Barash, Max S; Lavrov, Vadim M (1977): (Table 1) Thickness of the Holocene layer and sedimentation rates in the Atlantic Ocean [dataset]. P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow, PANGAEA, https://doi.org/10.1594/PANGAEA.754862, Supplement to: Barash, MS; Lavrov, VM (1977): On the thickness of the Holocene sediments within the bottom deposits of the Atlantic Ocean. Oceanology, 17(2), 172-176
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Abstract:
On the basis of planktonic foraminifera study, thickness of Holocene sediments has been ascertained in 60 sediment cores from various regions of the Atlantic Ocean. Ratios of species reflect warming of the upper water layer at the Pleistocene-Holocene boundary over the entire ocean. The Holocene boundary can be determined not only from microfaunal data, but also from lithologic ones including textural and structural features. Increase in CaCO3 contents in Holocene sediments as compared to Pleistocene is from 5-7% to 60-70% in different parts of the ocean.
Project(s):
Archive of Ocean Data (ARCOD)
Coverage:
Median Latitude: 29.919000 * Median Longitude: -27.021583 * South-bound Latitude: -35.278333 * West-bound Longitude: -78.310000 * North-bound Latitude: 63.946667 * East-bound Longitude: 7.896667
Minimum Elevation: -5260.0 m * Maximum Elevation: -670.0 m
Event(s):
AK1-K-39GC * Latitude: -4.990000 * Longitude: 1.966667 * Elevation: -5260.0 m * Location: Atlantic Ocean * Campaign: AKU1 * Basis: Akademik Kurchatov * Method/Device: Gravity corer (GC)
AK3-K-121GC * Latitude: -13.970000 * Longitude: -4.125000 * Elevation: -4695.0 m * Location: Atlantic Ocean * Campaign: AKU3 * Basis: Akademik Kurchatov * Method/Device: Gravity corer (GC)
AK3-K-176GC * Latitude: -19.866667 * Longitude: 7.896667 * Elevation: -4900.0 m * Location: Atlantic Ocean * Campaign: AKU3 * Basis: Akademik Kurchatov * Method/Device: Gravity corer (GC)
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | ||||
| 2 | Latitude of event | Latitude | ||||
| 3 | Longitude of event | Longitude | ||||
| 4 | Elevation of event | Elevation | m | |||
| 5 | Thickness | Thick | mm | Barash, Max S | Counting, foraminifera, planktic | of Holocene |
| 6 | Sedimentation rate | SR | cm/ka | Barash, Max S | Calculated |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
120 data points
Data
| 1 Event | 2 Latitude | 3 Longitude | 4 Elevation [m] | 5 Thick [mm] | 6 SR [cm/ka] |
|---|---|---|---|---|---|
| ML1_19GC | 62.3850 | -13.3917 | -1380 | 0 | 0.0 |
| ML1_26GC | 62.1167 | -20.4133 | -1640 | 660 | 6.0 |
| ML1_36GC | 58.6583 | -14.5650 | -1080 | 130 | 1.2 |
| ML1_61GC | 45.9283 | -14.2833 | -4910 | 930 | 8.5 |
| ML1_66GC | 49.0600 | -20.3067 | -4000 | 120 | 1.1 |
| ML2_80GC | 53.9250 | -34.5733 | -2240 | 400 | 3.6 |
| ML2_86GC | 49.3383 | -28.6250 | -3260 | 220 | 2.0 |
| ML2_89GC | 47.0000 | -26.0500 | -2960 | 250 | 2.3 |
| ML2_91GC | 45.4333 | -24.2533 | -2880 | 260 | 2.4 |
| ML2_141GC | 39.5167 | -46.0117 | -4280 | 120 | 1.1 |
| ML2_153GC | 50.0317 | -49.1833 | -1410 | 140 | 1.3 |
| ML2_183GC | 59.5067 | -28.5000 | -1806 | 250 | 2.3 |
| ML3_187GC | 56.6450 | -25.8783 | -2950 | 210 | 1.9 |
| ML3_189GC | 55.4067 | -23.4333 | -2300 | 240 | 2.2 |
| ML3_191GC | 54.2067 | -21.0367 | -3040 | 460 | 4.1 |
| ML3_198-4GC | 55.7083 | -18.9017 | -1265 | 570 | 5.2 |
| ML3_215GC | 46.8683 | -7.7500 | -4600 | 330 | 3.0 |
| ML4_231GC | 51.7217 | -24.4717 | -3670 | 650 | 5.9 |
| ML4_233GC | 52.9933 | -27.2717 | -3828 | 1050 | 9.6 |
| ML4_238GC | 55.9983 | -33.9667 | -2002 | 340 | 3.1 |
| ML4_246GC | 50.1117 | -29.7133 | -3149 | 210 | 1.9 |
| ML4_254GC | 43.7883 | -22.6000 | -3950 | 320 | 2.9 |
| ML4_257GC | 41.4750 | -21.3867 | -3500 | 310 | 2.8 |
| ML4_276GC | 51.1317 | -38.0000 | -3755 | 250 | 2.3 |
| ML5_348GC | 63.9467 | -30.0333 | -2262 | 290 | 2.6 |
| ML5_352GC | 56.4700 | -30.1317 | -2836 | 450 | 4.1 |
| ML5_356GC | 48.0167 | -29.9167 | -3558 | 210 | 1.9 |
| ML5_358GC | 44.0417 | -30.0550 | -2861 | 350 | 3.2 |
| ML5_390GC | -22.8850 | -39.7500 | -2745 | 880 | 8.0 |
| ML6_425GC | 40.8250 | -65.9700 | -2886 | 150 | 1.4 |
| ML6_427GC | 40.9000 | -63.2550 | -4231 | 360 | 3.3 |
| ML6_447GC | 37.4683 | -70.3700 | -4074 | 630 | 5.7 |
| ML6_483GC | 17.2667 | -34.0717 | -4833 | 20 | 0.2 |
| ML7_523GC | 36.4083 | -40.8333 | -4116 | 130 | 1.2 |
| ML7_540GC | 31.9633 | -78.3100 | -670 | 0 | 0.0 |
| ML10_827GC | -0.0667 | -10.7900 | -4126 | 250 | 2.3 |
| ML10_860GC | -9.0833 | -18.6100 | -4074 | 620 | 5.6 |
| ML10_878GC | -28.4333 | -33.3833 | -3823 | 130 | 1.2 |
| ML10_885GC | 24.0333 | -41.8833 | -1502 | 170 | 1.5 |
| ML10_909GC | 8.6183 | -30.2133 | -4461 | 140 | 1.3 |
| ML12_1033GC | 1.0933 | -30.0667 | -2450 | 220 | 2.0 |
| ML12_1045GC | -8.6517 | -34.4383 | -1250 | 190 | 1.7 |
| ML12_1056GC | -12.7367 | -36.0050 | -3860 | 120 | 1.1 |
| ML13_1101-3GC | -0.2167 | -20.3500 | -4480 | 380 | 3.4 |
| AK1-K-39GC | -4.9900 | 1.9667 | -5260 | 250 | 2.3 |
| AK3-K-121GC | -13.9700 | -4.1250 | -4695 | 300 | 2.7 |
| AK3-K-176GC | -19.8667 | 7.8967 | -4900 | 350 | 3.2 |
| AK3-K-178GC | -19.9967 | 5.9300 | -4490 | 200 | 1.8 |
| AK3-K-200GC | -22.9233 | 7.0750 | -2410 | 250 | 2.3 |
| AK3-K-212GC | -21.3583 | 7.3333 | -3100 | 200 | 1.8 |
| AK6-K-432GC | 40.5233 | -29.4700 | -3350 | 500 | 4.6 |
| AK6-K-434GC | 19.2333 | -26.2167 | -4620 | 250 | 2.3 |
| AK10-K-838GC | -35.2783 | -26.5583 | -4100 | 170 | 1.5 |
| DM1-M-2GC | 35.5333 | -29.5833 | -3570 | 200 | 1.8 |
| S218GC | 6.1933 | -25.3250 | -4300 | 70 | 0.7 |
| S227GC | 9.9350 | -45.0650 | -4830 | 180 | 1.6 |
| S243GC | 41.7333 | -24.3733 | -3950 | 200 | 1.8 |
| E-156GC | 58.8333 | -15.3250 | -1120 | 350 | 3.2 |
| E-159GC | 55.6383 | -13.8000 | -2700 | 750 | 6.8 |
| E-170GC | 57.9667 | -28.6517 | -2420 | 290 | 2.6 |