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Bolton, Clara T; Stoll, Heather M (2025): Records of coccolithophore calcification (coccolith length, thickness, and shape factor, estimated PIC:POC ratios) from three sites in the Atlantic Ocean over the past 29 million years compiled from literature [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.982715

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Published: 2025-07-04DOI registered: 2025-08-02

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Abstract:
This dataset contains the data plotted in Figure 6 (panels a to d) of the review paper Coccoliths as Recorders of Paleoceanography and Paleoclimate over the Past 66 Million Years by Bolton & Stoll (2025, AREPS; doi:10.1146/annurev-earth-040623-103211). It contains previously published, in some cases updated, data on coccolith on Noelaerhabdaceae coccolith length, thickness, and shape factor (ks) and estimated PIC:POC ratios. The data provide insights into coccolith morphological evolution and degree of calcification, of interest for paleoceanographic and micropaleontological research. Data come from ODP Sites 925 and 926 and IODP Site U1406 sediment cores, drilled in the Atlantic Ocean, and are based on light microscope analyses.
Keyword(s):
Carbon and oxygen stable isotopes; Cenozoic; Coccolithophores; Micropaleontology; morphology
Related to:
Bolton, Clara T; Stoll, Heather M (2024): Coccoliths as Recorders of Paleoceanography and Paleoclimate over the Past 66 Million Years. Annual Review of Earth and Planetary Sciences, https://doi.org/10.1146/annurev-earth-040623-103211
References:
Bolton, Clara T; Hernández-Sánchez, María T; Fuertes, Miguel-Ángel; González-Lemos, Saúl; Abrevaya, Lorena; Mendez-Vicente, Ana; Flores, José-Abel; Probert, Ian; Giosan, Liviu; Johnson, Joel; Stoll, Heather M (2016): Decrease in coccolithophore calcification and CO2 since the middle Miocene. Nature Communications, 7(1), 10284, https://doi.org/10.1038/ncomms10284
González-Lanchas, Alba; Hernández-Almeida, Iván; Flores, José Abel; Sierro, Francisco Javier; Guitián, José; Stoll, Heather M (2021): Carbon Isotopic Fractionation of Alkenones and Gephyrocapsa Coccoliths Over the Late Quaternary (Marine Isotope Stages 12–9) Glacial-Interglacial Cycles at the Western Tropical Atlantic. Paleoceanography and Paleoclimatology, 36(8), e2020PA004175, https://doi.org/10.1029/2020PA004175
Guitián, José; Fuertes, Miguel Ángel; Flores, José-Abel; Hernández-Almeida, Iván; Stoll, Heather M (2022): Variation in calcification of Reticulofenestra coccoliths over the Oligocene–Early Miocene. Biogeosciences, 19(20), 5007-5019, https://doi.org/10.5194/bg-19-5007-2022
Tanner, Thomas; Rae, James W B; Hernández-Almeida, Iván; Zhang, Hongrui; Jaggi, Madalina; Dumont, Matthew; Jurikova, Hana; Bernasconi, Stefano M; Stoll, Heather M (preprint): Multi-proxy estimates of sea surface temperature and CO2 in the western Atlantic during the Late Miocene. https://doi.org/10.22541/essoar.171535711.15687939/v1
Funding:
French National Research Agency (ANR), grant/award no. ANR-22-EDIR-0003-01
Swiss National Science Foundation (SNF), grant/award no. 200021_182070
Coverage:
Median Latitude: 16.091060 * Median Longitude: -46.015732 * South-bound Latitude: 3.719017 * West-bound Longitude: -51.649830 * North-bound Latitude: 40.349930 * East-bound Longitude: -42.908300
Date/Time Start: 1994-02-08T00:00:00 * Date/Time End: 1994-02-27T00:00:00
Minimum Elevation: -3813.8 m * Maximum Elevation: -3052.4 m
Event(s):
154-925  * Latitude: 4.204233 * Longitude: -43.489067 * Date/Time Start: 1994-02-08T00:00:00 * Date/Time End: 1994-02-14T00:00:00 * Elevation: -3052.4 m * Penetration: 2017 m * Recovery: 1607.6 m * Location: North Atlantic Ocean * Campaign: Leg154 * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE) * Comment: 184 cores; 1729.6 m cored; 0 m drilled; 92.9% recovery
154-926  * Latitude: 3.719017 * Longitude: -42.908300 * Date/Time Start: 1994-02-19T00:00:00 * Date/Time End: 1994-02-27T00:00:00 * Elevation: -3610.0 m * Penetration: 1331.1 m * Recovery: 1322.4 m * Location: North Atlantic Ocean * Campaign: Leg154 * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE) * Comment: 141 cores; 1330.6 m cored; 0 m drilled; 99.4% recovery
342-U1406  * Latitude: 40.349930 * Longitude: -51.649830 * Elevation: -3813.8 m * Campaign: Exp342 (Paleogene Newfoundland Sediment Drifts) * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL)
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
Event labelEventBolton, Clara T
Latitude of eventLatitudeBolton, Clara T
Longitude of eventLongitudeBolton, Clara T
Date/Time of eventDate/TimeBolton, Clara T
Elevation of eventElevationmBolton, Clara T
AgeAgeMaBolton, Clara TFrom literatureFrom original publication
AGEAgeka BPBolton, Clara TFrom literatureGeocode
Particulate inorganic carbon/particulate organic carbon ratioPIC/POCBolton, Clara TFrom literatureMean
Particulate inorganic carbon/particulate organic carbon ratio, standard deviationPIC/POC ratio std dev±Bolton, Clara TFrom literature
10 Coccoliths, lengthCocco lµmBolton, Clara TFrom literature
11 Coccoliths, length, standard deviationCocco l std dev±Bolton, Clara TFrom literature
12 Coccoliths, thicknessCocco thickµmBolton, Clara TFrom literature
13 Coccoliths, thickness, standard deviationCocco thick std dev±Bolton, Clara TFrom literature
14 Coccoliths, shape factorksBolton, Clara TFrom literature
15 Coccoliths, shape factor, standard deviationks std dev±Bolton, Clara TFrom literature
16 Coccoliths, shape factorksBolton, Clara TFrom literature3.5 µm to 4.5 µm
17 Coccoliths, shape factor, standard deviationks std dev±Bolton, Clara TFrom literature3.5 µm to 4.5 µm
18 Reference/sourceReferenceBolton, Clara T
19 Uniform resource locator/link to referenceURL refBolton, Clara T
20 Sample commentSample commentBolton, Clara T
Status:
Curation Level: Enhanced curation (CurationLevelC)
Size:
579 data points

Data

Download dataset as tab-delimited text — use the following character encoding:


Event

Latitude

Longitude

Date/Time

Elevation [m]

Age [Ma]
(From original publication)

Age [ka BP]

PIC/POC
(Mean)

PIC/POC ratio std dev [±]
10 
Cocco l [µm]
11 
Cocco l std dev [±]
12 
Cocco thick [µm]
13 
Cocco thick std dev [±]
14 
ks
15 
ks std dev [±]
16 
ks
(3.5 µm to 4.5 µm)
17 
ks std dev [±]
(3.5 µm to 4.5 µm)
18 
Reference
19 
URL ref
20 
Sample comment
154-925 4.2042-43.48911994-02-08-30520.947947.440.7960.1273.1840.8080.3130.0620.0640.0160.0550.011Bolton et al. (2016)doi:10.1038/ncomms10284Bolton et al 2016 updated Tanner et al subm
154-9254.2042-43.48911994-02-08-30521.8931893.120.7810.1563.5651.4360.3200.0730.0620.0220.0560.011Bolton et al. (2016)doi:10.1038/ncomms10284Bolton et al 2016 updated Tanner et al subm
154-9254.2042-43.48911994-02-08-30522.9772976.550.8380.1303.0660.7500.3250.0680.0650.0150.0630.011Bolton et al. (2016)doi:10.1038/ncomms10284Bolton et al 2016 updated Tanner et al subm
154-9254.2042-43.48911994-02-08-30524.0464046.070.5980.1472.8371.1650.2250.0890.0500.0170.0460.013Bolton et al. (2016)doi:10.1038/ncomms10284Bolton et al 2016 updated Tanner et al subm
154-9254.2042-43.48911994-02-08-30525.0285027.600.7010.1315.0981.3010.3520.0880.0440.0120.0380.010Bolton et al. (2016)doi:10.1038/ncomms10284Bolton et al 2016 updated Tanner et al subm
154-9254.2042-43.48911994-02-08-30527.2167215.781.5300.2093.2011.0980.5910.0700.1220.0420.0940.018Bolton et al. (2016)doi:10.1038/ncomms10284Bolton et al 2016 updated Tanner et al subm
154-9254.2042-43.48911994-02-08-30528.0398038.991.1920.1913.6431.3400.4940.0900.0920.0360.0850.013Bolton et al. (2016)doi:10.1038/ncomms10284Bolton et al 2016 updated Tanner et al subm
154-9254.2042-43.48911994-02-08-30528.4158415.201.5400.1632.5901.0350.5420.0610.1340.0340.0830.024Bolton et al. (2016)doi:10.1038/ncomms10284Bolton et al 2016 updated Tanner et al subm
154-9254.2042-43.48911994-02-08-30529.8179817.461.1190.2165.9012.6100.5970.2060.1130.0410.0710.016Bolton et al. (2016)doi:10.1038/ncomms10284Bolton et al 2016 updated Tanner et al subm
154-9254.2042-43.48911994-02-08-305213.20013200.101.3010.1654.5101.3970.6040.1040.0900.0260.0930.015Bolton et al. (2016)doi:10.1038/ncomms10284Bolton et al 2016 updated Tanner et al subm
342-U1406 40.3499-51.6498-381418.00018000.001.0650.1885.2701.7070.5290.1330.0660.0180.0620.017Guitián et al. (2020)doi:10.5194/bg-19-5007-2022
342-U140640.3499-51.6498-381418.40818408.460.8470.1275.9301.6620.4840.1080.0500.0140.0520.021Guitián et al. (2020)doi:10.5194/bg-19-5007-2022
342-U140640.3499-51.6498-381418.80418803.730.7940.1286.5901.9880.4980.1030.0480.0130.0590.017Guitián et al. (2020)doi:10.5194/bg-19-5007-2022
342-U140640.3499-51.6498-381420.67220672.080.9810.1484.5101.7940.4500.1580.0650.0150.0700.018Guitián et al. (2020)doi:10.5194/bg-19-5007-2022
342-U140640.3499-51.6498-381422.00122001.030.9240.1285.5001.6880.4940.1480.0610.0140.0610.014Guitián et al. (2020)doi:10.5194/bg-19-5007-2022
342-U140640.3499-51.6498-381423.13323132.760.9350.1203.6001.4030.3620.1190.0620.0130.0610.015Guitián et al. (2020)doi:10.5194/bg-19-5007-2022
342-U140640.3499-51.6498-381423.77223772.470.8970.1254.6601.6140.4220.1420.0610.0120.0640.012Guitián et al. (2020)doi:10.5194/bg-19-5007-2022
342-U140640.3499-51.6498-381425.26925268.790.8630.1435.0601.9140.4440.1710.0580.0130.0590.014Guitián et al. (2020)doi:10.5194/bg-19-5007-2022
342-U140640.3499-51.6498-381425.79925798.870.8670.1585.1602.3140.4400.1910.0580.0140.0590.018Guitián et al. (2020)doi:10.5194/bg-19-5007-2022
342-U140640.3499-51.6498-381426.60626606.140.8800.1294.2802.2140.3790.1630.0570.0130.0550.013Guitián et al. (2020)doi:10.5194/bg-19-5007-2022
342-U140640.3499-51.6498-381428.31228311.900.9040.1363.8301.7830.3680.1270.0580.0150.0590.015Guitián et al. (2020)doi:10.5194/bg-19-5007-2022
154-926 3.7190-42.90831994-02-19-36105.5325532.220.8220.1193.6420.9200.3470.0710.0560.0180.0560.018Tanner et al. (2024)doi:10.22541/essoar.171535711.15687939/v1Pre-print
154-9263.7190-42.90831994-02-19-36105.7815780.551.1720.1783.2601.2450.4670.0930.0770.0270.0770.027Tanner et al. (2024)doi:10.22541/essoar.171535711.15687939/v1Pre-print
154-9263.7190-42.90831994-02-19-36105.8245823.880.7310.1243.2311.3630.2940.0850.0530.0150.0530.015Tanner et al. (2024)doi:10.22541/essoar.171535711.15687939/v1Pre-print
154-9263.7190-42.90831994-02-19-36105.9915991.441.4320.1673.5391.3420.5950.0940.1100.0270.1100.027Tanner et al. (2024)doi:10.22541/essoar.171535711.15687939/v1Pre-print
154-9263.7190-42.90831994-02-19-36106.1836183.000.8860.1313.2641.1850.3530.0790.0670.0170.0670.017Tanner et al. (2024)doi:10.22541/essoar.171535711.15687939/v1Pre-print
154-9263.7190-42.90831994-02-19-36106.2806280.161.1710.1463.2221.0300.4650.0900.0880.0220.0880.022Tanner et al. (2024)doi:10.22541/essoar.171535711.15687939/v1Pre-print
154-9263.7190-42.90831994-02-19-36106.3676367.250.8460.1242.9861.4250.3190.0750.0640.0220.0640.022Tanner et al. (2024)doi:10.22541/essoar.171535711.15687939/v1Pre-print
154-9263.7190-42.90831994-02-19-36106.5276527.480.7710.1743.1031.4540.2990.0880.0440.0250.0440.025Tanner et al. (2024)doi:10.22541/essoar.171535711.15687939/v1Pre-print
154-9263.7190-42.90831994-02-19-36106.6536652.631.0350.1754.1721.4380.4700.1190.0670.0210.0670.021Tanner et al. (2024)doi:10.22541/essoar.171535711.15687939/v1Pre-print
154-9263.7190-42.90831994-02-19-36106.6976696.570.9710.1943.7891.5830.4130.1110.0670.0260.0670.026Tanner et al. (2024)doi:10.22541/essoar.171535711.15687939/v1Pre-print
154-9263.7190-42.90831994-02-19-36106.8466846.001.2650.2013.1051.2220.4850.0880.0970.0330.0970.033Tanner et al. (2024)doi:10.22541/essoar.171535711.15687939/v1Pre-print
154-9263.7190-42.90831994-02-19-36106.9696968.860.8570.1843.5781.3440.3560.1100.0610.0210.0610.021Tanner et al. (2024)doi:10.22541/essoar.171535711.15687939/v1Pre-print
154-9263.7190-42.90831994-02-19-36107.0977097.331.3290.2313.2491.0340.5190.0900.1020.0320.1020.032Tanner et al. (2024)doi:10.22541/essoar.171535711.15687939/v1Pre-print
154-9263.7190-42.90831994-02-19-36107.3277327.001.0160.2082.8440.9730.3750.0620.0770.0320.0770.032Tanner et al. (2024)doi:10.22541/essoar.171535711.15687939/v1Pre-print
154-9263.7190-42.90831994-02-19-36107.4447443.611.1310.1723.0950.9730.4340.0680.0850.0280.0850.028Tanner et al. (2024)doi:10.22541/essoar.171535711.15687939/v1Pre-print
154-9263.7190-42.90831994-02-19-36107.7357734.710.9690.1643.2771.1460.3830.0650.0710.0230.0710.023Tanner et al. (2024)doi:10.22541/essoar.171535711.15687939/v1Pre-print
154-9254.2042-43.48911994-02-08-30520.335334.690.9443.5280.345González‐Lanchas (2011)doi:10.1029/2020PA004175
154-9254.2042-43.48911994-02-08-30520.346345.770.8793.6520.326González‐Lanchas (2011)doi:10.1029/2020PA004175
154-9254.2042-43.48911994-02-08-30520.358357.860.8783.7050.329González‐Lanchas (2011)doi:10.1029/2020PA004175
154-9254.2042-43.48911994-02-08-30520.365365.130.9013.7290.338González‐Lanchas (2011)doi:10.1029/2020PA004175
154-9254.2042-43.48911994-02-08-30520.375374.580.9043.6020.333González‐Lanchas (2011)doi:10.1029/2020PA004175
154-9254.2042-43.48911994-02-08-30520.389389.350.8903.5940.328González‐Lanchas (2011)doi:10.1029/2020PA004175
154-9254.2042-43.48911994-02-08-30520.399399.350.9043.5830.333González‐Lanchas (2011)doi:10.1029/2020PA004175
154-9254.2042-43.48911994-02-08-30520.405405.230.9163.5230.334González‐Lanchas (2011)doi:10.1029/2020PA004175
154-9254.2042-43.48911994-02-08-30520.410410.060.8783.5380.321González‐Lanchas (2011)doi:10.1029/2020PA004175
154-9254.2042-43.48911994-02-08-30520.414414.330.9033.3960.324González‐Lanchas (2011)doi:10.1029/2020PA004175
154-9254.2042-43.48911994-02-08-30520.448447.630.8943.5880.329González‐Lanchas (2011)doi:10.1029/2020PA004175
154-9254.2042-43.48911994-02-08-30520.454454.240.9053.5180.330González‐Lanchas (2011)doi:10.1029/2020PA004175