# Subtropical Northeast Pacific Geochemistry and Sediment Physical Property Data Covering the Last 14,000 years #----------------------------------------------------------------------- # World Data Service for Paleoclimatology, Boulder # and # NOAA Paleoclimatology Program #----------------------------------------------------------------------- # Template Version 3.0 # Encoding: UTF-8 # NOTE: Please cite original publication, online resource and date accessed when using this data. # If there is no publication information, please cite Investigator, title, online resource and date accessed. # # Description/Documentation lines begin with # # Data lines have no # # # Online_Resource: https://www.ncdc.noaa.gov/paleo/study/25850 # Description: NOAA Landing Page # Online_Resource: http://www1.ncdc.noaa.gov/pub/data/paleo/contributions_by_author/arellano-torres2018/arellano-torres2018.txt # Description: NOAA location of the template # # Data_Type: Paleoceanography # # Dataset_DOI: # # Parameter_Keywords: geochemistry, physical properties #--------------------------------------- # Contribution_Date # Date: 2018-12-19 #--------------------------------------- # File_Last_Modified_Date # Date: 2018-12-19 #--------------------------------------- # Title # Study_Name: Subtropical Northeast Pacific Geochemistry and Sediment Physical Property Data Covering the Last 14,000 years #--------------------------------------- # Investigators # Investigators: Arellano-Torres, E.; Alvarez-Covelli, C.; Kasper-Zubillaga, J.J.; Lozano-GarcÃa, M.S. #--------------------------------------- # Description_Notes_and_Keywords # Description: Baja California margin Oxygen-Minimum Zone Sediment Geochemical Data # Provided Keywords: biogenic proxies, dust particles, teleconnections, carbon export, sub-orbital scales, Holocene #--------------------------------------- # Publication # Authors: Arellano-Torres, E., C. Alvarez-Covelli, J.J. Kasper-Zubillaga, and M.S. Lozano-GarcÃa # Published_Date_or_Year: 2018 # Published_Title: A 14 ka record of dust input and phytoplankton regime changes in the subtropical NE Pacific: oceanic and terrestrial processes linked by teleconnections at sub-orbital scales. # Journal_Name: Paleoceanography and Paleoclimatology # Volume: accepted December 2018 # Edition: # Issue: # Pages: # Report_Number: # DOI: # Online_Resource: # Full_Citation: # Abstract: We study shifts in phytoplankton proxies linked to terrigenous inputs and teleconnections in a core from Soledad Basin, Gulf of Ulloa, NW Mexico spanning the end of the deglaciation and the Holocene. We used biogenic opal (% opal), organic carbon (% TOC) and inorganic carbon (% CaCO3) as proxies of productivity; and opal/TOC and CaCO3/TOC ratios as proxies of nutrient uptake and C-export by siliceous and carbonate organisms. We reconstructed terrestrial inputs and identified authigenic gypsum. Based on opal/TOC and CaCO3/TOC ratios, we found periodic changes of ~0.5, 1.1 – 1.8 ka-cycle in phytoplankton proxies exporting siliceous and carbonate skeletal debris to the sediments. An increase in carbonate organisms occurred during 14 – 8.7 ka, corresponding to reduced ENSO-like variability, in parallel to the northward displacement of the Intertropical Convergence Zone (ITCZ) and an overall negative phase of the Pacific Decadal Oscillation (PDO). An increase in siliceous organisms occurred between 6 – 3 ka, coincident with strong ENSO-like conditions, southern migration of ITCZ and less intense but more frequent positive PDO-hydrological variability. Grain size analyses show significant amounts of fine fraction (dust < 6.6 µm) present during the early- to mid-Holocene in agreement to extreme weather on land, with episodes of aeolian and fluvial transport to the sea. The ENSO-like variations influenced biological C-export producers on a scale of 1.1-1.8 ka, but PDO-related variability is uncertain. We suggest that Holocene drivers for phytoplankton successions are changes in insolation, ITCZ migration, California Current upwelling, nutrient inputs by advection and terrestrial sources. #--------------------------------------- # Publication # Authors: Marchitto, T.M.; Muscheler, R.; Ortiz, J.D.; Carriquiry, J.D.; van Geen, A. # Published_Date_or_Year: 2010 # Published_Title: Dynamical Response of the Tropical Pacific Ocean to Solar Forcing During the Early # Journal_Name: Science # Volume: 330 # Edition: # Issue: 6009 # Pages: 1378-1381 # Report_Number: # DOI: 10.1126/science.1194887 # Online_Resource: # Full_Citation: # Abstract: #--------------------------------------- # Publication # Authors: Dean, W.E., Zheng, Y., Ortiz, J D., and van Geen, A. # Published_Date_or_Year: 2006 # Published_Title: Sediment Cd and Mo accumulation in the oxygen-minimum zone off western Baja California linked to global climate over the past 52 kyr. # Journal_Name: Paleoceanography # Volume: 21 # Edition: # Issue: 4 # Pages: # Report_Number: # DOI: 10.1029/2005PA001239 # Online_Resource: # Full_Citation: # Abstract: #--------------------------------------- # Funding_Agency # Funding_Agency_Name: Universidad Nacional Autonoma de Mexico-PAPIIT # Grant: IA105517 #--------------------------------------- # Site_Information # Site_Name: MV99-GC41/PC14 # Location: Eastern Pacific Ocean # Country: # Northernmost_Latitude: 25.2 # Southernmost_Latitude: 25.2 # Easternmost_Longitude: -112.7 # Westernmost_Longitude: -112.7 # Elevation: -540 #--------------------------------------- # Data_Collection # Collection_Name: MV99-GC41/PC14 Arellano-Torres2018 # First_Year: 13620 # Last_Year: 503 # Time_Unit: cal yr BP # Core_Length: 15.22 # Notes: Age model of composite core as in Marchitto et al., 2010 #--------------------------------------- # Chronology_Information # Chronology: #--------------------------------------- # Variables # Data variables follow that are preceded by "##" in columns one and two. # Variables list, one per line, shortname-tab-longname components (9 components: what, material, error, units, seasonality, archive, detail, method, C or N for Character or Numeric data) ## core_ID notes,,,,,paleoceanography,,,N,Core name identification number - Composite Core MV99 GC41-PC14 ## core_depth depth,,,centimeter,,paleoceanography,,,N,Depth in core ## Age_2010 age,foraminifer,,calendar year before present,,paleoceanography,,,N,Age model by Marchito et al., 2010 ## %opal biogenic silica,dry sediment,variance,weight percent,,paleoceanography,raw,spectrophotometry,N,Mortlock, R. A., & Froelich, P. N. (1989). A Simple Method for the Rapid-Determination of Biogenic Opal in Pelagic Marine-Sediments. Deep-Sea Research Part a-Oceanographic Research Papers, 36(9), 1415-1426. ## %TC carbon,dry sediment,variance,weight percent,,paleoceanography,raw,elemental analysis,N,Interval between 149-966 cm in core MV99 PC14 was published by Dean et al., 2006 ## %TIC inorganic carbon,dry sediment,,weight percent,,paleoceanography,differenced,elemental analysis,N,Interval between 149-966 cm in core MV99 PC14 was published by Dean et al., 2007 ## %TOC organic carbon,dry sediment,variance,weight percent,,paleoceanography,raw,elemental analysis,N,Interval between 149-966 cm in core MV99 PC14 was published by Dean et al., 2008 ## %CaCO3 calcium carbonate,calcium carbonate,,weight percent,,paleoceanography,differenced,elemental analysis,N,Interval between 149-966 cm in core MV99 PC14 was published by Dean et al., 2009 ## %clay grain size ,sediment,variance,percent,,paleoceanography,raw,Laser Particle size analysis,N,Size fraction 0.06-4 microns ## %silt grain size 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