Technical Note : Determining the size-normalised weight of planktic foraminifera

Introduction Conclusions References Tables Figures


Introduction
The ocean contains about 38 Gt of carbon, accounting for 98% of the combined oceanatmosphere carbon reservoir (Zeebe and Wolf-Gladrow, 2001).The size and nature of the marine carbon inventory implies that the ocean plays a significant role in determining atmospheric pCO 2 concentrations, and therefore global climate, from decadal to millenial timescales (Broecker and Peng, 1982).Palaeoclimatic research has provided valuable insights into the global climate system, but our understanding of the carbon Figures cycle is far from complete (e.g.Archer et al., 2000;Sigman and Boyle, 2000;Peacock et al., 2006).As anthropogenic pCO 2 emissions continue to alter marine carbon chemistry (Caldeira and Wickett, 2003;Zeebe et al., 2008), with ill-defined consequences for marine biota (Orr et al., 2005;Raven et al., 2005), there is a pressing need to better understand the operation of marine biogeochemical processes.
One palaeo-proxy with the potential to shed light on past changes in marine carbon chemistry is the size-normalised weight (SNW) of planktic foraminifera, which is a measure of test wall thickness and density.SNW of planktic foraminifera collected from the seafloor is influenced by calcite dissolution processes, with lower SNW values indicative of waters with a low calcite saturation state (Ω) and low [CO 2−  3 ] (Zeebe and Wolf-Gladrow, 2001;Broecker and Clark, 2001a).SNW was therefore originally proposed and developed as a quantitative deepwater [CO 2− 3 ] proxy (Lohmann, 1995;Broecker andClark, 2001a,b, 2003) under the assumption that, for any given species, the initial SNW is uniform in space and time.We now know, however, that the initial SNW is determined by the ambient environmental conditions during calcification (Broecker and Clark, 2004).In particular, culture studies reveal that calcification rate is enhanced, and the test wall thickness and hence SNW increased, at elevated CO 2− 3 concentrations (Bijma et al., 1999(Bijma et al., , 2002;;Russell et al., 2004).Well-preserved foraminiferal specimens collected from marine sediments have therefore been used to investigate past changes in surface water [CO 2− 3 ], which, significantly, is inversely related to atmospheric pCO 2 concentrations (e.g.Barker and Elderfield, 2002;Moy et al., 2009;de Moel et al., 2009).However, a recent analysis of the SNW-[CO 2− 3 ] correlations suggests that SNW is a function of multiple, as yet undetermined, environmental controls and not [CO 2− 3 ] exclusively (Beer et al., 2010).Although clearly in development, SNW remains an inexpensive, easily determined and potentially highly valuable palaeo-proxy.
Different researchers have used different methods to generate SNW data, making direct comparison between studies difficult.In essence, techniques used to establish SNW attempt to gauge changes in test wall thickness/density and must remove the influence of test size on weight.It is important that size is accounted for effectively be-  (Hecht, 1976;Schmidt et al., 2002Schmidt et al., , 2006) ) and therefore potentially obfuscate the test wall thickness/density signal.Broadly speaking, size is constrained, and SNW established, using one of two methods.The simplest method with most rapid throughput involves weighing specimens picked from a narrow sieve fraction (typically a 50 µm range) with the resultant data here termed the "sieve-based weight" (SBW; e.g.Broecker and Clark, 2001a).The second method is more labour-intensive and involves measuring the size of each individual test which has been picked from within a narrow sieve fraction.The test weights are then normalised to the mean measured test size to obtain a "measurement-based weight" (MBW; e.g.Barker and Elderfield, 2002).Ideally, weight would be normalised to the mean volume enclosed within the exterior perimeter of the test wall.This volume parameter is, however, very difficult and time-consuming to establish and alternative size parameters, such as test diameter, are typically substituted for volume.
In this study, well-preserved planktic foraminiferal specimens collected by nets from the water column in the North Atlantic Ocean are employed to generate SNW estimates using both techniques on the same aliquots.Our aims are to i) quantitatively assess whether sieving satisfactorily removes the influence of size on test weight, ii) determine which of the two techniques are preferable for the estimation of SNW and iii) consider which of the test size measurements (e.g.diameter) is best used to normalise test weight.added to the samples in order to retard remineralisation of organic material, which engenders carbonate dissolution, and buffered using hexamethyltetramine to a pH of 8.2.Specimens were then isolated from the sample using a pipette and dried before sieving.Only specimens of G. bulloides that did not possess spines were employed.Specimens were delicately brush-cleaned to remove adhered material not associated with the foraminifera prior to analysis.A total of 219 aliquots from 29 locations in the North Atlantic, mainly in the vicinity of BIOTRANS ( 47• N, 20

Foraminiferal specimens of
• E; Table 1), were used in this study.A minimum of 10 specimens (mean=19) from the 200-250 µm fraction were picked, uniformly orientated with umbilical side facing upwards and measured using an integrated, semi-automated microscope and image analysis system (cf. Bollmann et al., 2004).Use of the 200-250 µm fraction represents a compromise between the need to obtain a statistically reasonable number of tests and the desire to use large specimens and thereby obtain a sufficient aliquot mass for precision weighing.The image analysis system provides mean values for the test silhouette area and test diameter for each aliquot, where diameter is taken to be the mean of the diameters which bisect the centre of the foraminiferal test, as observed in 2-dimensions.Following size-analysis, the tests were placed into pre-weighed aluminium capsules and transferred to an environmentally controlled weighing room.The samples were left for a minimum of 12 h to equilibrate with the ambient atmospheric moisture content before being weighed (precision=0.001mg) to obtain SBW.Samples were not oven dried before being weighed because it was found that they increased in weight during the weighing process, presumably as they absorbed moisture from the atmosphere.MBW was calculated by normalising SBW to the mean diameter (MBW diam ) and area (MBW area ) for the corresponding species.
Given the large density difference between calcite (2.71 g cm −3 ) and wet cytoplasm (1.07 g cm −3 ), and their fractional contributions to the dry test mass (0.97 and 0.03, respectively; Schiebel et al., 2007) we did not treat the specimens for organic matter prior to weighing.

Results
In Fig. 1 we show SBW against test size (area) for all four species considered in this study -in each case our data reveal a correlation between SBW and area (0.5<r 2 <0.7).In contrast, no such correlations are obtained between MBW area and area (Fig. 2).Note that the weight differences observed within our dataset are quite large, and are perhaps attributable to gametogenic crusts.Our data also demonstrate that SBW correlates more strongly with MBW diam (r 2 = 0.91; p<0.0001) than MBW area (r 2 = 0.67; p<0.0001; supplementary Fig. 1, see http://www.biogeosciences-discuss. net/7/905/2010/bgd-7-905-2010-supplement.pdf).In Fig. 3 we show the percentage difference between MBW area and SBW for each aliquot.Our results show that the mean difference between MBW area and SBW is close to zero, but the standard deviation is 11.3%.Overall, 23% of MBW area values differ from their corresponding SBW values by more than ±10%.

Efficacy of sieving
The correlations between SBW and area seen in our data (0.5<r 2 <0.7;Fig. 1) indicate that use of a narrow sieve fraction (200-250 µm) fails to remove the influence of test size on test weight.The maximum effect of size variations within the sieve fraction can be calculated by assuming that all the foraminifera weighed in an aliquot are either 200 µm or 250 µm in diameter, spherical in shape and effectively sieved.If all specimens were 200 µm in diameter, and normalised to the mid-point of the range (225 µm), SBW would be 27% less than MBW area .Conversely, if all specimens were 250 µm in diameter, SBW would exceed MBW area by 19%.However, because foraminiferal tests are not spherical, some tests are found outside of these theoretical extremes (Fig. 3).Moreover, we find that sieved tests are larger than would be expected given the sieve The finding that SBWs are in part determined by test size implies that SBW is not a good approximation of SNW.The mean difference between values of SBW and MBW area is approximately zero, but the standard deviation (σ) is 11.3%.We take this value (11%) to equal the error in SBW for the sieve fraction used in this study (200-250 µm).Although not directly comparable because different studies use different sieve size fractions, it is instructive to note that this error estimate is of the same order of magnitude as the change observed in some published downcore records of SNW.For example, published records describe a 20-33% change in SNW during the last deglaciation (Barker and Elderfield, 2002;de Moel et al., 2009;Moy et al., 2009) jma et al., 1999, 2002).The use of larger specimens and a narrower sieve size window improves sieve-based estimates of SNW, as does increasing the number of specimens employed (J.Bijma, personal communication, 2010).This is illustrated in Fig. 4, where the calculated potential difference between SBW and MBW area is shown to decrease with the use of larger specimens and a narrower sieve fraction window.However, reducing the size of the sieve size window reduces the number of specimens available for weighing, as does use of large specimens.Moreover, there are important pragmatic considerations.
SNW data are often generated as a "by-product" on samples prepared for geochemical analyses, so the sieve size fraction may be pre-determined.Hence, while the SBW method is best suited to situations where a large number of large specimens are available from a narrow sieve fraction, in many circumstances, an alternative approach to generating SNW is needed.

Establishing MBW
Ideally, measurement-based weight is calculated by normalizing SBW to test volume.However, volume is very difficult to measure so must be either estimated from, or substituted by, alternative parameter(s).In the absence of empirical functions linking test volume to more easily measured variables, volume must be estimated by assuming that the foraminiferal test is a certain shape.An alternative approach, which avoids the use of necessarily crude approximations of the test shape, is the use of area or diameter to directly normalise test weight.In doing so, test diameter, area and volume are assumed to remain proportional to one another over the size range of interest (Barker, 2002).Although proportionality cannot be demonstrated (because of the absence of volume measurements) the strong correlation between area and diameter (r 2 = 0.87) lends support to the assumption of proportionality between the three measurements.Moreover, our results indicate that, unlike SBW, both MBW diam and MBW area do not correlate with test area (r 2 = 0.18 and r 2 = 0.007, respectively; supplementary Fig. 3; Fig. 2) and diameter (r 2 = 0.07 and r 2 = 0.003, respectively; supplementary Fig. 3).
This finding suggests that MBW, calculated using either area or diameter, provides a means by which variations in test wall density and thickness can be reliably characterised.

Conclusions
The SNW of planktic foraminifera, a measure of test wall thickness and density, has the potential to provide valuable palaeoceanographic information.However, the different methods employed by different workers to establish SNW makes comparisons between studies difficult.Our results, based on specimens picked from the 200-250 µm fraction, show that sieving the tests does not adequately remove the influence of test size.In Introduction

Conclusions References
Tables Figures

Back Close
Full Screen / Esc Printer-friendly Version Interactive Discussion our experiment, SNW estimates based on the sieve-based method using tests from the 200-250 µm fraction are associated with an error of ca.11%.This source of error may be reduced by increasing the number of specimens per aliquot and by employing a smaller sieve fraction range relative to the size of the foraminifera examined.However, in many circumstances this will not be practically possible because, for example, too few large tests are present.In such circumstances it is preferable to employ the measurement-based method, which does not necessitate the use of numerous large specimens picked from a very narrow sieve size window, in order to characterise test wall thickness and density and thereby obtain reliable SNW estimates.
Full The difference between SBW and MBW area for different sieve window sizes from 150 to 25 µm centred on 300 µm.The smallest differences between SBW and MBW area are obtained by using large foraminifera and a small sieve window.

Fig. 1 .Fig. 2 .Fig. 3 .
Fig. 1.The mean sieve-based test weight (SBW; µg) versus the mean test area (µm2 ) for aliquots of planktic foraminifera sampled using a multiple-opening-closing net in the North Atlantic Ocean picked from the 200-250 µm sieve fraction.The correlations observed (0.5<r 2 <0.7; p<0.0001) suggest that typically "narrow" sieve fractions provide an insufficient control on the size-determined variations in test weight.

Table 1 .
Locations of multinet sampling stations in the North Atlantic.