Barron, John A; Metcalf, Sarah E; Addison, Jason A (2012): (Table S1) Opal content of sediment core OXMZ01MV-GC31 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.824830, Supplement to: Barron, JA et al. (2012): Response of the North American monsoon to regional changes in ocean surface temperature. Paleoceanography, 27(3), PA3206, https://doi.org/10.1029/2011PA002235
Always quote citation above when using data! You can download the citation in several formats below.
Abstract:
The North American monsoon (NAM), an onshore wind shift occurring between July and September, has evolved in character during the Holocene largely due to changes in Northern Hemisphere insolation. Published paleoproxy and modeling studies suggest that prior to ~8000 cal years BP, the NAM affected a broader region than today, extending westward into the Mojave Desert of California. Holocene proxy SST records from the Gulf of California (GoC) and the adjacent Pacific provide constraints for this changing NAM climatology. Prior to ~8000 cal years BP, lower GoC SSTs would not have fueled northward surges of tropical moisture up the GoC, which presently contribute most of the monsoon precipitation to the western NAM region. During the early Holocene, the North Pacific High was further north and SSTs in the California Current off Baja California were warmer, allowing monsoonal moisture flow from the subtropical Pacific to take a more direct, northwesterly trajectory into an expanded area of the southwestern U.S. west of 114°W. A new upwelling record off southwest Baja California reveals that enhanced upwelling in the California Current beginning at ~7500 cal year BP may have triggered a change in NAM climatology, focusing the geographic expression of NAM in the southwest USA into its modern core region east of ~114°W, in Arizona and New Mexico. Holocene proxy precipitation records from the southwestern U.S. and northwestern Mexico, including lakes, vegetation/pollen, and caves are reviewed and found to be largely supportive of this hypothesis of changing Holocene NAM climatology.
Further details:
van Geen, Alexander; Zheng, Y; Bernhard, Joan M; Cannariato, Kevin G; Carriquiry, José D; Dean, Walter E; Eakins, Barry W; Ortiz, Joseph D; Pike, Jennifer (2003): On the preservation of laminated sediments along the western margin of North America. Paleoceanography, 18(4), 1098, https://doi.org/10.1029/2003PA000911
Coverage:
Latitude: 23.467170 * Longitude: -111.598500
Date/Time Start: 1999-11-11T00:00:00 * Date/Time End: 1999-11-11T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 3.77 m
Event(s):
OXMZ01MV-GC31 * Latitude: 23.467170 * Longitude: -111.598500 * Date/Time: 1999-11-11T00:00:00 * Elevation: -705.0 m * Campaign: OXMZ01MV * Basis: Melville * Method/Device: Gravity corer (GC)
Comment:
Age scale from Van Geen et al. (2003).
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Depth, composite | Depth comp | mcd | Barron, John A | Intercore correlation | shifted down 25 cm to align with associated multicore (Van Geen et al., 2003) |
| 3 | AGE | Age | ka BP | Geocode | ||
| 4 | Opal, biogenic silica | bSiO2 | % | Barron, John A |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
140 data points
Data
| 1 Depth sed [m] | 2 Depth comp [mcd] | 3 Age [ka BP] | 4 bSiO2 [%] |
|---|---|---|---|
| 0.00 | 0.25 | 0.824 | 10.76 |
| 0.05 | 0.30 | 0.992 | 8.97 |
| 0.10 | 0.35 | 1.126 | 13.32 |
| 0.15 | 0.40 | 1.294 | 10.59 |
| 0.25 | 0.50 | 1.631 | 8.26 |
| 0.30 | 0.55 | 1.799 | 8.93 |
| 0.35 | 0.60 | 1.967 | 8.81 |
| 0.40 | 0.65 | 2.135 | 7.68 |
| 0.45 | 0.70 | 2.303 | 8.96 |
| 0.50 | 0.75 | 2.471 | 9.25 |
| 0.55 | 0.80 | 2.639 | 5.43 |
| 0.60 | 0.85 | 2.807 | 7.08 |
| 0.65 | 0.90 | 2.975 | 8.68 |
| 0.70 | 0.95 | 3.144 | 14.73 |
| 0.75 | 1.00 | 3.312 | 8.10 |
| 0.80 | 1.05 | 3.480 | 7.47 |
| 0.85 | 1.10 | 3.648 | 7.45 |
| 0.90 | 1.15 | 3.816 | 7.98 |
| 0.95 | 1.20 | 3.984 | 7.82 |
| 1.00 | 1.25 | 4.152 | 8.04 |
| 1.05 | 1.30 | 4.320 | 6.37 |
| 1.10 | 1.35 | 4.488 | 8.13 |
| 1.15 | 1.40 | 4.657 | 6.40 |
| 1.20 | 1.45 | 4.825 | 5.79 |
| 1.25 | 1.50 | 4.993 | 6.09 |
| 1.30 | 1.55 | 5.161 | 5.99 |
| 1.35 | 1.60 | 5.329 | 9.08 |
| 1.40 | 1.65 | 5.497 | 5.84 |
| 1.45 | 1.70 | 5.665 | 7.00 |
| 1.50 | 1.75 | 5.833 | 6.51 |
| 1.51 | 1.76 | 5.867 | 7.98 |
| 1.55 | 1.80 | 6.001 | 6.52 |
| 1.60 | 1.85 | 6.169 | 6.47 |
| 1.65 | 1.90 | 6.338 | 6.97 |
| 1.75 | 2.00 | 6.674 | 6.58 |
| 1.80 | 2.05 | 6.842 | 7.21 |
| 1.85 | 2.10 | 7.010 | 7.34 |
| 1.90 | 2.15 | 7.178 | 6.72 |
| 2.00 | 2.25 | 7.514 | 6.17 |
| 2.10 | 2.35 | 7.851 | 4.55 |
| 2.15 | 2.40 | 8.019 | 5.01 |
| 2.25 | 2.50 | 8.355 | 4.75 |
| 2.30 | 2.55 | 8.523 | 4.63 |
| 2.35 | 2.60 | 8.691 | 4.67 |
| 2.40 | 2.65 | 8.859 | 4.51 |
| 2.45 | 2.70 | 9.027 | 4.72 |
| 2.50 | 2.75 | 9.195 | 2.59 |
| 2.55 | 2.80 | 9.363 | 5.33 |
| 2.60 | 2.85 | 9.532 | 5.22 |
| 2.65 | 2.90 | 9.700 | 5.51 |
| 2.75 | 3.00 | 10.036 | 6.38 |
| 2.80 | 3.05 | 10.204 | 5.96 |
| 2.85 | 3.10 | 10.372 | 7.77 |
| 2.90 | 3.15 | 10.540 | 5.93 |
| 2.97 | 3.22 | 10.641 | 7.11 |
| 3.02 | 3.27 | 10.944 | 7.21 |
| 3.07 | 3.32 | 11.112 | 7.21 |
| 3.12 | 3.37 | 11.280 | 6.22 |
| 3.17 | 3.42 | 11.448 | 7.54 |
| 3.22 | 3.47 | 11.616 | 5.69 |
| 3.27 | 3.52 | 11.784 | 4.41 |
| 3.32 | 3.57 | 11.952 | 4.00 |
| 3.37 | 3.62 | 12.120 | 4.94 |
| 3.42 | 3.67 | 12.288 | 2.54 |
| 3.47 | 3.72 | 12.457 | 4.61 |
| 3.57 | 3.82 | 12.793 | 4.20 |
| 3.62 | 3.87 | 12.961 | 1.38 |
| 3.67 | 3.92 | 13.129 | 3.97 |
| 3.72 | 3.97 | 13.297 | 3.14 |
| 3.77 | 4.02 | 13.465 | 4.53 |