Technical note 09 Aug 2018
Technical note  09 Aug 2018
Technical note: A refinement of coccolith separation methods: measuring the sinking characteristics of coccoliths
 ^{1}State Key Laboratory of Marine Geology, Tongji University, Shanghai, 200092, China
 ^{2}Geological Institute, Department of Earth Science, Sonneggstrasse 5, ETH, 8092, Zurich, Switzerland
 ^{3}AixMarseille Université, CNRS, IRD, Coll. de France, CEREGE, AixenProvence, France
 ^{1}State Key Laboratory of Marine Geology, Tongji University, Shanghai, 200092, China
 ^{2}Geological Institute, Department of Earth Science, Sonneggstrasse 5, ETH, 8092, Zurich, Switzerland
 ^{3}AixMarseille Université, CNRS, IRD, Coll. de France, CEREGE, AixenProvence, France
Correspondence: Chuanlian Liu (liucl@tongji.edu.cn)
Hide author detailsCorrespondence: Chuanlian Liu (liucl@tongji.edu.cn)
Quantification sinking velocities of individual coccoliths will contribute to optimizing laboratory methods for separating coccoliths of different sizes and species for geochemical analysis. The repeated settling–decanting method was the earliest method proposed to separate coccoliths from sediments and is still widely used. However, in the absence of estimates of settling velocity for nonspherical coccoliths, previous implementations have depended mainly on timeconsuming empirical method development by trial and error. In this study, the sinking velocities of coccoliths belonging to different species were carefully measured in a series of settling experiments for the first time. Settling velocities of modern coccoliths range from 0.154 to 10.67 cm h^{−1}. We found that a quadratic relationship between coccolith length and sinking velocity fits well, and coccolith sinking velocity can be estimated by measuring the coccolith length and using the length–velocity factor, k_{v}. We found a negligible difference in sinking velocities measured in different vessels. However, an appropriate choice of vessel must be made to avoid “hindered settling” in coccolith separations. The experimental data and theoretical calculations presented here support and improve the repeated settling–decanting method.
Coccolithophores are some of the most important phytoplankton in the ocean. They can secrete calcareous plates called coccoliths, which contribute significantly to discrete particulate inorganic carbon in the euphotic zone and to CaCO_{3} fluxes to the deep ocean (e.g., Young and Ziveri, 2000; Sprengel et al., 2002). Coccolith morphology, geochemistry and fossil assemblage composition can reflect paleoenvironmental changes (e.g., Beaufort et al., 1997; Stoll et al., 2002; Zhang et al., 2016). However, the use of coccolith geochemical analyses in paleoenvironmental reconstructions has so far been impeded by the difficulty of isolating coccoliths compared with foraminifera. Two main methods have been developed to concentrate nearmonospecific assemblages of coccoliths from bulk sediments: one is the method based on a decanting technique (Paull and Thierstein, 1987; Stoll and Ziveri, 2002) and the other is that based on microfiltration (Minoletti et al., 2009). The improvement of separation techniques offered a new perspective to study the Earth's history (e.g., Stoll, 2005; Beltran et al., 2007; Bolton and Stoll, 2013; Rousselle et al., 2013). Moreover, the development of coccolith oxygen and carbon isotope studies in culture in recent years (e.g., Ziveri et al., 2003; Rickaby et al., 2010; Hermoso et al., 2016; McClelland et al., 2017) has provided an improved mechanistic understanding of coccolith isotope data and therefore stimulated the need for more purified coccolith fraction samples from the fossil record.
Both decanting and microfiltering are widely used methods for coccolith separation. The microfiltering method separates coccoliths with a polycarbonate microfilter membrane (with pore sizes of 2, 3, 5, 8, 10 and 12 µm). This method is highly effective in the larger size ranges but is very timeconsuming in sediments with a high proportion of small (< 5 µm) coccoliths (which tends to be the case in natural populations). It is also impossible to separate coccoliths such as Florisphaera profunda and Emiliania huxleyi with similar lengths by microfiltration (Hermoso et al., 2015). Decanting, on the other hand, is highly effective for the smallsized coccoliths, because their slow settling times permit a greater ability to separate different sizes. Consequently, in some studies, a combination of the micro filtering and sinking or centrifugation method were applied for coccolith separation (Stoll, 2005; Bolton et al., 2012; Hermoso et al., 2015). The repeated sinking–decanting method, first employed by (Edwards, 1963; Paull and Thierstein, 1987) follows the simple principle formalized by Stokes' law for spherical particles: particles of a larger size settle more quickly because they have a higher ratio of volume and mass (accelerating sinking) to sectional area (resistance retarding sinking). However, the sinking velocities of coccoliths with a complex shape are difficult to calculate and have not been quantified in previous studies. Consequently, the repeated decanting method has generally used settling times based on empirical trial and error.
In the current study, we present a novel and rigorous estimation of sinking velocity for 16 species of modern and Cenozoic coccoliths, carefully measured in 0.2 % ammonia at 20 ^{∘}C. With this new dataset, we explore how to estimate the sinking velocity of coccoliths based on their shape and length, which allows our estimations to be generalized for other species and for situations where the mean length of coccoliths of a given species was different from that of our study. These generalizations, together with our results on sinking velocities of one coccolith species (Gephyrocapsa oceanica) in different vessels, should allow a significant improvement in the efficiency of future protocols for the separation of coccoliths by repeated decanting.
2.1 Sample selections
We measured the sinking velocity of 16 different species of coccoliths, isolated from eight deepsea sediment samples from the Pacific and Atlantic oceans (Fig. 1, Table A1 in Appendix). Sample were principally of Quaternary age but include two Neogene/Paleogene samples. In general, numbers of small coccoliths, including E. huxleyi, Gephyrocapsa spp. and Reticulofenestra spp., are about 1 order of magnitude greater than that of larger coccoliths. However, the larger coccoliths' contributions to carbonate can be as high as 50 % (Baumann, 2004; Jin et al., 2016). Moreover, both small coccoliths and large coccoliths are useful in geochemical analyses (Ziveri et al., 2003; Rickaby et al., 2010; Candelier et al., 2013; Bolton et al., 2012, 2016; Bolton and Stoll, 2013). Therefore, both small and large coccoliths were studied in this research. Pictures of the studied coccolith are shown in Appendix B, and all classifications follow Nannotax3 except Reticulofenestra spp. (Fig. C2 in Appendix C).
2.2 Experiment designs
2.2.1 Sample pretreatments
The sinking velocity measurement depends on absolute abundance estimation (more details in Sect. 2.2.2). However, on microscope slides, larger coccoliths and foraminifer fragments may cover smaller coccoliths, reducing the accuracy of coccolith absolute numbers. Thus, before sinking experiments were carried out, raw sediments were pretreated to purify the target coccoliths to reduce errors in coccolith counting. The raw sediments were disaggregated in 0.2 % ammonia and sieved through a 63 µm sieve and then treated by the sinking method or the filtering method (Bolton et al., 2012; Minoletti et al., 2009) to concentrate the target species up to at least more than 50 % of the total assemblage (for Noelaerhabdaceae coccoliths, a percentage of more than 90 % can be easily achieved). In one sample with aggregation (ODP 807), we did a rapid settling (30 min, 2 cm) to eliminate aggregates. Most of the species were measured individually in settling experiments, except for Pseudoemiliania lacunosa and Umbilicosphaera sibogae, which were measured together.
2.2.2 Measuring the sinking speeds of coccoliths
We are not aware of any prior direct determination of the sinking velocity of individual coccoliths, although the sinking velocities of live coccolithophores and other marine algal cells have been successfully measured by the FlowCAM method (Bach et al., 2012) or a similar photography technique (e.g., Miklasz and Denny, 2010). Here, we introduce a simple method to measure the particle sinking speeds without special equipment.

After pretreatment, the coccolith suspensions were gently shaken and then moved into comparison tubes which were vertically mounted on tube shelves. We set the timer going and let the suspension settle for a specified period of time, marked as sinking time or settling duration (T).

Thereafter, we removed the upper 15 mL supernatant into a 50 mL centrifuge tube with a 10 mL pipette. This operation was performed slowly and gently to avoid drawing lower suspensions upward. The absolute counting of coccolith was achieved by using the “drop technique” to make quantitative microscope sides (Koch and Young, 2007; Bordiga et al., 2015). In total, 0.3 mL mixed suspension was extracted with pipettes onto a glass cover, and the slider was dried on a hotplate.

The lower suspension was than homogenized and another slider was prepared as described above.

The number of coccoliths in the upper and lower suspensions were carefully counted on microscope at ×1250 magnification and the number of coccoliths and fields of view (FOV) were recorded for further calculations. More than 300 specimens were counted for most of the measurements. For the Helicosphaera carteri measurements, more than 100 FOV were checked and about 100 specimens were counted.
To calculate the sinking velocities of coccoliths, we define a parameter named the separation ratio (R), which represents the percentage of removed coccoliths in one separation by pumping out the upper suspension. This parameter is important and will be repeatedly mentioned in the following part. R was measured using the following equation (more details about derivation can be found in Appendix D):
where N_{1} and N_{2} are numbers of coccoliths counted on upper and lower suspension slides, respectively; n_{1} and n_{2} are the number of FOV counted. V_{1} and V_{2} are the volume of the settling vessel defined by the settling distance, as shown in Fig. 2.
The separation ratio, R, also has a relationship with sinking time, T (Appendix D):
where V_{1}, V_{2} and D are the shape parameters shown in Fig. 2 and v is the average sinking velocity of measured coccoliths. If we plot R against T, the slope of the line has a relationship with v. Then linear regressions between R and T were processed with MATLAB to calculate the v (details about error analyses can be found in Appendix E).
There are still two issues to be explained. Firstly, to eliminate the shape differences among vessels, all separation ratios have been transferred to calibrated separation ratios (R_{cal}), which means the separation ratio measured in a standard vessel with V_{1}=15 mL, V_{2}=10 mL and D=6 cm (more details about transformation from R to R_{cal} can be found in Appendix D). Secondly, we treated the average sinking velocities as the sinking velocities of the coccoliths with the average length. This approximation is proved reasonable in Appendix D.
2.2.3 Detecting the potential influence of vessels
Seven commonly used vessels were selected to detect the potential influence of vessels (Fig. 3). Two of them are made of plastics (no. 2 and no. 3 in Fig. 3), and all others are pyrex glass vessels. About 500 mg of sediment from core KX212 were pretreated as described in Sect. 2.2.1 and suspended in about 500 mL diluted ammonia. After that, settling experiments were performed as described in Sect. 2.2.2 using different vessels. In these experiments, only the dominant species, G. oceanica, was measured.
2.2.4 Other factors influencing the sinking velocity
Temperature can change the density and viscosity of liquid. Generally speaking, the higher the temperature is, the lower the density and viscosity will become and the faster pellets will sink. Take water, for instance: if the temperature increases from 15 to 30^{∘}, the particle sinking velocity will increase by ∼43 % (Table 1). All sinking velocities measured or discussed in the following sections were velocities at 20 ^{∘}C to minimize the influence of temperature.
The calibration of sinking velocity in highconcentration suspension has been calculated by Richardson and Zaki (1954):
where the α_{s} is the solids volume fraction. Based on Eq. (3), the higher the suspension concentration is, the slower the sinking velocity will be. This is socalled “hindered settling”. When the α_{s}=0.2 %, the reduction in sinking velocity owing to hindered settling is negligible (v∕v_{0} equals 99.46 %). Hence, in this study all suspensions have solid volume fractions lower than 0.2 % to avoid notable reductions in coccolith sinking velocities.
3.1 Influence of vessels
The sinking velocities of G. oceanica in the core KX212 in 0.2 % ammonia at 20 ^{∘}C measured in different vessels vary from 0.99 to 1.23 cm h^{−1}. The lowest value occurred in the 100 mL centrifuge tube and the highest sinking velocity was measured in the 50 mL centrifuge tube experiments. The correlations between sinking velocities and different vessel parameters are quite low: r=0.13 for the vessel inner diameter, r=0.0005 for the sinking distance, and r=0.051 for the upper volume and total volume ratio (${V}_{\mathrm{1}}/({V}_{\mathrm{1}}+{V}_{\mathrm{2}})$). The dissipation of energy by friction between the moving fluid and the walls can cause a reduction in sinking speed (wall effect). A significant wall effect will be detected when a particle is settling in a vessel with a diameter that is smaller than 100 times the particle size (Barnea and Mizarchi, 1973). The length of coccoliths is on the micron scale, so the diameters of vessels used in the laboratory are more than 4 orders of magnitude larger than coccoliths. Moreover, our results show that the difference between vessel materials, glass and plastics can also be ignored (Fig. 4). Hence, we suggest that vessel type almost has no significant influence on the sinking velocity of coccoliths.
However, our experiments were premised on the basis that the concentration of suspension was equal among different vessels. This means that large vessels can treat more sediment at one time, but if we choose a larger vessel, we need to spend more time in pumping suspensions, and it often costs more time in terms of sinking (often due to longer sinking distance). Assuming that the sediment is composed of 50 % calcite (with a density of 2.7 g cm^{−3}) and 50 % clay (about 1.7 g cm^{−3}), the largest amount of sediment that can be used without a significant reduction in the sinking velocity (5 %) is about 400 mg in 100 mL suspension (this calculation is based on Eq. 3). However, because sediments accumulate in the lower suspension, the particle concentration can be more than 4 times higher than in the initial homogenous concentration. This phenomenon will be more significant for a vessel with a narrow bottom, such as centrifuge tubes. To avoid this, we recommend using about 100 mg dry sediment suspended in at least 100 mL suspension to avoid hindered settling. If more sediment is necessary for geochemistry analyses, then a larger vessel should be selected to separate enough sample at one time.
3.2 Sinking velocities at 20 ^{∘}C in 0.2 % ammonia
We measured the separation ratios of different coccoliths in comparison tubes at 20 ^{∘}C in 0.2 % ammonia (Fig. 5). The sinking velocities of coccoliths were then calculated by linear fitting of separation ratios and settling durations. The sinking velocities of studied coccoliths vary by 2 orders of magnitude from 0.154 to 10.67 cm h^{−1} (Table 2). The highest sinking velocity was found in the measurement of Coccolithus pelagicus, and the lowest velocity was found for F. profunda. The average sinking speed of coccoliths is about 10 %–50 % of the terminal sinking velocities of calcite spheres calculated by Stokes' law (Fig. 6c). These ratios are comparable to the ovalobject (e.g., seeds) data from Xie and Zhang (2001) and smaller than the steelellipsoid data from McNown and Malaika (1950). The sinking velocities of coccoliths measured in our experiment are about 2–3 orders of magnitude smaller than values from sediment traps of 143–243 m d^{−1} (595 ∼1012 cm h^{−1}) in the North Atlantic (Ziveri et al., 2000; Stoll et al., 2007), suggesting that the coccoliths sinking out of the euphotic layer are mainly in the form of sinking aggregates rather than individual coccoliths.
3.3 Estimating the sinking velocities
Generally speaking, the sinking velocities of coccoliths increase with distal shield length (Fig. 5a), as expected from the increase in volume to sectional area for a given geometry as length increases. Our data imply that the sinking velocity has a power function relationship with distal shield length.
We propose that the sinking velocity of coccoliths might have a quadratic relationship with distal shield length as described by Stokes' law (Fig. 6a). If we use data for all species except H. carteri (the reason can be found in the following discussion), the sinking velocities can be described by the following equation:
Based on this quadratic regression, we derive a shape–velocity factor (k_{v}) that relates settling velocity to coccolith length.
Furthermore, this factor is analogous to the shape–mass factor, k_{s}, used to relate coccolith mass to coccolith length (Young and Ziveri, 2000). The length and shape–velocity factor of coccoliths can be used to predict most of the sinking velocity variations; however, variations may also arise due to changes in coccolith mass and thickness, for a given length, and due to the hydrodynamics of particular shapes. We noticed that the smaller coccolith G. caribbeanica has a greater sinking velocity than the larger coccolith, G. oceanica. We suggest that this was caused by greater mass per length (or greater average thickness) in the case of G. caribbeanica, and this may be due to the closed central area while G. oceanica has an open central area. Another example is H. carteri, the lower sinking velocity of which can be explained by the unique structure of H. carteri coccolith. Firstly, the broad edge of H. carteri can increase the drag force significantly. Moreover, most of the measured coccoliths have a ellipticity (major axis length and minor axis length ratio) larger than 0.8, while the ellipticity of H. carteri is around 0.6, which means the mass of H. carteri is smaller than other species of coccoliths with similar lengths (Figs. 6d and C3). That is also the reason H. carteri was excluded from the general regression in Eq. (4). In the case of partial dissolution, the wellpreserved Cyclicargolithus floridanus may have higher mass than dissolved (or disarticulated) C. floridanus and therefore a slightly higher shape–velocity factor.
To improve coccolith separation by settling methods, we measured sinking velocities of different coccoliths by gravity. Sinking velocities in this study varied from 0.154 to 10.61 cm h^{−1}, about 10 % to 50 % of those of calcite spheres with the same diameter. The shape of different vessels had little impact on the sinking velocity. But we should consider the volume of vessels to avoid hindered settling. The sinking velocities are mainly controlled by the shape of coccoliths, including the distal shield length, the size of the central area and the ellipticity of coccoliths. Besides the shape of coccoliths, temperature is also crucial to the coccolith separations because of the dependence of sinking velocities on temperature. Length–velocity factors were proposed to estimate coccolith sinking velocities, so coccolith separation can be achieved by the following steps:

Measure the length of coccoliths in your target assemblage under the microscope and regress the length distribution by the assumption of a normal distribution (details are in Appendix C).

Estimate sinking velocities for each important species. For species whose sinking speed has been directly measured, we can use the length–velocity factor directly ($v={k}_{\mathrm{v}}\times {\mathit{\varphi}}^{\mathrm{2}}$). For unmeasured species, we can choose the length–velocity factor of coccoliths with a similar morphology in this study or use the general length–velocity formula ($v=\mathrm{0.098}(\pm \mathrm{0.001}\times {\mathit{\varphi}}^{\mathrm{2}}$).

Calculate the separation time for the main species. For example, in KX212 there are three main coccoliths (F. profunda, G. oceanica and C. leptoporus), and we wish to separate G. oceanica out from the bulk sediment. Calculate each coccolith's sinking velocity distributions as described in Step 2 above. As shown in Fig. 7, a sinking velocity intermediate between F. profunda (with a length 2σ larger than average, marked as +2σ) and G. oceanica (with a length 2σ smaller than average, marked as −2σ), optimal for separating them, would be 0.6 cm h^{−1}. Similarly, we can chose speed thresholds of 1.85 cm h^{−1} to separate G. oceanica from C. leptoporus. If we settle in a 50 mL centrifuge tube with a sinking distance, D, equal to 5.84 cm, the sinking time for separating F. profunda should be $T=\mathrm{5.84}/\mathrm{0.6}=\mathrm{9.73}$ h. Similarly, we can calculate the time for separating G. oceanica by $T=\mathrm{5.84}/\mathrm{1.85}=\mathrm{3.16}$ h.

Homogenize the sediment suspension and let coccoliths settle for the period calculated in Step 3. After that, pump out the upper part of the suspension. In the upper part, we exclusively have the smaller of the main coccoliths. However, the column will still contain some smaller ones. So this step (settling and pumping) should be repeated until the lower part no longer has any significant contribution from the smaller coccoliths. This step has been described well in previous studies, and more details can be found in Stoll and Ziveri (2002) and Bolton et al. (2012).
We find that, if we use the general formula, a closed central area coccolith will sink faster than predicted (G. caribbeanica and small C. leptoporus will settle ∼40 % faster) and coccoliths with greater ellipticity can settle much more slowly (H. carteri will settle as 30 % of the predicted sinking velocity for coccoliths with similar length). Moreover, the sinking method cannot separate every species of coccoliths perfectly. As mentioned in Sect. 2.2.1, P. lacunosa and U. sibogae cannot easily be separated from each other because they have similar sinking velocities. Nevertheless, this study provides the first direct estimation of coccolith settling velocities, which should simplify the implementation of future methods to separate coccoliths by settling time.
The sinking velocities and coccolith length results can be found in Table 2.
To measure the distal shield length of coccoliths, pictures were taken at a magnification of 1250× under circular polarized light. The coccolith lengths were measured by using the image analysis software, ImageJ. More than five pictures were taken, and more than 50 (usually more than 100) coccolith specimens were measured. The length distributions of coccoliths measured in our experiments are shown in Fig. C1.
The classification of coccoliths by length was supported by mixture analysis in PAST (Hammer et al., 2001), such as Reticulofenestra spp. and Gephyrocapsa spp. Reticulofenestra spp. in the Miocene were classified into two groups, Ret. (< 4 µm) and Ret. (> 4 µm). The traditional classification of Reticulofenestra spp. is < 3, 3–5 and 5–7 µm did not pass the normal distribution test. Hence, in this study the Reticulofenestra spp. are divided at 4 µm (Fig. C2). Gephyrocapsa spp. were divided by the shape (length and central area) of coccoliths into small Gephyrocapsa (central area opening and length < 3.5 µm), G. oceanica (central area opening and length > 3.5 µm) and G. caribbeanica (closed central area).
In this part, the derivation of the equation will be explained in detail including proofs of several assumptions mentioned in the Materials and methods section.
When the wellmixed sediment begins to sink, the decrease in coccolith number in the upper suspension (N_{u}) can be described by the following equation:
where the D is the length of upper suspension and ${N}_{\mathrm{u}(t=\mathrm{0})}/D$ is the initial number of coccoliths in a cross section with a unit thickness; v is the mean sinking velocity of coccolith. In practice, the velocities of coccoliths are different, so we assume that the measured velocity is the mean sinking velocity of bulk coccolith. This assumption will be proved valid in the following. The particle can reach 99.9 % of the maximum sinking velocity within only 10^{−7} s, so we assume that the particle sinks with maximum velocity from when it begins to settle.
Through integrating Eq. (D1), we can get the variation in coccolith number in the upper column over time:
where T is settling time. After a period of time (T), we pump out the upper suspension. Here, we define the number of coccoliths in the upper supernatant dividing the total coccoliths number in the tube (N_{t}) as the separation ratio (R), which represents the percentage of total coccoliths removed in one separation. R can be expressed by
Assuming all coccoliths are uniformly distributed in the suspension at the beginning of settling, N_{u(t=0)} has the following relationship with N_{t}:
where V_{1} is the volume of upper suspension and V_{2} is the volume of lower suspension.
Combining the Eqs. (D1), (D2), (D3) and (D4), we obtain the relationship between the separation ratio, R, and sinking velocity, v, as follows:
If we plot R and T on a figure, the slope of the line is a function of V_{1}, V_{2}, D and v. Since V_{1}, V_{2} and D are known parameters, we say the slope of R−T is a function of v, which is exactly what we want.
The comparison tubes used in our experiments have the same V_{1} and V_{2} but different D. Other vessels used in other experiments have different V_{1}, V_{2} and D. So we should adjust the raw separation ratio to the calibrated separation ratio (R_{cal}), which represents the separation ratio in a standard vessel with V_{1 SD}=15 mL, V_{2 SD}=10 mL and D_{SD}=6 cm. This step can be described by Eq. (D6):
After calibration, the slope of R_{cal}−T (k) has the following relationship with v:
where k is the slope of R_{cal} against T from regression and other parameters are as described above. Hence, the sinking velocity of different coccoliths can be achieved by measuring the variations in R_{cal} over time.
The coccoliths' lengths in the sediment have some variations. So what we measured is actually the bulk settling velocity of the whole coccolith population. We also offer a test for the assumption that the average sinking velocity of all coccoliths can be treated as the sinking velocity of coccoliths with the average length. Here, we used the data of G. oceanica. A normal distribution was fitted to the measured length distribution (Fig. D1a). We generated 100 000 coccolith following the normal distribution, and let these coccolith evenly distribute in the comparison tube at the beginning and then allowed them to sink without colliding with each other. The sinking velocities of different size coccoliths were calculated by the velocity–shape parameter k_{v} as described in the Results and discussions section. We modeled the coccoliths sinking process and computed the separation ratio (red dashed line in Fig. D1b), coccolith length (red dashed line in Fig. D1c) and instant sinking velocities (orange dots in Fig. D1d) at different time sections.
For G. oceanica experiments, the instant sinking velocity would not change significantly until settling for more 3 h. That means for all R_{cal} larger than 15 % are safe for linear regressions. The minimum safe number of R_{cal} will decrease with the drop of dispersion degree of the coccolith length distribution. Hence, our assumption of average sinking velocity and the use of linear regression are proved to be reasonable.
The errors of the measured separation ratio (R) and calculated sinking velocity (v) are mainly caused by counting coccoliths, the error of which follows the Poisson distribution. To detect the influence of counting number on the result error, the error of the separation ratio was simulated by 5000 Monte Carlo calculations with assumptions that ${V}_{\mathrm{1}}:{V}_{\mathrm{2}}=\mathrm{15}:\mathrm{10}$ and n_{1}=n_{2} (Fig. E1). The result shows that the number of coccoliths counted in the upper column has greater influence on the relative error ($R{R}_{\mathrm{95}\mathrm{CL}}/R$). That means more coccoliths in the upper suspension should be counted to make results more accurate. The slope of R_{cal}−T was calculated by linear fitting with the intercept fixed on ${V}_{\mathrm{1}}/({V}_{\mathrm{1}}+{V}_{\mathrm{2}}$). The input R_{cal} were generated from measured values considering the error of coccolith counting (by the Matlab function “random”). The regressions of R_{cal}−T were repeated by 5000 regressions in the software Matlab (by the function “lsqcurvefit”), and the error of sinking velocity, v, was taken from the distribution slope of R_{cal}−T in the Monte Carlo process.
This study was conceived by HZ and CL. Measurements and calculations were conducted by HZ. HZ, HS and CB wrote the paper with the help from XJ and CL.
The authors declare that they have no conflict of interest.
This study was supported by grants from the Chinese National Science Foundation
(91428310, 91428309 and 41530964, to Chuanlian Liu) and ETH Zurich (to Heather
Stoll). It was also supported by Chinese Scholarship Council (CSC) scholarship
to Hongrui Zhang. We thank the Integrated Ocean Drilling Program (IODP) for providing the samples. The IODP is sponsored by
the US National Science Foundation and participating countries under
management of IODP Management International, Inc (IODPMI). We thank Zhimin Jian for providing the sample of the core ODP 807.
We thank three anonymous reviewers as well as the editor for their comments and
suggestions, which helped us to improve the original version of the paper.
Edited by: Lennart de Nooijer
Reviewed by:
three anonymous referees
Bach, L. T., Riebesell, U., Sett, S., Febiri, S., Rzepka, P., and Schulz, K. G.: An approach for particle sinking velocity measurements in the 3–400 µm size range and considerations on the effect of temperature on sinking rates, Mar. Biol., 159, 1853–1864, https://doi.org/10.1007/s0022701219452, 2012.
Barnea, E. and Mizrahi, J.: A generalized approach to the fluid dynamics of particulate systems: Part 1. General correlation for fluidization and sedimentation in solid multiparticle systems, Chem. Eng. J., 5, 171–189, https://doi.org/10.1016/03009467(73)800085, 1973.
Baumann, K.H.: Importance of size measurements for coccolith carbonate flux estimates, Micropaleontology, 50, 35–43, 2004.
Beaufort, L., Lancelot, Y., Camberlin, P., Cayre, O., Vincent, E., Bassinot, F., and Labeyrie, L.: Insolation cycles as a major control of equatorial Indian Ocean primary production, Science, 278, 1451–1454, https://doi.org/10.1126/science.278.5342.1451, 1997.
Beltran, C., de Rafélis, M., Minoletti, F., Renard, M., Sicre, M. A., and Ezat, U.: Coccolith δ^{18}O and alkenone records in middle Pliocene orbitally controlled deposits: Highfrequency temperature and salinity variations of sea surface water, Geochem. Geophy. Geosy., 8, Q05003, https://doi.org/10.1029/2006GC001483, 2007.
Bolton, C. T. and Stoll, H. M.: Late Miocene threshold response of marine algae to carbon dioxide limitatio, Nature, 500, 558–562, https://doi.org/10.1038/nature12448, 2013.
Bolton, C. T., Stoll, H. M., and MendezVicente, A.: Vital effects in coccolith calcite: Cenozoic climatepCO_{2} drove the diversity of carbon acquisition strategies in coccolithophores, Paleoceanography, 27, PA4204, https://doi.org/10.1029/2012pa002339, 2012.
Bolton, C. T., HernandezSanchez, M. T., Fuertes, M. A., GonzalezLemos, S., Abrevaya, L., MendezVicente, A., Flores, J. A., Probert, I., Giosan, L., Johnson, J., and Stoll, H. M.: Decrease in coccolithophore calcification and CO_{2} since the middle Miocene, Nat. Commun., 7, 10284, https://doi.org/10.1038/ncomms10284, 2016.
Bordiga, M., Bartol, M., and Henderiks, J.: Absolute nannofossil abundance estimates: Quantifying the pros and cons of different techniques, Revue de Micropaléontologie, 58, 155–165 https://doi.org/10.1016/j.revmic.2015.05.002, 2015.
Candelier, Y., Minoletti, F., Probert, I., and Hermoso, M.: Temperature dependence of oxygen isotope fractionation in coccolith calcite: A culture and core top calibration of the genus Calcidiscus, Geochim. Cosmochim. Ac., 100, 264–281, https://doi.org/10.1016/j.gca.2012.09.040, 2013.
Channell, J., Sato, T., Kanamatsu, T., Stein, R., and Alvarez Zarikian, C.: Expedition 303/306 synthesis: North Atlantic climate, Channell, JET, edited by: Kanamatsu, T., Sato, T., Stein, R., Alvarez Zarikian, C. A., Malone, M. J., and the Expedition, 303, 306: 4–6, 2010.
Edwards, A. R.: A preparation technique for calcareous nannoplankton, Micropaleontology, 9, 103–104, 1963.
Hammer, Ø., Harper, D., and Ryan, P.: Paleontological Statistics Software: Package for Education and Data Analysis, Palaeontol. Electron., 4, 1–9, 2001.
Hermoso, M., Candelier, Y., Browning, T. J., and Minoletti, F.: Environmental control of the isotopic composition of subfossil coccolith calcite: Are laboratory culture data transferable to the natural environment?, Geoci. Res. J., 7, 35–42, https://doi.org/10.1016/j.grj.2015.05.002, 2015.
Hermoso, M., Chan, I. Z. X., McClelland, H. L. O., Heureux, A. M. C., and Rickaby, R. E. M.: Vanishing coccolith vital effects with alleviated carbon limitation, Biogeosciences, 13, 301–312, https://doi.org/10.5194/bg133012016, 2016.
Jin, H., Jian, Z., Cheng, X., and Guo, J.: Early Pleistocene formation of the asymmetric eastwest pattern of upper water structure in the equatorial Pacific Ocean, Chinese Sci. Bull., 56, 2251–2257, 2011.
Jin, X., Liu, C., Poulton, A. J., Dai, M., and Guo, X.: Coccolithophore responses to environmental variability in the South China Sea: species composition and calcite content, Biogeosciences, 13, 4843–4861, https://doi.org/10.5194/bg1348432016, 2016.
Kell, G. S.: Density, thermal expansivity, and compressibility of liquid water from 0^{∘} to 150^{∘} correlations and tables for atmospheric pressure and saturation reviewed and expressed on 1968 temperature scale, J. Chem. Engin. Data, 20, 97–105, 1975.
Kestin, J., Sokolov, M., and Wakeham, W. A.: Viscosity of liquid water in the range −8 ^{∘}C to 150 ^{∘}C, J. Phys. Chem. Ref. Data, 7, 941–948, 1978.
Koch, C. and Young, J.: A simple weighing and dilution technique for determining absolute abundances of coccoliths from sediment samples, J. Nannoplankton Res., 29, 67–69, 2007.
Li, C.F., Lin, J., and Kulhanek, D. K.: South China Sea tectonics: Opening of the South China Sea and its implications for southeastAsian tectonics, climates, and deep mantle processes since the late Mesozoic, IODP Sci. Prosp., 349, 32–39, 2013.
Liang, D. and Liu, C.: Variations and controlling factors of the coccolith weight in the Western Pacific Warm Pool over the last 200 ka, J. Ocean U. China, 15, 456–464, 2016.
McClelland, H. L., Bruggeman, J., Hermoso, M., and Rickaby, R. E.: The origin of carbon isotope vital effects in coccolith calcite, Nat. Commun., 8, 14511, https://doi.org/10.1038/ncomms14511, 2017.
McNown, J. S. and Jamil, M.: Effects of particle shape on settling velocity at low Reynolds numbers, Eos, 31, 74–82, 1950.
Miklasz, K. A. and Denny, M. W.: Diatom sinkings speeds: Improved predictions and insight from a modified Stokes' law, Limnol. Oceanogr., 55, 2513–2525, https://doi.org/10.4319/lo.2010.55.6.2513, 2010.
Minoletti, F., Hermoso, M., and Gressier, V.: Separation of sedimentary micronsized particles for palaeoceanography and calcareous nannoplankton biogeochemistry, Nat. Protocol., 4, 14–24, https://doi.org/10.1038/nprot.2008.200, 2009.
Paull, C. K. and Thierstein, H. R.: Stable isotopic fractionation among particles in Quaternary coccolithsized deepsea sediments, Paleoceanography, 2, 423–429, https://doi.org/10.1029/PA002i004p00423, 1987.
Richardson, J. and Zaki, W.: The sedimentation of a suspension of uniform spheres under conditions of viscous flow, Chem. Eng. Sci., 3, 65–73, 1954.
Rickaby, R. E. M., Henderiks, J., and Young, J. N.: Perturbing phytoplankton: response and isotopic fractionation with changing carbonate chemistry in two coccolithophore species, Clim. Past, 6, 771–785, https://doi.org/10.5194/cp67712010, 2010.
Rousselle, G., Beltran, C., Sicre, M.A., Raffi, I., and De Rafélis, M.: Changes in seasurface conditions in the Equatorial Pacific during the middle Miocene–Pliocene as inferred from coccolith geochemistry, Earth Planet. Sc. Lett., 361, 412–421, https://doi.org/10.1016/j.epsl.2012.11.003, 2013.
Sprengel, C., Baumann, K.H., Henderiks, J., Henrich, R., and Neuer, S.: Modern coccolithophore and carbonate sedimentation along a productivity gradient in the Canary Islands region: seasonal export production and surface accumulation rates, DeepSea Res. Pt. II, 49, 3577–3598 https://doi.org/10.1016/S09670645(02)000991, 2002.
Stoll, H. M.: Limited range of interspecific vital effects in coccolith stable isotopic records during the PaleoceneEocene thermal maximum, Paleoceanography, 20, PA1007, https://doi.org/10.1029/2004pa001046, 2005.
Stoll, H. M. and Ziveri, P.: Separation of monospecific and restricted coccolith assemblages from sediments using differential settling velocity, Mar. Micropaleontol., 46, 209–221, https://doi.org/10.1016/S03778398(02)000403, 2002.
Stoll, H. M., Rosenthal, Y., and Falkowski, P.: Climate proxies from Sr/Ca of coccolith calcite: calibrations from continuous culture of Emiliania huxleyi, Geochim. Cosmochim. Ac., 66, 927–936, https://doi.org/10.1016/S00167037(01)008365, 2002.
Xie, H.Y. and Zhang, D.W.: Stokes shape factor and its application in the measurement of spherity of nonspherical particles, Powder Technol., 114, 102–105, https://doi.org/10.1016/S00325910(00)002692, 2011.
Young, J. R. and Ziveri, P.: Calculation of coccolith volume and it use in calibration of carbonate flux estimates, DeepSea Res. Pt. II, 47, 1679–1700, https://doi.org/10.1016/S09670645(00)000035, 2000.
Zhang, H., Liu, C., Jin, X., Shi, J., Zhao, S., and Jian, Z.: Dynamics of primary productivity in the northern South China Sea over the past 24,000 years, Geochem. Geophy. Geosy., 17, 4878–4891, https://doi.org/10.1002/2016GC006602, 2016.
Ziveri, P., Stoll, H., Probert, I., Klaas, C., Geisen, M., Ganssen, G., and Young, J.: Stable isotope “vital effects” in coccolith calcite, Earth Planet. Sc. Lett., 210, 137–149, https://doi.org/10.1016/S0012821X(03)001018, 2003.
 Abstract
 Introduction
 Materials and methods
 Results and discussions
 Suggestions for coccolith velocity estimations and separations
 Data availability
 Appendix A: Sample selections
 Appendix B: Coccolith images under circular polarized light
 Appendix C: The length distribution of coccoliths
 Appendix D: Coccolith movement in gravity settling
 Appendix E: Statistical and error analyses
 Author contributions
 Competing interests
 Acknowledgements
 References
 Abstract
 Introduction
 Materials and methods
 Results and discussions
 Suggestions for coccolith velocity estimations and separations
 Data availability
 Appendix A: Sample selections
 Appendix B: Coccolith images under circular polarized light
 Appendix C: The length distribution of coccoliths
 Appendix D: Coccolith movement in gravity settling
 Appendix E: Statistical and error analyses
 Author contributions
 Competing interests
 Acknowledgements
 References