby, M.E.; Bonuso, N.; Patterson, W.P.; Palermo, J.; Silveira, E. Abbott Lake, California 1,400 Year Sediment Physical Properties Data 2017-08-25 NCDC-Paleoclimatology ONLINE Files Pending https://www.ncdc.noaa.gov/paleo/study/22586 Investigator C.A. Hiner Investigator M.E. Kirby Investigator N. Bonuso Investigator W.P. Patterson Investigator J. Palermo Investigator E. Silveira earth science paleoclimate paleolimnology grain size class,sediment,null,percent,null,paleolimnology,null,laser particle size analysis,N,Result 62.50um-124.99um earth science paleoclimate paleolimnology grain size class,sediment,null,percent,null,paleolimnology,null,laser particle size analysis,N,Result 125.00um-249.99um earth science paleoclimate paleolimnology delta 18O,gastropod,null,per mil VPDB,null,paleolimnology,null,isotope ratio mass spectrometry,N,null earth science paleoclimate paleolimnology carbon,sediment,null,percent,null,paleolimnology,null,loss on ignition,N,loss on ignition at 950C earth science paleoclimate paleolimnology grain size class,sediment,null,percent,null,paleolimnology,null,laser particle size analysis,N,Result 3.90um-7.79um earth science paleoclimate paleolimnology grain size class,sediment,null,percent,null,paleolimnology,null,laser particle size analysis,N,Result 500.00um-1000.00um earth science paleoclimate paleolimnology clay,sediment,null,percent,null,paleolimnology,null,laser particle size analysis,N,null earth science paleoclimate paleolimnology grain size class,sediment,null,micrometer,null,paleolimnology,null,laser particle size analysis,N,10% of particles smaller than given particle diameter earth science paleoclimate paleolimnology depth,null,null,centimeter,null,paleolimnology,null,null,N,null earth science paleoclimate paleolimnology grain size class,sediment,null,percent,null,paleolimnology,null,laser particle size analysis,N,Result 31.00um-62.49um earth science paleoclimate paleolimnology grain size class,sediment,null,percent,null,paleolimnology,null,laser particle size analysis,N,Result 250.00um-499.99um earth science paleoclimate paleolimnology grain size class,sediment,null,percent,null,paleolimnology,null,laser particle size analysis,N,Result 1000.01um-2000.00um earth science paleoclimate paleolimnology sand,sediment,null,percent,null,paleolimnology,null,laser particle size analysis,N,null earth science paleoclimate paleolimnology sand,sediment,null,standard deviation unit,null,paleolimnology,normalized,laser particle size analysis,N,null earth science paleoclimate paleolimnology grain size class,sediment,null,micrometer,null,paleolimnology,null,laser particle size analysis,N,90% of particles smaller than given particle diameter earth science paleoclimate paleolimnology grain size class,sediment,null,percent,null,paleolimnology,null,laser particle size analysis,N,Result 7.80um-15.59um earth science paleoclimate paleolimnology grain size class,sediment,null,percent,null,paleolimnology,null,laser particle size analysis,N,Result 15.60um-30.99um earth science paleoclimate paleolimnology grain size mode,sediment,null,micrometer,null,paleolimnology,null,laser particle size analysis,N,null earth science paleoclimate paleolimnology mass magnetic susceptibility,sediment,null,cubic meter per kilogram,null,paleolimnology,null,magnetic susceptibility measurement,N,units are 10^-7 cubic meter per kilogram earth science paleoclimate paleolimnology grain size class,sediment,null,micrometer,null,paleolimnology,null,laser particle size analysis,N,50% of particles smaller than given particle diameter earth science paleoclimate paleolimnology silt,sediment,null,percent,null,paleolimnology,null,laser particle size analysis,N,null earth science paleoclimate paleolimnology organic matter,sediment,null,percent,null,paleolimnology,null,loss on ignition,N,loss on ignition at 550C earth science paleoclimate paleolimnology grain size class,sediment,null,percent,null,paleolimnology,null,laser particle size analysis,N,Result 0.02um-3.89um earth science paleoclimate paleolimnology age,null,null,calendar year before present,null,paleolimnology,null,null,N,null earth science paleoclimate paleolimnology oxygen isotopes earth science paleoclimate paleolimnology physical properties geoscientificInformation 1392 cal yr BP -61 cal yr BP Complete 36.231017 36.231017 -121.4824 -121.4824 260 260 Continent North America United States Of America California Abbott Lake>LATITUDE 36.231017>LONGITUDE -121.4824 None Please cite original publication, online resource, dataset and publication DOIs (where available), and date accessed when using downloaded data. If there is no publication information, please cite investigator, title, online resource, and date accessed. The appearance of external links associated with a dataset does not constitute endorsement by the Department of Commerce/National Oceanic and Atmospheric Administration of external Web sites or the information, products or services contained therein. For other than authorized activities, the Department of Commerce/NOAA does not exercise any editorial control over the information you may find at these locations. These links are provided consistent with the stated purpose of this Department of Commerce/NOAA Web site. English DOC/NOAA/NESDIS/NCEI National Centers for Environmental Information, NESDIS, NOAA, U.S. Department of Commerce https://www.ncdc.noaa.gov/data-access/paleoclimatology-data DATA Center Contact Bruce Bauer bruce.a.bauer@noaa.gov paleo@noaa.gov 303-497-6280 303-497-6513

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Boulder CO 80305-3328 USA online ASCII Christine A. Hiner, Matthew E. Kirby, Nicole Bonuso, William P. Patterson, Jennifer Palermo, Emily Silveira 2016 Journal of Paleolimnology 56 4 299-313 10.1007/s10933-016-9912-4 https://link.springer.com/article/10.1007%2Fs10933-016-9912-4

Abbott Lake (Monterey County, California) is one of only a few natural, permanent lakes located in coastal central California. As a result, it represents an important site for assessing spatiotemporal patterns of past hydroclimatic variability. Combined sedimentologic and isotopic analyses are used to describe 1400 years of hydrologic variability within the lake and its drainage basin. Specifically, changes in sand content, percent total organic matter, and d18O(G. parvus) values suggest changes in paleo-runoff, depositional environment, and relative d18O(lake water) values, respectively. Nine AMS 14C dates on discrete organic material provide age control with a basal age estimate of ~2400 cal years BP. However, we focus on the most recent 1400 years where the age model is most robust. The results indicate that coastal central California was relatively dry (less runoff) during the Medieval Climatic Anomaly (MCA) and variably wet (more runoff) during the Little Ice Age (LIA). These results are compared to Zaca Lake (Kirby et al. 2014) and Lake Elsinore (Kirby et al. 2010), both located south of Abbott Lake, and to flood event layers from Santa Barbara Basin (Hendy et al. 2013). All three sites, including SBB's flood event history, indicate a variably wet LIA and dry MCA; however, the absolute timing of wet and dry episodes is more congruent between Zaca and Elsinore than to Abbott Lake suggesting real spatiotemporal variability along the southern to central California coast. Finally, Abbott Lake is compared to Pacific Decadal Oscillation and Pacific sea surface temperature reconstructions. These comparisons suggest a Pacific-sourced control on late Holocene hydroclimates along coastal central California. STUDY NOTES: Physical properties (magnetic susceptibility, grain size, and loss-on-ignition) data, plus gastropod d18O, from sediment core AL13PC-1 collected in Abbott Lake, California, for the past 1,400 years.

GET DATA https://www1.ncdc.noaa.gov/pub/data/paleo/paleolimnology/northamerica/usa/california/abbott2016.txt Formatted Text Data File; Abbott Lake Sediment Physical Properties Data USA/NOAA DIF Version 9.8.4 2019-06-03 2019-06-03