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Tell, Franziska (2022): Base of productive zone of N. pachyderma during cruises ARK-IV/3, ARK-XI/1, ARK-XIII/2, ARK-XV/1, ARK-XV/2, M21/4, M21/5, M39/4, MSM44, MSM66, MSM09/2, NEWP-92, NEWP-93, PS93.1, PS31, PS78 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.940549, In: Tell, F (2022): Neogloboquadrina pachyderma compiled data from vertical profiles in the Arctic Ocean [dataset bundled publication]. PANGAEA, https://doi.org/10.1594/PANGAEA.941250

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Abstract:
Based on shell concentrations of the planktonic foraminifera Neogloboquadrina pachyderma from vertically resolved plankton tow samples during cruises ARK-IV/3, ARK-XI/1, ARK-XIII/2, ARK-XV/1, ARK-XV/2, MSM44, MSM66, M21/4, M21/5, M39/4, MSM09/2, NEWP-92, NEWP-93, PS93.1, PS31, PS78, the base of the productive zone is calculated. The calculation is based on the assumption that the base of productive zone is located where shell concentration begins to substantially decline and it is calculated after Lončarić et al. (2006).
Keyword(s):
Arctic; Neogloboquadrina pachyderma; Planktonic foraminifera
Related to:
Tell, Franziska; Jonkers, Lukas; Meilland, Julie; Kucera, Michal (2022): Upper-ocean flux of biogenic calcite produced by the Arctic planktonic foraminifera Neogloboquadrina pachyderma. Biogeosciences, 19(20), 4903-4927, https://doi.org/10.5194/bg-19-4903-2022
Source:
Bauch, Dorothea; Carstens, Jörn; Wefer, Gerold (1997): Oxygen isotope composition of living Neogloboquadrina pachyderma (sin.) in the Arctic Ocean. Earth and Planetary Science Letters, 146(1-2), 47-58, https://doi.org/10.1016/S0012-821X(96)00211-7
Greco, Mattia; Jonkers, Lukas; Kretschmer, Kerstin; Bijma, Jelle; Kucera, Michal (2019): Depth habitat of the planktonic foraminifera Neogloboquadrina pachyderma in the northern high latitudes explained by sea-ice and chlorophyll concentrations. Biogeosciences, 16, 3425–3437, https://doi.org/10.5194/bg-16-3425-2019
Kohfeld, Karen E; Fairbanks, Richard G; Smith, Sharon L; Walsh, Ian D (1996): Neogloboquadrina Pachyderma (sinistral coiling) as Paleoceanographic Tracers in Polar Oceans: Evidence from Northeast Water Polynya Plankton Tows, Sediment Traps, and Surface Sediments. Paleoceanography, 11(6), 679-699, https://doi.org/10.1029/96PA02617
Pados, Theodora; Spielhagen, Robert F (2014): Species distribution and depth habitat of recent planktic foraminifera in Fram Strait, Arctic Ocean. Polar Research, 33(1), 22483, https://doi.org/10.3402/polar.v33.22483
Schiebel, Ralf (2002): Planktic foraminiferal sedimentation and the marine calcite budget. Global Biogeochemical Cycles, 16(4), 1065, https://doi.org/10.1029/2001GB001459
Simstich, Johannes; Sarnthein, Michael; Erlenkeuser, Helmut (2003): Paired d18O signals of Neogloboquadrina pachyderma (s) and Turborotalita quinqueloba show thermal stratification in Nordic Seas. Marine Micropaleontology, 48(1-2), 107-125, https://doi.org/10.1016/S0377-8398(02)00165-2
Stangeew, Elena (2001): Distribution and isotopic composition of living planktonic foraminifera N. pachyderma (sinistral) and T. quinqueloba in the high latitude North Atlantic. PhD Thesis, Mathematisch-Naturwissenschaftliche Fakultät der Christian-Albrechts-Universität zu Kiel, Germany, 90 pp, urn:nbn:de:gbv:8-diss-4645
Volkmann, Renate (2000): Planktic foraminifer ecology and stable isotope geochemistry in der Arctic Ocean: implications from water column and sediment surface studies for quantitative reconstructions of oceanic parameters (Ökologie planktischer Foraminiferen und stabile Isotope im Arktischen Ozean: Anwendbarkeit für die quantitative Rekonstruktion von ozeanischen Parametern). Berichte zur Polarforschung = Reports on Polar Research, 361, 100 pp, https://doi.org/10.2312/BzP_0361_2000
Funding:
German Research Foundation (DFG), grant/award no. 221211316: GRK/IRTG 1904: ArcTrain - Processes and impacts of climate change in the North Atlantic Ocean and the Canadian Arctic
Coverage:
Median Latitude: 75.364512 * Median Longitude: 2.985520 * South-bound Latitude: 48.856800 * West-bound Longitude: -79.307450 * North-bound Latitude: 86.101667 * East-bound Longitude: 149.973300
Date/Time Start: 1987-07-08T00:00:00 * Date/Time End: 2017-08-20T17:22:00
Minimum Elevation: -4653.0 m * Maximum Elevation: -298.0 m
Event(s):
M21/4_MSN694 (224) * Latitude: 62.502750 * Longitude: -13.992350 * Date/Time: 1992-06-07T05:09:00 * Elevation: -1483.0 m * Campaign: M21/4 * Basis: Meteor (1986) * Method/Device: Multiple opening/closing net (MSN)
M21/4_MSN696 (225) * Latitude: 64.000117 * Longitude: -9.870567 * Date/Time: 1992-06-08T01:04:00 * Elevation: -665.0 m * Campaign: M21/4 * Basis: Meteor (1986) * Method/Device: Multiple opening/closing net (MSN)
M21/4_MSN697 (227) * Latitude: 65.515560 * Longitude: -3.971780 * Date/Time: 1992-06-09T07:07:00 * Elevation: -3117.0 m * Location: Aegir Ridge * Campaign: M21/4 * Basis: Meteor (1986) * Method/Device: Multiple opening/closing net (MSN)
Comment:
The calculation of the base of the productive zone of N. pachyderma is based on the assumption that the base of productive zone is located where shell concentration begins to substantially decline, which was determined visually. For all cases in which abundances decrease with depth, it is calculated after Lončarić et al. (2006): Z_BPZ=(C_n-C_exp)/C_(n-1) (Z_n-Z_(n-1) )+Z_(n-1)
All BPZ that is based on this equation have the remark “regular” in the column of calculation method. As the equation is constructed for cases where the shell concentration decreases with depth, it cannot be applied where this is not the case (such as where there is a distinct subsurface maximum), as the estimated BPZ would appear to lie below the depth interval of the transition zone. In those cases, the BPZ was defined as the bottom depth of the transition zone (labeled as range end).
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Event labelEventTell, Franziska
2Optional event labelEvent 2Tell, Franziska
3Sample code/labelSample labelTell, Franziska
4Campaign of eventCampaignTell, Franziska
5Date/Time of eventDate/TimeTell, Franziska
6Latitude of eventLatitudeTell, Franziska
7Longitude of eventLongitudeTell, Franziska
8Elevation of eventElevationmTell, Franziska
9Neogloboquadrina pachyderma, Base of Productive ZoneN. pachyderma BPZmTell, FranziskaCalculated after Lončarić et al. (2006)
10Calculation method, Base of Productive ZoneMethod BPZTell, Franziska
11Reference/sourceReferenceTell, Franziska
12Reference/sourceReferenceTell, Franziska
13Reference/sourceReferenceTell, Franziska
14Reference/sourceReferenceTell, Franziska
Status:
Curation Level: Enhanced curation (CurationLevelC)
Size:
632 data points

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