2.1. Hexane Wash of the Epicuticular Wax of M. pharaonis
Analysis of the hexane wash of the foragers revealed 34 identifiable peaks for the sample using 120 ants and 0.5 min of vortexing (Ant_ref_1). When increasing the number of foragers to 300 (Ant_ref_2), 1200 (Ant_ref_3) and 1200 (Ant_ref_4), the number of peaks identified increased to 40, 51 and 53, respectively. From each peak (
Figure 1), one or multiple compounds were identified, which are all listed in
Table 1.
The 19 extra peaks identified in Ant_ref_4 sample compared to Ant_ref_1 corresponded mostly to compounds with less than 23 or over 31 carbon atoms and all of these compounds were present in low quantities. Nearly all of the GC peaks, identified in reference samples prepared with more foragers and longer vortex times, already showed corresponding peaks in the other reference samples but the resolution was not sufficient for undoubted identification.
While the n-hexane extracts of the
M. pharaonis foragers were made to identify the compounds of the epicuticular wax layer, they also contained several alkaloid compounds (
Figure 1 and
Table 1). These components, including monomorines I, II, III and IV, are not present in the epicuticle, but produced by the ants’ abdominal glands [
31]. Due to the complete immersion of the foragers in n-hexane, the extraction was not limited to the epicuticle and compounds from these glands were also present in the extracts. All of the known monomorines were identified and the presence of several pyrrolines was also registered; however, there was no trace of the previously determined trail pheromone 5-methyl-3-butyl-octahydroindolizine (faranal) [
32]. A compound we did identify in all of the extracts was
trans-2-(1-hex-5-enyl)-5-(non-8-enyl)-pyrrolidine, an alkaloid which was previously defined in the venom of other
Monomorium species [
31,
33]. A trail component previously found in
Solenopsis invicta, α-farnesene [
34], was also found in all of the samples, but present in very small quantities. Finally, both 2-pentyl-5-(1-hex-5-enyl)-1-pyrroline and 2-(1-hexenyl)-5-(hept-6-enyl)-1-pyrroline were also identified based on their GC-MS spectra [
31,
35,
36,
37]. While these exact components were not previously identified, a recent publication by Chen et al. identifies several 2,5-dialkenylpyrrolines as well as a 2-alkyl-5-alkenylpyrroline in the venom of
Monomorium minimum [
38]. Using the same interpretation of the mass spectra (
Appendix A) enabled the identification of these compounds.
The epicuticular waxes extracted by n-hexane consisted solely of hydrocarbons, with the exception of cholesterol (
Figure 1 and
Table 1). Cholesterol was one of the sterols already previously detected in the epicuticular wax layer of
Solenopsis invicta and
richteri [
18].
The relative recovered amounts of the waxes are visualized in the heat map in
Figure 2, except for cholesterol, which was excluded due to its singular profile and small recovered quantity. The hydrocarbons were further divided into compound classes, listed in decreasing order by their recovery in the extract: monomethylalkanes (MeC
n), alkanes (C
n), alkenes (C
n:1), dimethylalkanes (diMeC
n), alkadienes (C
n:2) and trimethylalkanes (triMeC
n) (
Table 2). Nelson already stated that methylated alkanes are often found to be the major component in an insect’s epicuticular wax layer [
39], which is also the case for the pharaoh ant.
In some cases, multiple compound classes, mostly alkenes and alkadienes, were identified in an overlapped GC peak. All of the identified compounds and isomers are listed in
Table 1. In the data presentation of
Figure 2 and in
Table 2, the compound with the highest intensity of its molecular ion of an overlapped GC peak accounts for the full area of the peak. The full dataset from which
Figure 2 is constructed, is provided in
Appendix B (
Table A1).
From the overview of the recovered epicuticular compounds (
Figure 2 and
Table 1), it is clear that, overall, hydrocarbon compounds with an uneven carbon number are present in larger quantities than the compounds with an even carbon number. According to Blomquist, this is a consequence of the formation of these components occurring mainly from two carbon units and a subsequent decarboxylation. However, an occasional chain initiation by propionyl-CoA instead of acetyl-CoA can lead to a small quantity of even n-alkanes [
26]. Unsaturated hydrocarbons with an even carbon number, with exception of triacontene (x-C
30:1), were not observed in the wax extracts. In addition, methylated alkanes with an uneven carbon number in the backbone only have isomers with the methyl groups present in uneven positions. For backbones with an even carbon number, methyl branches were located in both even and uneven positions. While the synthesis pathways of terminal alkanes (2-, 3-, 4-, 5- and 6-methylalkanes) are slightly different from the synthesis pathways of internally branched alkanes (7- to center-chain methylalkanes), the difference between methyl positions on even and odd backbones is identical in both cases and also a result of their biosynthetic origin, confirming these findings [
26]. The same holds for the dimethyl- and trimethylalkanes which all contained, with the exception of 12,16-dimethyldotriacontane (12,16-diMeC
32), uneven backbones. The methyl groups on the uneven backbones were always located in uneven positions. The overall composition of the wax layer of the pharaoh ant bears resemblance to the composition presented for the red harvester ant
Pogonomyrmex barbatus [
17]. The main differences lie in the majority compounds, which are n-heptacosane (n-C27) and n-nonacosane (n-C29) in the pharaoh ant extracts and n-pentacosane (n-C25) for the harvester ants [
17]. In addition, for the pharaoh ant extracts, the dimethylalkanes and trimethylalkanes consistently show the same methyl group positions, with the second (and third) methyl group being separated by three or seven methylene groups, e.g. 9,13,21-trimethyltritriacontane (9,13,21-triMeC
33) and 11,15,23-trimethyltritriacontane (11,15,23-triMeC
33). These distributions are also observed very often in epicuticular wax compositions [
26].
2.2. Adsorption of Synthetic Alkane Mixture on Zeolites
To assess the selectivity of adsorption and the efficiency of the extraction procedure using n-hexane, a synthetic alkane mixture (alkane_mix) was prepared containing the two most abundant n-alkanes present in the wax layer of the pharaoh ant, viz. n-heptacosane and n-nonacosane, as well as a methylated compound, 3-methylpentacosane (3-MeC
25). This product was produced in-house and contained three side-products: 3-methyltetracosane (3-MeC
24), 3-methylhexacosane (3-MeC
26) and 3-methylheptacosane (3-MeC
27). The results of the GC-MS analysis of this alkane mixture and the extracts of the samples loaded with this mixture are provided in
Table 3. In
Table 3, the compounds are grouped per material class, n-alkanes and monomethylalkanes.
Table A2 in
Appendix B provides a full account of the data, listed per individual compound.
These results showed that the analysis of the adsorbed compounds is not trivial. The quantity of hydrocarbons recovered in the n-hexane extracts was systematically lower than the quantity loaded onto the zeolites, indicating that part of the adsorbed hydrocarbons could not be extracted again using n-hexane. The distribution of n-alkanes and monomethylalkanes in the extracts (
Figure 3 and
Table 3) showed that zeolites H-Y-30, H-Y-80, H-BEA-300, NH4-MOR-38 and Na-X-2.2 are non-selective while other zeolite materials—H-BEA-30, NH
4-ZSM5-30, NH
4-ZSM5-280 and H-ZSM22-45—strongly adsorb n-alkanes rather than methylated compounds and thus the extract is enriched with more weakly adsorbed methylated compounds. This effect is less severe in the H-BEA-30 sample, where the percentage of n-alkanes in the extract is still 45.5% compared to 71.1% in total (extractable and non-extractable compounds). In NH
4-ZSM5-30, NH
4-ZSM5-280 and H-ZSM22-45, the zeolites with the narrowest pores of the investigated zeolite collection, the amount of n-alkanes in the extract did not even reach 0.5%, indicating these compounds are particularly strongly adsorbed.
These findings on heavy alkanes are in line with earlier reported selectivity patterns for lighter alkanes by Denayer et al. [
24]. In that study on NH
4-ZSM22-91 zeolite, n-alkanes were found to penetrate deeply inside the pores and were adsorbed strongly, while branched alkanes adsorbed on the surface of the zeolite crystals and in pore mouths where the interaction with the zeolite is weaker [
24]. Short branched alkanes interact with one pore mouth while longer branched alkanes with (C
12+) can penetrate in two or more neighboring pore mouths with part of their chains, a mechanism called key-lock adsorption [
23,
40]. For the small hydrocarbons used by Denayer et al., zeolite Na-Y-60 showed no selectivity towards adsorbing n-alkanes or isoalkanes in its micropores. Zeolite H-ZSM5-274 performed similarly to zeolites mordenite and beta, showing a slight selectivity towards adsorbing n-alkanes over branched compounds in its micropores [
24]. For the long hydrocarbon chains present in the epicuticular wax layer and adsorbed onto the zeolites, the ZSM-5 samples used here (NH
4-ZSM5-30 and NH
4-ZSM5-280) all strongly adsorbed n-alkanes and weakly adsorbed branched compounds, leading to higher recovery of methylated compounds in the extracts. The same behavior was observed by H-ZSM22-45 (
Figure 3 and
Table 4). H-BEA-30 also showed selective adsorption of the n-alkanes over the monomethyl-branched compounds, but this selectivity was less pronounced and zeolites H-Y-30, Na-X2.2, NH
4-MOR-38 and H-BEA-300 did not show any selectivity.
This adsorption selectivity can be explained by the pore sizes of the zeolites (
Table 5) which are in decreasing order: Y = X > MOR > BEA > ZSM5 > ZSM22. Overall, as the hydrocarbons get larger, there is a large increase in adsorption enthalpy, but also a large loss of entropy for adsorption in materials with narrow pores. The loss of entropy is caused by immobilizing the hydrocarbon chain inside the pores. This indicates that longer alkanes, when they are adsorbed, are usually very strongly adsorbed in materials with narrow pores. As the n-alkanes become larger, the pore size they can be strongly adsorbed in also appears to become larger. Not only do NH
4-ZSM5-30 and NH
4-ZSM5-280 (pore size 0.54 × 0.56 nm) strongly adsorb the n-alkanes, even H-BEA-30 (pore size 0.57 × 0.75 nm) shows selective adsorption of the n-alkanes. Overall, H-BEA-30, NH
4-ZSM5-30, NH
4-ZSM5-280 and H-ZSM22-45 strongly adsorb more of all of the compounds in the synthetic alkane mixture, both the n-alkanes and 3-methylalkanes than the other samples, because both can enter the small micropores, at least for the most part, up to the position of the methyl branch [
23]. However, it is likely that the 3-methyl branched compounds undergo key-lock adsorption and some of the molecules are adsorbed mostly on the surface of the zeolite, where they are less strongly adsorbed (
Figure 4).
The selectivity for H-BEA-300 was different from H-BEA-30, although these samples have the same pore architecture. A possible explanation is that the H-BEA-300 sample has more framework defects, widening the pores, since the high Si/Al ratio of 300 was obtained by a dealumination treatment which damages the zeolite crystals [
41]. This assumption is backed by the smaller microporous surface area and larger BET (Brunauer-Emmett-Teller) specific surface area in H-BEA-300 compared to H-BEA-30, indicating the presence of more pores with a larger pore size in H-BEA-300 than H-BEA-30 (
Table 6) [
21].
2.3. Adsorption of Epicuticular Waxes on Zeolites
The zeolites adsorbed a significant amount of hydrocarbons upon contact with the pharaoh ant foragers. Zeolite Na-X-2.2 was the only material adsorbing some alkaloid components (
Table 2) in addition to hydrocarbons. This is probably due to the polarity of this zeolite, since it contains a large amount of sodium cations in its pores. In some zeolites, overlapping peaks of alkenes and alkadienes showed a higher abundance of alkenes, whereas, in the hexane wash of the foragers, the alkadienes were more prominent. In addition, the peak corresponding to dotriacontene (x-C
32:1), found in some zeolite samples, is largely masked in the ant extract by 3-methylhentriacontane (3-MeC
31). In addition, two compounds were recovered from these zeolite extracts which could not be defined in the reference samples obtained from the foragers: 7- to 13-methylhexacosane (7- to 13-MeC
26) and both 9,13,21- and 11,15,23-trimethyltritriacontane (9,13,21- and 11,15,23-triMeC
33) (
Figure 2). The observation of these compounds in extracts from zeolites and not in the hexane wash of the foragers shows that these compounds were more effectively collected on the zeolites than in the n-hexane solvent.
Similar to what was observed with the synthetic alkane mixture, the adsorbed cuticular hydrocarbons could not be quantitatively recovered from the zeolite samples by extraction with n-hexane. The adsorption selectivity was probed by analyzing the uptake of compounds which were also present in the synthetic alkane mixture: n-heptacosane (n-C27), n-nonacosane (n-C29), 3-methylpentacosane (3-MeC25) and 3-methylheptacosane (3-MeC27) (
Figure 5A and
Table A3). 3-methyltetracosane (3-MeC
24) and 3-methylhexacosane (3-MeC
26) were not included, since they were not found in the extracts from the zeolites.
While all zeolite extracts were slightly enriched with 3-methylalkanes, showing that n-alkanes are overall more difficult to extract, the lowest enrichment was present in H-Y-80 sample. This zeolite has the widest pores in the zeolite collection (
Table 5) and serves as the reference sample. The extracts from zeolites H-BEA-30, NH4-ZSM5-30, NH4-ZSM5-280 and H-ZSM22-45 were further enriched in 3-methyl branched compounds, showing these zeolites are shape selective. Shape selectivity in alkane adsorption means that the uptake of linear alkanes is preferred over branched ones. Shape selectivity earlier observed with shorter alkanes in the literature was clearly present with epicuticular wax compounds in this research [
23,
24,
40].
Since the epicuticular wax layer of the pharaoh ants consists of more compounds than were present in the synthetic alkane mixture, deeper investigation into the adsorption selectivity of the zeolites was possible. Shape selective adsorption of n-alkanes on zeolites H-BEA-30, NH
4-ZSM5-30, NH
4-ZSM5-280 and H-ZSM22-45 is observed for very long chains up to n-C
30 (n-triacontane) and monomethyl-branched isomers (
Figure 5B,
Table A3). This adsorptive discrimination among linear and mono-branched alkanes vanished, however, for alkanes containing 30 or more carbon atoms (
Figure 6).
The absence of shape selectivity with the longest chains suggests that these very heavy alkanes do not penetrate entirely inside the small pores of zeolites ZSM5, ZSM22 and H-BEA-30. If the increase in adsorption enthalpy does not compensate the loss of entropy, the adsorption of the whole chain would be thermodynamically unfavorable. In this instance, part of the hydrocarbon chain containing the methyl branching would stay outside of the pores as would a similar-sized part of a corresponding n-alkane chain. This leads to a similar Gibbs free energy of adsorption in both cases and thus the absence of selectivity.
The dataset was also used to evaluate whether there was adsorption selectivity based on chain length. For this purpose, the n-alkanes were divided in two groups: n-alkanes shorter than C
30 and C
30 and longer. This revealed that some zeolites (NH
4-ZSM5-30, NH
4-ZSM5-280, H-ZSM22-45, H-BEA-30, Na-X-2.2 and NH
4-MOR-38) selectively adsorb n-alkanes smaller than n-triacontane (n-C
30). The ZSM-5 and ZSM-22 zeolites haves the narrowest pores among the investigated zeolites. It is now observed that these zeolites preferentially adsorb shorter chains. These shape selective zeolites, ZSM5 and ZSM22, also showed adsorption preference for n-alkanes over dimethyl- and trimethylalkanes as well as for monomethylalkanes over dimethylalkanes and trimethylalkanes (
Figure 7A–D and
Table A3).
This is to be expected since branching widens the molecules. Zeolite H-BEA-30 having somewhat wider pores adsorbs n-alkanes preferentially and also discriminates according to chain length, but the selective adsorption is less pronounced in both cases (
Figure 5 and
Figure 6). Zeolites Na-X-2.2 and NH
4-MOR-38 do not discriminate according to branching, but do according to chain length. This is surprising, since these zeolites have among the widest pores (
Table 7). Zeolite H-BEA-300 was again different because this one shows a preference for adsorbing branched compounds over linear ones. Such a selectivity was coined inverse shape selectivity and may be explained by the tighter fitting of branched isomers in the pores of the zeolite [
42].
Finally, the data also provided insight on the adsorption selectivity of unsaturated hydrocarbons (
Figure 8 and
Table A3). Here, the preferential uptake of alkenes and alkadienes is most pronounced on NH
4-ZSM5-280 and H-BEA-300 (
Figure 7A–D and
Table A3). There is no straightforward explanation why these zeolites would stand out. NH
4-ZSM5-30 and H-ZSM22-45 also selectively adsorbed the n-alkenes and n-alkadienes, but the selectivity was less prominent in these samples. This selectivity is also evident in the identification of the epicuticular wax compounds, where dotriacontene (x-C32) was only identified in the extract from H-Y-30, H-Y80, Na-X-2.2 and NH
4-MOR-38, but, at the same retention time, 3-methylhentriacontane was identified in the extracts from H-BEA-300 and H-ZSM22-45. O’Connor already showed a similar use of preferential adsorption by applying a molecular sieve (5A) to adsorb alkanes from a synthetic mixture to reveal small dimethylalkane peaks which would otherwise be unidentifiable [
44].
With exception of the extracts from the more polar zeolite Na-X-2.2, zeolite H-ZSM22-45 and zeolite NH
4-MOR-38—the three least insecticidal materials—all of the zeolite extracts show an enrichment of alkene over alkadiene components when compared to the hexane wash (
Table 2). A full overview of the selectivity types found in the zeolites and their pore sizes is provided in
Table 5.
A peculiar note is that NH
4-MOR-38 shows by far the highest total adsorbed amounts of cuticular hydrocarbons while it was one of the less effective insecticidal materials from previous research [
21] (
Table 1 and
Table 2, and
Figure 2). These observations lead us to think not only the adsorption capacity itself is important, but that also the selective adsorption by the insecticidal material of certain components can strongly influence their effectiveness.