Abstract
In the ectomycorrhizal caesalpiniaceous groves of southern Korup National Park, the dominant tree species, Microberlinia bisulcata, displays very poor in situ recruitment compared with its codominant, Tetraberlinia bifoliolata. The reported ex situ experiment tested whether availabilities of soil potassium and magnesium play a role. Seedlings of the two species received applications of K and Mg fertilizer in potted native soil in a local shade house, and their responses in terms of growth and nutrient concentrations were recorded over 2 years. Amended soil concentrations were also determined. Microberlinia responded strongly and positively in its growth to Mg, but less to K; Tetraberlinia responded weakly to both. Added Mg led to strongly increased Mg concentration for Microberlinia while added K changed that concentration only slightly; Tetraberlinia strongly increased its concentration of K with added K, but only somewhat its Mg concentration with added Mg. Additions of Mg and K had small but important antagonistic effects. Microberlinia is Mg‐demanding and apparently Mg‐limited in Korup soil; Tetraberlinia, whilst K‐demanding, appeared not to be K‐limited (for growth). Added K enhanced plant P concentrations of both species. Extra applied Mg may also be alleviating soil aluminum toxicity, and hence improving growth indirectly and especially to the benefit of Microberlinia. Mg appears to be essential for Microberlinia seedling growth and its low soil availability in grove soils at Korup may be an important contributing factor to its poor recruitment. Microberlinia is highly shade‐intolerant and strongly light‐responding, whilst Tetraberlinia is more shade‐tolerant and moderately light‐responding, which affords an interesting contrast with respect to their differing responses to Mg supply. The study revealed novel aspects of functional traits and likely niche‐partitioning among ectomycorrhizal caesalps in African rain forests. Identifying the direct and interacting indirect effects of essential elements on tropical tree seedling growth presents a considerable challenge due the complex nexus of causes involved.
Keywords: Growth, magnesium: potassium, recruitment limitation, tree seedlings, tropical forest
Introduction
The Atlantic Coastal Forest of Central Africa is a spatially and temporally complex forest type characterized by patches of varying extent in which species of the subfamily Caesalpiniaceae (family Fabaceae = Leguminosae) dominate compositional abundance (Letouzey 1968, 1985). A great majority of these species are in the tribe Amherstieae and accordingly they are ectomycorrhizal (EM) (Newbery et al. 1988). A question central to understanding the ecology of this African forest is how, locally and regionally, these relatively few EM species have come to be much more abundant than the many non‐EM ones (Gartlan et al. 1986; Newbery and Gartlan 1996; Newbery et al. 1997). At Korup in southwest Cameroon, three caesalps species, Microberlinia bisulcata A. Chev., Tetraberlinia bifoliolata Harms (Haumann), and Tetraberlinia korupensis Wieringa, codominate in groves (large patches), among which M. bisulcata is the most abundant in terms of basal area and defines grove perimeter (Newbery et al. 2004, 2013). Korup lies within the Guinea–Congolean refugium, one of the last large and intact remnants of the Atlantic Coastal Forest (Gartlan 1992). This lowland tropical rain forest stands on strongly weathered, well‐draining, and nutrient‐poor, sandy soils at an elevation of 50–150 m above sea level.
Despite the apparent high degree of adaptation of adult M. bisulcata trees to the site, and copious seed and seedling production every 2–3 years on mast fruiting (Green and Newbery 2002; Newbery et al. 2006a, 2009; Norghauer and Newbery 2015), M. bisulcata is nevertheless not replacing itself either within or outside the groves (Newbery et al. 1997, 2004). This is evidenced by the high seedling mortality, and resulting in very low densities of sapling and juvenile trees (Newbery et al. 2006b, 2010, 2013). By contrast, T. bifoliolata and T. korupensis do show good regeneration in terms of seedling, sapling, and juvenile tree densities. This situation has naturally been the subject of intensive research since the mid‐1980s, leading to a new hypothesis of ‘transient dominance’ explaining the current frequency distribution of tree sizes of M. bisulcata (Newbery et al. 2013). Norghauer and Newbery (2010) showed that establishment limitation was 2–4‐fold stronger than seed limitation in M. bisulcata, whereas seed limitation was always stronger than seedling limitation in the codominant T. bifoliolata.
Seedlings of M. bisulcata are highly shade‐intolerant and highly light‐responsive (Green and Newbery 2001a,b), and saplings can survive well in the open nursery conditions (D. M. Newbery, unpubl.). By contrast, the two Tetraberlinia species are much more shade‐tolerant and conversely respond less fast to increasing light levels. The relatively small seeds of M. bisulcata (at 0.64 g, 40–50% the dry mass of those of the Tetraberlinia spp.; Green and Newbery 2001a), and their postdispersal susceptibility to fungal infection and animal predation largely in the understorey (Green and Newbery 2002; Norghauer and Newbery 2011), although leaf herbivore attack on seedlings occurs mainly under lighted gap conditions (Green and Newbery 2001b; Norghauer and Newbery 2013, 2014), all play important roles in seedling survival. Neither leaf pathogens (Norghauer et al. 2010) nor soil phosphorus limitation (Newbery et al. 2002) affected seedling growth and survival. And whilst EM infection occurred on seedlings both close to and away from adults (no effect of adult basal area abundance), being infected had little effect on survival in their first 2 years (Newbery et al. 2000). Nitrogen, judging from seedling leaf concentrations, gave no indication of limiting growth and survival in M. bisulcata either (Newbery et al. 2000, 2002; Green and Newbery 2001a,b); levels in soil and litter, likely because of generally high N‐fixing activity in the forest, also did not suggest N‐limitation (Newbery et al. 1997; Chuyong et al. 2002). Of the untested macro‐elements, however, apart from calcium, and ones that might be essential for growth response to light, were potassium and magnesium.
Across the groves and into the surrounding forest matrix of mixed tree species, the deep and, in places stony, sandy acidic quartzite soils have atop them a thin well‐marked 1‐ to 2‐cm layer of organic matter, fine roots, and EM hyphae (Newbery et al. 1988, 1997, 2000;). The intense May–October wet season at Korup (annual rainfall c. 5.5 m, reaching 0.8–1.0 m in August alone), set between the equally marked single December–March dry season (Newbery et al. 1998, 2002, 2006a), means not only a considerable leaching of the canopy and of the soils, but also that this throughfall is coupled with lagged effects of the annual dry‐season peak in litterfall (Chuyong et al. 2000, 2002, 2004). The organic layer is clearly essential for the efficient recycling of N and P through decomposition (Newbery et al. 1997) and it is surmised – and currently under test – that the layer is essential too for the trapping and reuptake of potassium (K) and magnesium (Mg) from this throughfall (G. A. Neba, thesis in prep. and unpubl. data). Litter‐bag trials at Korup (Chuyong et al. 2002) indicated that among the five macronutrients, just Mg showed significantly much higher mineralization rates in grove than nongrove soils, indicative of a large demand by predominantly adult M. bisulcata trees for Mg, and in turn that available levels of Mg would be reduced for seedlings around adults. This new insight led to the hypothesis that Mg could be a potentially limiting factor for M. bisulcata regeneration. The laterally extensive buttressing on M. bisulcata is thought to allow large trees nutrient exploration of very large areas of surface soil in the forest (Newbery et al. 2009).
Gartlan et al. (1986) reported a close association between low phosphorus (P) and low K concentrations in soils of the grove‐forming EM species in Korup. Whilst P has received much attention because of the putative role of EM species in enhancing its availability to, and acquisition by, trees in low‐P soils (Newbery et al. 1997, 2002), the potential role of K in the Korup ecosystem and as a controlling factor of seedling recruitment has been overlooked. Its nutrient transfer, operating to a large degree also via throughfall, gives its nutrient cycling strong temporal parallels with Mg, although the quantities involved are eightfold higher for K than Mg (Chuyong et al. 2004). Furthermore, how availability of K affects seedlings and their EM development, and thereby the efficacy in P uptake, is unknown; it is also unclear how K and Mg may interact in their possible limitations of seedling growth. Thus, a comparison of responses by the light‐responsive M. bisulcata and one of the shade‐tolerant codominant Tetraberlinia spp. to K and Mg supply at levels relevant to their ecology and conditions in the forest was prompted.
The specific aim was to evaluate the effects of Mg and K in various combinations of application level on seedling growth, allocation of dry matter, and nutrient status. The more general aim, however, was to use the results to reach a deeper understanding of whether the two species might be partitioning the forest niche with regard to their use of the elements in early growth. If Mg and K are varying spatially across the forest, as recent findings suggest (G. Neba, unpubl. data), this process might lead to one species recruiting better than the other at different locations (Newbery et al. 2006b, 2010). The experiment set out, therefore, to test a new hypothesis concerning regeneration in the groves of codominant caesalpiniaceous tree species at Korup.
The shade‐house experiment reported here used T. bifoliolata as the second species because its seeds were available along with those of M. bisulcata in the start year. T. korupensis would have been a good alternative had it seeded (Newbery et al. 1988, 2000, 2013). The two selected species will be referred to from here on by just their generic names.
Methods
Experimental design and setup
The experiment was conducted at an open nursery site within the PAMOL plantation near the footbridge over the Mana River, at the entrance to Korup National Park. This 0.3‐ha research site of the University of Bern was set up in 1995 by the clearance of the then 4‐year‐old palms. It had previously supported mature palms, and had received rock phosphate fertilization up until 1982 (Green and Newbery 2001a,b). The substrate, soil, and climatic parameters for the site are otherwise very similar to those of the southern part of the Park, where all the ecological field work has been conducted. Soil of the nursery site was not used in the experiment itself and only as a bedding medium.
Two seed beds were prepared inside of a mesh‐covered shade house (Tildenet, UK) that allowed 25% transmission of external radiation. The bedding soil was inoculated with 10 kg of fresh organic matter collected from below the litter in the top 1–2 cm of the soil profile from under the canopies of six large Microberlinia trees in the 82.5‐ha permanent P‐plot, situated within the main grove at Korup (Newbery et al. 2004, 2013), to ensure suitable ectomycorrhizal inoculation of seedlings. Over 600 freshly collected (fungus‐free) seeds of each species were sown on 5 August 2010. They came from under 30 fruiting Microberlinia and six Tetraberlinia trees across the main Korup grove. Nursery bags were filled with well‐mixed top soil (5.0 kg oven dry weight per bag) excavated from under Microberlinia trees in a 6.75‐ha experimental plot inside another smaller grove lying just outside the southern boundary of the Park, at Isangele Road (Newbery et al. 2002). The surface litter was carefully moved aside and soil taken to a depth of 5–7 cm, which included the thin surface organic layer with larger roots removed. Eight hundred 10‐week‐old seedlings from the nursery bed were individually transplanted into standard 20‐cm diameter and 25‐cm deep black polyethylene nursery bags on 10 November 2010 and allowed to establish. Seedlings were irrigated regularly during the dry season with water from the Mana River.
The experiment was laid out in a randomized block design. On 6 January 2011, each seedling in its bag was placed on a plastic plate and these arranged on benches raised 0.7 m above ground in the shade house (Fig. S1). Between 5 and 12 April 2011, surviving seedlings, now 7.5 months old, were sorted according to size and arranged into four blocks, with block 1 having the largest seedlings and block 4 the smallest ones. The basic experimental unit for the treatments consisted of 16 seedlings, replicated four times to give a total of 64 seedlings per species, and 128 seedlings for the two species in each of the four blocks. Initial size was recorded in terms of seedling height and leaf and branch numbers before applying the treatments.
The treatments consisted of two factors, potassium (K) and magnesium (Mg), each at four increasing levels (L1 to L4) in a crossed structure. Potash as the source of K was obtained from the local market, while kieserite as the source of Mg was obtained from a commercial company (Yara Cameroon), and both put through quality control testing at the Universities of Dschang and Bern. Impurity loads in the samples were negligible. The amounts to be applied were calculated from the concentrations of the fertilizers as follows. The proportion of K2O in potash was 50.11%, and accordingly the levels of K applied were: (1) no fertilizer; (2) 5 g potash > 2.08 g K (low); (3) 10 g potash > 4.16 g K (intermediate); and (4) 15 g potash > = 6.24 g K (high). The proportion of MgO in kieserite was 27.65%, and likewise the levels of Mg applied were: (1) no fertilizer; (2) 5 g kieserite > 0.83 g Mg (low); (3) 10 g kieserite > 1.68 g Mg (intermediate); and (4) 15 g kieserite > 2.49 g Mg (high). The larger range in amounts of K compared with Mg applied was done to reflect the relatively 2‐ to 3‐fold higher available concentrations of K to Mg in organic matter/top mineral soil at the P‐plot and Isangele Road (see later Results). The seedlings were numbered from 1 to 256 for each species and the treatments allocated at random within blocks. Fertilizers were spread dry on the surface of each pot, making sure that they did not touch the stems of seedlings, and watered in well. Two equal rounds of fertilizer application were made in exactly the same manner, one on 12 April 2011, and the other on 18 January 2012.
Estimates of solar radiation were available from the PAMOL meteorological station at Bulu, 4 km from Mana Bridge. Due to a failure of the Gunn–Bellani radiometer, relevant data were available only from 30 May 2011 to the end of the experiment. Estimates for 4 April 2011 (day prior to start of experiment) and up to this date in May were achieved by substituting averages of the matching daily values of 2006–08.
Plant and soil measurements
From 20 April 2011, seedlings were measured at approximately monthly intervals, at which times pots were randomly relocated within blocks: on the 19 occasions (the 9th, 14th, and last were just before the harvests), plant height, leaf number, and branch number were recorded for each survivor. Later at harvests 2 and 3, basal stem diameter (just above ground, point paint‐marked) and leaf area were measured. The three harvests were on 10–17 January 2012 (H1), 3–10 July 2012 (H2), and 2–14 December 2012 (H3), each marking the end of a growth phase. Some seedlings suffered a shock in terms of sudden temporary leaf shedding 1 month after the first fertilizer application.
At each harvest, 64 seedlings per species were randomly selected such that one replicate seedling per treatment was taken from each block. Leaves were removed and placed in paper bags. A soil sample was taken from the upper and lower layers of each pot at harvests 1 and 2. Soil samples were later air‐dried and sieved (2‐mm mesh) for chemical analysis at Bern. Each pot was then left in water for about 10 min and the soil carefully washed from the roots of seedlings. Roots of Microberlinia were visually scored for ectomycorrhizal abundance by estimating the proportion of root tips colonized; for Tetraberlinia this was not possible because, unlike on Microberlinia, the fungal sheaths are much less obvious without a microscope. Washed seedlings were separated into roots and stems, and bagged.
Plant samples from the first harvest were oven‐dried in Mundemba (65°C for 72 h) before transport to the University of Buea, redried, and weighed (Ohaus, electronic balance; ±0.01 g). Second‐ and third‐harvest samples were treated in similar manner, except that they were transported fresh to Buea and their leaf areas measured (Delta‐T, Cambridge, UK) before drying. All leaf samples were later milled, as were roots and stems from just the second harvest, and in Bern, 300 mg each was digested in a 2.5‐mL mixture of selenium, sulphuric acid, and salicylic acid, and analyzed for total Ca, K, and Mg using the Inductively Coupled Plasma Optical Emission Spectrometer (ICP – OES; model Optima 7000DV), and total N and P on a Continuous Flow Optical‐Absorption Spectrometer (CF‐OAP; Skalar Scan+). Soil samples were also oven‐dried (65°C overnight), extracted in 1M ammonium acetate, filtered, and analyzed for the three cations in the same way as the plant materials.
Statistical analysis
A principal component analysis (PCA) of initial height and leaf number provided a starting size covariate. Counts of leaf number (lvn t) in growth phase 1 were used to form a measure of leaf loss, or ‘seedling shock’. This shock covariate was defined as:
where lvn x is leaf number at time x. Strongly, or severely, affected seedlings were those for which shock was, respectively, ≥ 0.5 yet <1.0, or equal to 1.0. The 4‐month period integrated any shock intensification and/or recovery.
Growth measurements (height, leaf number, stem diameter) within the three phases did not require transformation and were subject to repeated measures analysis of variance (REM‐ANOVA), for each species separately, using GenStat version 16 (Payne et al. 2011). Factorial ANOVA (species separately again) was used to analyze harvest dry mass (ln‐transformed) with and without starting size and shock covariates individually. Just one plant of Microberlinia died and was irreplaceable by harvest 3; any lost replicates could normally be substituted from the extra quarter of plants that remained not harvested by the end of the experiment. As the first covariate had scarcely any impact on the results for either species, but the second one often did, so this shock one was retained for all ANOVAs. Factorial ANOVA was also applied to leaf nutrient concentrations (ln‐transformed), but only for stem and root nutrients from harvest 2. There were no obviously outlying values for dry weights or plant nutrient concentrations. For the soil nutrient concentrations (again ln‐transformed), data for upper and lower layers were analyzed separately because they were not statistically independent. Here there were a few very high concentrations, likely due to contamination, and these were treated as missing (four K and Ca in Microberlinia, and four K in Tetraberlinia, pots; >4‐fold their means). Least significant differences between means (P = 0.05) enabled treatment comparisons.
Results
Growth responses
Over the course of the experiment, radiation changed according to the normal seasonal cycle at Korup (Fig. 1A), so that the start and end of seedling growth would have followed the same annual pattern that wildings in the forest would have experienced, albeit in the latter case at lower levels on average than in the nursery (Green and Newbery 2001b). Period 1 therefore spanned a first wet season with its typical steep drop in radiation in August–September, period 2 a dry season with a peak in December, and period 3 again a wet season (Fig. 1A). Averaging daily values for the individual time intervals corresponding to the 19 nondestructive measurements, means (±SD) of radiation for periods 1, 2, and 3 were 140.7 ± 25.0 (n = 9), 165.1 ± 16.3 (n = 5), and 121.2 ± 24.7 (n = 5), respectively. Thus, between harvests 2 and 3, the seedlings experienced a substantial 26.6% fall in radiation.
Whilst height and branch number continued to rise steadily until the time of harvest 3 (Fig. 1B and D), leaf number for Microberlinia decreased after harvest 1 (in periods 2 and 3), and for Tetraberlinia it became constant after midway between harvests 1 and 2 (within period 2, Fig. 1C). These trends are based on the 50% of plants (i.e., two out of the four replicates) that were left to grow to the end of the experiment. Tetraberlinia attained greater height and had more leaves than Microberlinia, although it branched less (Fig. 1B–D). The shock effect is well evident at the second date from the temporary drop in leaf numbers on Microberlinia (Fig. 1C): had this not occurred, leaf numbers for both species would probably have been very similar up to harvest 1. Even so, the later decline in leaf number for Microberlinia, as well as its lessening of height growth and branching rates, actually began when radiation was at its highest (Fig. 1A). Using independently sampled seedlings, dry mass continued to increase significantly, although leaf number and area decreased between harvests 2 and 3, in contrast to Tetraberlinia, which later increased leaf area despite little change in its leaf number. Mean ectomycorrhizal score across the 16 treatments was 23% (range 13–38%), significantly higher in the control than for K addition (P < 0.01), but unaffected by Mg application and harvest (P > 0.05).
Of the 256 Microberlinia seedlings, 30 (11.7%) suffered strong shock, 27 (10.5%) were severely shocked, and four (1.6%) died as a consequence. By comparison, only six (2.3%) Tetraberlinia seedlings suffered strong shock, of which one (0.4%) was severely shocked and three (1.2%) died. Of these shocked Microberlinia and Tetraberlinia seedlings, 92 and 90%, respectively, had received K‐addition levels 3 and 4. Shock values for Microberlinia increased significantly with increasing K level (P < 0.001), but showed only a weak decrease with Mg level (P = 0.36). For Tetraberlinia, no significant trend was apparent for either factor.
Microberlinia seedlings treated with fertilizer (L2–L4) performed better than control (L1) seedlings in all growth parameters and during all growth phases. Repeated measures ANOVA showed that seedlings of this species with Mg application had highly significant increases in height, leaf number, and stem diameter. K application, however, produced only marginally significant increases (Table S1). Tetraberlinia seedlings with Mg application showed improved growth compared with controls, but significantly so only for diameter, whilst K application resulted in growth reductions, again only significantly for diameter (Table S1). Interactions between K and Mg rarely produced significant differences for growth of either species. Average leaf area per leaf for Microberlinia was only marginally higher at Mg level 3 than the control (P < 0.05) and showed no differences regarding K addition; Tetraberlinia showed no effects of Mg and K as factors (P > 0.05).
Dry mass responses
For Microberlinia, seedlings with Mg addition produced highly significantly more dry matter (DM) in total and per plant part than the controls (L1): the differences were most noticeable for the first application level (L2) vs. the control (L1), compared with the relatively smaller increases caused by higher applications (L2 to L3/L4). With K‐treated seedlings, only the stem (DMS) and total dry masses (DMT) were marginally significantly higher than control seedlings (Table 1). For Tetraberlinia, Mg application resulted in relatively small effects on dry mass, with weakly significant increases in roots (DMR) and total dry mass only. By contrast, Tetraberlinia seedlings with K application showed barely any effect on leaf dry mass and decreases in stem, root, and total dry mass (Table 1). Both species increased dry mass highly significantly with time, especially between harvests 1 and 2, but leaf dry mass (DML) decreased for Microberlinia and stabilized for Tetraberlinia at the third harvest. Interactions between K and Mg resulted in very few, and then only marginally, significant effects on dry mass.
Table 1.
Factor | Level | Microberlinia | Tetraberlinia | ||||||
---|---|---|---|---|---|---|---|---|---|
DML | DMS | DMR | DMT | DML | DMS | DMR | DMT | ||
K | 1 | 5.29b | 9.40b | 9.22a | 24.24b | 13.71a′ | 18.60a | 15.39a | 48.18a |
2 | 5.52ab | 10.54ab | 9.86ab | 26.26ab | 13.83a′ | 17.55a | 14.45ab | 46.34ab | |
3 | 5.98a | 11.83a | 10.55a | 28.73a | 13.07ab′ | 15.58b | 13.30b | 42.44bc | |
4 | 5.96a | 11.07a | 10.41ab | 27.72a | 12.52b′ | 14.70b | 13.41b | 40.98c | |
Mg | 1 | 4.99b | 8.22b | 8.51b | 21.89b | 12.55a | 15.04b | 12.86b′ | 40.85b |
2 | 5.73a | 11.29a | 10.36a | 27.74a | 13.34a | 17.20a | 14.73a′ | 45.79a | |
3 | 6.24a | 12.00a | 10.94a | 29.58a | 13.77a | 17.46a | 14.79a′ | 46.43a | |
4 | 5.84a | 11.65a | 10.36a | 28.20a | 13.41a | 16.54ab | 14.17ab′ | 44.66ab | |
Harvest | 1 | 4.63b | 5.94c | 6.20c | 16.84c | 10.45b | 10.01c | 9.21c | 29.82c |
2 | 6.47a | 12.88b | 11.39b | 30.97b | 14.53a | 17.69b | 15.32b | 47.85b | |
3 | 6.12a | 15.89a | 14.13a | 36.45a | 15.38a | 25.51a | 19.95a | 61.25a | |
F‐values | K | 1.71ns | 3.71* | 1.56ns | 2.68* | 2.04ns | 7.37*** | 3.68* | 5.27** |
Mg | 8.05*** | 15.35*** | 7.06*** | 12.07*** | 1.52ns | 2.59o | 3.04* | 2.88* | |
Harvest | 38.6*** | 176.2*** | 139.5*** | 145.6* | 57.3*** | 178.9*** | 152.5*** | 159.0*** | |
NIntS | 1 | 1 | 0 | 1 | 0 | 0 | 0 | 0 |
Means that do not share the same superscripted small letters among levels of the same factor are significantly different (P ≤ 0.05). The ′‐marks to sets of letters indicate that differences are strictly insufficient as P(F) was > 0.05. [Error df: Mb, 137; Tb, 140.] Significance levels, P(F): ***≤0.001; **≤0.01; *0.05; o≤0.10; ns >0.10.
For any particular growth variable, each of the mean responses to the 16 treatment combinations (over the three harvests) could be related to the control as a percentage change (perch = {DM [i,j] / DM [1,1]} × 100, where i and j are levels of K and Mg factors, respectively). These means were the back‐transformed values from ANOVAs that incorporated shock as a covariate (i.e., they were different from means of untransformed and unadjusted means). Figure 2 highlights the marked difference between Microberlinia and Tetraberlinia, the former's response being much stronger than the latter for leaf and total dry mass, and with similar patterns for root and stem parts (Fig. S2). A large portion of the change was between L1 and L2, especially for Mg. Highest levels of application led to growth reductions, with maxima around L3 for both K and Mg. Tetraberlinia responded weakly to Mg, and barely to K, addition: Microberlinia responded strongly to Mg and partially to K addition, suggesting that only Microberlinia was Mg‐limited, and its positive response to Mg enabled it to respond further to the added K, that is, once Mg limitation was released, K limitation came into play.
The mean proportion of dry mass allocated to roots (DMR/DMT) was 0.376 for Microberlinia (root–shoot ratio, (DMR / [DML + DMS]) = 0.609) and correspondingly 0.320 (0.475) for Tetraberlinia. Only for Microberlinia across levels of Mg addition did the proportion alter with treatment, and as a significant decrease (0.390 to 0.369, L1 to L4; P < 0.05). Between harvests 1 and 3, the ratio did increase slightly (Microberlinia: 0.370 to 0.389, P < 0.001; Tetraberlinia 0.310 to 0.328, P < 0.05). Leaf mass–area and height–diameter ratios were unaffected by the treatments (P > 0.05). The effects of Mg and K addition on dry mass allocation were therefore very small for these two tree species' seedlings.
Nutrient responses
Increasing levels of K significantly raised concentrations on K in the leaves of both Microberlinia and Tetraberlinia, again largely due to a difference between the control (L1) and the first addition level (L2), and likewise and even stronger was the effect of Mg addition on the concentration of leaf Mg (Table 2). However, added K led to decreases in leaf Mg concentration in both species, significantly for Tetraberlinia but less so for Microberlinia. Concentrations of Ca significantly decreased, respectively increased, with raised additions of K and Mg, in both species, whilst N concentration did not differ significantly across treatments for either species (Table 2). More marked was that K addition led to significant increases in leaf P concentration in both species too. As with the results for growth and dry mass responses, interactions between K and Mg were rarely or only weakly significant for concentrations, except for K addition on Tetraberlinia. For all elements and both species, leaf concentrations decreased over successive harvests (Table 2).
Table 2.
Factor | Level | Microberlinia | Tetraberlinia | ||||||||
---|---|---|---|---|---|---|---|---|---|---|---|
Ca | K | Mg | N | P | Ca | K | Mg | N | P | ||
K | 1 | 7.29a | 5.73c | 4.78a′ | 19.29a | 0.849b | 5.47a | 3.75c | 2.66a | 14.70a | 0.648b |
2 | 6.49b | 7.55b | 4.69ab′ | 19.40a | 0.850b | 4.55b | 5.48b | 2.16b | 14.73a | 0.655b | |
3 | 5.90c | 8.40ab | 4.70ab′ | 19.22a | 0.918b | 4.51b | 6.50a | 1.77c | 14.91a | 0.715a | |
4 | 6.08bc | 8.85a | 4.58b′ | 19.65a | 1.017a | 4.53b | 6.44a | 1.98bc | 15.26a | 0.730a | |
Mg | 1 | 5.65c | 10.20a | 1.41c | 20.74a | 0.992a | 4.24c | 5.94a | 0.99c | 14.95a | 0.698a |
2 | 6.42b | 6.89b | 6.19b | 19.10b | 0.853b | 4.50bc | 5.38b | 2.47b | 14.83a | 0.675a | |
3 | 6.51b | 6.90b | 7.41a | 18.92b | 0.901b | 4.89b | 5.13b | 2.73ab | 15.07a | 0.685a | |
4 | 7.19a | 6.63b | 7.45a | 18.86b | 0.882b | 5.45a | 5.25b | 3.00a | 14.74a | 0.687a | |
Harvest | 1 | 7.69a | 9.11a | 5.29a | 22.52a | 1.065a | 5.76a | 6.35a | 2.22a | 17.74a | 0.884a |
2 | 6.44b | 7.03b | 4.58ab | 18.24b | 0.792c | 4.36b | 5.31b | 2.12ab | 14.15b | 0.621b | |
3 | 5.34c | 6.65b | 4.24b | 17.74c | 0.880b | 4.26b | 4.72c | 2.01b | 13.18c | 0.588b | |
F‐value | K | 6.66*** | 15.49*** | 0.38ns | 0.27ns | 2.76* | 8.01*** | 94.96*** | 18.38*** | 1.37ns | 5.69*** |
Mg | 10.91*** | 31.87*** | 172.17*** | 5.55*** | 3.98** | 10.72*** | 5.86** | 162.41*** | 0.43ns | 0.26ns | |
Harvest | 49.1*** | 30.0*** | 4.3* | 66.9*** | 31.2*** | 33.9*** | 41.7*** | 2.1ns | 144.2*** | 98.0*** | |
NIntS | 1 | 2 | 2 | 0 | 0 | 2 | 3 | 2 | 0 | 1 |
Means that do not share the same superscripted small letters among levels of the same factor are significantly different (P ≤ 0.05).The ′‐marks to sets of letters indicate that differences are strictly insufficient as P(F) was > 0.05. [Error df: Mb, 129; Tb, 133.] Significance levels, P(F): ***≤0.001; **≤0.01; *0.05; o≤0.10; ns >0.10.
Addition of K and Mg had corresponding effects of significantly increasing K and Mg concentrations, respectively, also in roots and stems of both species (harvest 2, Tables S2a, b), but there were hardly any other significant effects of these additions on concentrations of the other elements, besides K addition increasing P concentrations in both species (three of four cases at P ≤ 0.05). Mg addition significantly increased concentrations of Ca in roots of both species, however (Table S2b). As with leaves, the main differences were between the controls (L1) and first addition levels (L2). At harvest 2 – by then seedlings were almost completely free of shock effects – grouping into those primary (Fig. 3) and those secondary (Fig. S3) indicated how across the 16 treatments, Mg and K concentrations were varying far less than in the leaves, although still largely being correlated positively with trends in the latter. The higher levels of K addition led to rather smooth or similar sets of responses in their K and Mg concentrations for Microberlinia plant parts, although in comparison responses were less consistent for Tetraberlinia (Fig. 3). By contrast, Mg addition resulted in clearer, more pronounced, changes in both elements, especially for the leaves of Microberlinia. For instance, where Mg was added with K, this led to sustained high concentrations of Mg, but not of K, for Microberlinia at the higher treatment combinations (Fig. S3, secondary treatments). This was not quite the case for Tetraberlinia, with Mg concentrations decreasing when combined with K addition, and conversely for this species added Mg sustained the high K concentrations. Although interactions were not always strong, there is some evidence of a reciprocal effect: K enhancing Mg for Microberlinia and vice versa for Tetraberlinia.
Differences in Ca were likewise better structured for Microberlinia than Tetraberlinia (Fig. S4A), yet barely existing for N and P, for either species (Fig. S4B and C). However, a clear difference between N and P vs. K, Mg, and Ca was that the former group had higher concentrations in roots than stems, and these were closer to corresponding leaf concentrations, than did the latter group. For Tetraberlinia, the closest leaf, root, and stem concentrations occurred for P at the higher levels of K and Mg addition, pointing to K perhaps aiding P uptake for this species, which was not the case for Microberlinia. Percent changes in K and Mg concentrations in leaves were also very different between species, suggesting further a reciprocal pattern of response with Microberlinia taking up (and responding to) more Mg as it was applied and responding less to K; and Tetraberlinia responding more to K addition and less to Mg (Fig. 4). Percentage changes in Ca, N, and P were much less well defined with respect to K and Mg additions (Fig. S5).
Soil–seedling relationships
Additions of K and Mg as treatments had the expected effects on the available concentrations of these elements in the pot soils (Tables S3a, b). For K addition, pot concentrations were approximately linearly related to the amounts added, and for Mg addition, these were more convexly curvilinear (the change from control [L1] to first level added [L2], being greater than L2 to L3/L4). The second fertilizer application must clearly have raised the concentrations in the pots considerably at harvest 2 for this to be reflected in leaf concentrations. In the upper parts of the pots, Ca concentrations increased with application levels for both species, but significantly so only when Mg was added. The lower parts of the pots showed the opposite effect for Mg addition. Nevertheless, Mg addition also decreased soil K concentrations for both species in both upper and lower soils. The effect of K addition on Mg concentration was seemingly complex due to many interactions between the main factors, species, and pot parts: for Microberlinia, it moderately increased Mg in the upper soil, but in Tetraberlinia, it strongly decreased it in the lower soils (Tables S3a, b). The response surfaces showed how Mg addition affected less the K levels as K addition affected the Mg levels (Fig. S6A and B).
Means of upper‐ and lower‐layer concentrations of K and Mg in pot soils were significantly positively (and linearly) dependent on the level of fertilizer applied for both species by harvest 1 (P < 0.001), confirming the efficacy of the treatments overall with slopes of 11.9 and 11.6 μg/g K for Microberlinia and Tetraberlinia, respectively, and correspondingly 19.1 and 23.2 μg/g Mg. As each incremented level of addition was equal to 2.08 ga K and 0.83 ga Mg per pot (start to harvest 1; ga means g‐applied), then averaging over species' pot concentrations, the treatment efficacy was 5.65 μg/g/ga K and 51.0 μg/g/ga Mg. Thus, Mg was made much more available than K in the soil for the seedlings. Furthermore, regressions had very different slopes for K depending on whether upper or lower pot soils were considered, with the slopes of 2.80 and 3.39 μg/g, for Microberlinia and Tetraberlinia, respectively, for upper soils; and 21.1 and 19.8 μg/g for lower ones. By contrast, the slopes for Mg were closer between layers with corresponding values 14.6 and 16.9, and 23.5 and 29.4 μg/g. Concentrations across blocks were consistent for each element. These results indicate that strong leaching occurred down the pot profile for K, and moderate leaching for Mg.
Generalized linear model fits for Microberlinia total seedling dry mass (DMT) at harvest 1 against K and Mg level number (L1‐L4, i.e., exactly linearly related to the application rates) were slightly better for Mg (Mg, P = 0.025; K, P = 0.84) than when the actual mean pot concentrations were used as independent variables (Mg, P = 0.054; K, P = 0.40). And in a similar way K fits were better too with the original level numbers (K, P = 0.004; Mg, P = 0.096) than the actual concentrations (K, P = 0.049; Mg, P = 0.12). Thus, whilst confirming the main results of analyses of variance based on levels applied, more detailed knowledge of the pot concentrations led to weaker rejection of the key null hypotheses (Mg effect for Microberlinia, K effect for Tetraberlinia).
Concentrations of K and Mg in leaves were strongly and significantly positively correlated with those in roots and shoots for both species, and likewise with the corresponding pot concentrations (Table 3). For Ca, N, and P, correlations were far weaker and mostly not significant. Total dry mass (DMT) correlated negatively with leaf K (significantly for Tetraberlinia, P < 0.01; not for Microberlinia), strongly positively with leaf Mg (P < 0.001, both species significant), but weakly and marginally with Ca, N, and P concentrations (P < 0.10). Usually K, P, and N were positively intercorrelated as were K, Ca, and Mg (Table 3), although more essential was that Mg and N were strongly and significantly negatively correlated for Microberlinia yet not for Tetraberlinia.
Table 3.
L vs. S | L vs. R | L vs. DMT | L vs. SoilU | L vs. SoilL | L vs. L | ||||
---|---|---|---|---|---|---|---|---|---|
Mb | K | Mg | Ca | N | |||||
K | 0.837*** | 0.806*** | −0.290ns | 0.855*** | 0.762*** | ||||
Mg | 0.986*** | 0.963*** | 0.816*** | 0.930*** | 0.958*** | −0.701** | |||
Ca | −0.047ns | −0.379ns | 0.186ns | 0.448o | −0.182ns | −0.886*** | 0.630** | ||
N | −0.003ns | 0.365ns | −0.582* | – | – | 0.667** | −0.777*** | −0.582* | |
P | 0.605* | 0.406ns | −0.124ns | – | – | 0.758*** | −0.454o | −0.675** | 0.568* |
Tb | |||||||||
K | 0.850*** | 0.910*** | −0.668** | 0.862*** | 0.968*** | ||||
Mg | 0.968*** | 0.919*** | 0.646** | 0.872*** | 0.953*** | −0.508* | |||
Ca | 0.208ns | −0.316ns | 0.489o | 0.149ns | −0.211ns | −0.716** | 0.683** | ||
N | 0.142ns | 0.236ns | −0.226ns | – | – | 0.464o | −0.128ns | −0.278ns | |
P | 0.793*** | 0.590* | −0.442o | – | – | 0.703** | −0.307ns | −0.402ns | 0.681** |
***P ≤ 0.001; **P ≤ 0.01; *P ≤ 0.05; o P ≤ 0.1; ns P > 0.1.
Mean pot concentrations across species in controls (L1) at harvest 1 were 15.6 μg/g K and 9.4 μg/g Mg, and raising each to addition level 1 (L2) resulted in 44.7 μg/g K and 44.3 μg/g Mg. In the preparation of the pot medium, the top 6 cm of soil at Isangele Road had been taken and mixed. In separate soil sampling for two related experiments performed in March 2012, one at Isangele Road and the other in main P‐plot in Korup, the top 6 cm had weighted mean available concentrations of 44.4 and 45.8 μg/g K and 21.2 and 25.4 μg/g Mg. This means that by harvest 1, plants in the controls had depleted the available K and Mg concentrations, and level 1 addition had reinstated it for K but overstated it for Mg.
Discussion
Nutrient levels and demands
Experiments of a similar type elsewhere in the tropics for primary forests are very few and far between, and only two by Burslem et al. (1995, 1996) added Mg as one of their single treatments to a native soil. In a third experiment by Gunatilleke et al. (1997), Mg was added too but to a non‐native soil and factors Mg and P were partially confounded. In the experiment of Turner et al. (1993), K was part of a general NPK treatment and therefore its effect not readily separable from that of P and N, although in two other studies K was added singly (Nilus et al. 2011; Santiago et al. 2012). Nutrient supply to seedlings of very different species, from Sri Lanka, SE Asia, and Central America, is unlikely to be of too much ecological relevance for the very different species and soils at Korup though. Because of the widely assumed but unfounded notion of nutrients being nonlimiting for tropical rain forest tree seedlings, although possibly limiting tree growth (Wright et al. 2011 for K in particular), it is perhaps not surprising that there are only just two studies published for Mg, and so very few others involving K. Further reported experiments compared different soils and their nutrient levels on seedling growth using correlative approaches (e.g., Juliana et al. 2009; Holste et al. 2011), but these at best can only be indicative.
Whilst seedlings of Microberlinia and Tetraberlinia grown in the control Korup soils appear to have been differentially limited in their growth by Mg and K supply, they were not severely deficient in either element. This is evidenced by the absence of characteristic leaf deficiency symptoms, especially the chlorotic leaf tissues characteristic of plants with very low Mg or necrosis at leaf tips and edges when K is critically low (Marschner 1995; Barker and Pilbeam 2007), and by the fact that very few plants died during the experimental period, even among the controls. Furthermore, there was little experimental evidence of large changes in R/S ratio (c. 5% only for Microberlinia) with increasing supply of Mg and K, a phenomenon shown repeatedly for herbaceous and crop plants, although only when the elemental levels were very severely reduced (Hermans et al. 2005, 2006). There was no evidence of fungal attack, which is often associated with a deficiency of K (Marschner 1995). Nevertheless, some Microberlinia seedlings did lose leaflets across all treatments over time, and this loss was usually proceeded by a yellowing of the leaves: the analysis of mean individual LA per plant did not suggest any linkage with control vs. additions though. Deficiencies may have been obscured on some plants accordingly and gone unrecorded because individual leaflets are so small.
For 21 tree species' values taken from the extensive tabulation of Merhaut (2007), mean minima and mean maxima Mg concentrations defined diagnostically as being ‘sufficient’ in leaves (with SEs and ranges) were 1.86 ± 0.15 mg/g (0.9–3.5) and 7.09 ± 0.51 mg/g (3.6–12.0). The two species' values in Table 2 sit well within this range except for the controls (Mg L1) being both definitely lower, and on this basis can be labeled ‘insufficient’. More general data for K suggested that typically sufficient concentrations lie in the ranges 6–10 mg/g for conifers, 11–20 mg/g for fruit trees, and 12–15 mg/g for broad‐leaf trees (all temperate; Mengel 2007). In this respect, all values in Table 3 are low, even though the concentrations were close to the ranges for other Korup experiments and no strong effect of added K was found. Are rain forest tree seedlings inherently low in K? Burslem et al. (1996) and Nilus et al. (2011) reported K leaf concentrations in the range 10–15 mg/g for nursery seedlings of five rainforests tree species, which points to the situation in Korup being rather special with wildings and out‐plants reaching just 10 mg/g K (Table 4). In an extensive 8‐year field experiment in Panama investigating limitations of N, P, and K, Santiago et al. (2012) found that adding K had a small but significant effect on in situ seedling growth of five understory species. Concentrations of leaf K and Mg ranged from 3.96 to 35.16 mg/g and 0.77 to 8.41 mg/g, respectively (L. Santiago, pers. comm.).
Table 4.
K | Mg | |||||||
---|---|---|---|---|---|---|---|---|
Mb | (%) | Tb | (%) | Mb | (%) | Tb | (%) | |
This experiment – Control | 6.71 | 82 | 3.55 | 47 | 1.45 | 45 | 1.31 | 68 |
L1 | 9.96 | 121 | 6.42 | 85 | 5.38 | 168 | 3.32 | 172 |
L3 | 13.32 | 162 | 7.34 | 97 | 8.01 | 250 | 3.46 | 179 |
Other studies: | ||||||||
Light quantity triala | 5.91 | 7.24 | 2.57 | 2.24 | ||||
Transplants – P‐plotb | 9.55 | 8.13 | 2.56 | 1.77 | ||||
P‐fertilization trialb | 3.90 | – | 3.11 | – | ||||
Wildings in P‐plotc | 10.99 | – | 4.19 | – | ||||
Herbivory trialc | 9.78 | 7.32 | 3.99 | 1.78 | ||||
Nursery out‐plantsd | 9.04 | – | 2.86 | – | ||||
Average, others | 8.20 | 7.56 | 3.21 | 1.93 |
The comparison with leaf concentrations in other Korup studies, experimental and field, indicated that Mg (in controls, L1) was suboptimal for both Microberlinia and Tetraberlinia, rising toward field levels under Mg addition, whilst for K there was no clear case of suboptimality for Microberlinia (concentrations on par with other experiments and field studies), although for Tetraberlinia there was a stronger difference (Table 4). This comparison suggests that Microberlinia is strongly Mg‐ but not K‐limited, and Tetraberlinia neither K‐ nor Mg‐limited, in the Korup soil. But it must be remembered that the seedlings in the present experiment, although using freshly collected soils from the forest, were, as in all such similar local nursery ones, growing ex situ. The shock resulting from the first addition of the higher levels of K for Microberlinia, but not Tetraberlinia, was most pronounced among blocks with the smaller seedlings. The phenomenon can be explained by Microberlinia tending to have more fine roots near the soil surface than Tetraberlinia (G. Neba, pers. obs.), and thus the temporarily high K concentrations in the top 1–2 cm of the pots would probably have invoked a strong local osmotic effect after first watering.
Response physiology: K and Mg
The addition of Mg had significant effects on the growth and dry mass in both species. Seedlings that received additions of this element grew better in terms of height, diameter, and leaf number than those without it. They produced correspondingly larger leaf areas and more dry matter for the different parts than control seedlings. The effects of Mg on Microberlinia were far more pronounced than on Tetraberlinia: for both species different plant parts changed in similar proportions. It can be concluded that Mg was limiting nursery growth in Microberlinia, and probably does so too in the forest. In a similar way, Tetraberlinia appears not to be K‐limited. Nevertheless, a proviso is needed because the K leaf concentrations in Microberlinia and Tetraberlinia at Korup are relatively low; and so it is curious that adding plenty of K experimentally did not raise them much higher. Interestingly, mature canopy leaves of Microberlinia and Tetraberlinia also had relatively low K concentrations of 5.91 and 4.23 mg/g, respectively (Chuyong et al. 2000).
Mg addition has been shown generally to increase chlorophyll content, phloem loading, and transport of photosynthates to sink sites and thus affect productivity (Marschner 1995). In the herbaceous crop plants Phaseolus vulgaris and Beta vulgaris, transport of sucrose out of leaves can be restricted under severe Mg‐deficiency (Cakmak et al. 1994a,b), leading to accumulations fourfold those of Mg‐sufficient leaves (Hermans et al. 2004, 2005). Strong Mg‐deficiency can inhibit root development, especially fine root growth (Marschner 1995; Ericsson and Kahr 1995; for Betula pendula; McDonald et al. 1996; for Alnus incana; Hermans et al. 2006; review). Given that Mg was most likely not so severely deficient in the present experiment, the most obvious role for it was building chlorophyll a and b, and hence improving the rate of photosynthesis (Laing et al. 2000 for Pinus radiata; Mehne‐Jakobs 1995, 1996 for Picea abies; Yang et al. 2012; for Citrus spp.; Cakmak and Kirkby 2008; review). Mg bound to H+‐ATPase also effects several plasma‐membrane processes, is a constituent of many protein‐building enzymes, and is further involved in photosynthetic reactions (Epstein and Bloom 2005; Yang et al. 2007;). Despite the known role of K in stomatal regulation, osmotic potential in the vacuoles, and translocation physiology, it is not so directly involved in photosynthesis (Marschner 1995). These findings are largely for temperate herbaceous and woody (mostly conifer) plants, and whilst investigations on tropical tree seedling physiology regarding K and Mg are almost entirely lacking, the basic plant physiology is expected to be generally applicable.
Nutrient limitation in seedlings was indicated by nutrient concentrations in the various plant parts, especially leaves (Marschner 1995), and by percentage change in concentration across addition levels from the control to the treatment showing the highest plant dry mass. The mean percentage changes (perch) of 526 and 276% at Mg level 3 (2nd addition level; Tables 1 & 2) in leaf Mg concentration for Microberlinia and Tetraberlinia, respectively, support the idea that Mg was causing the increases in dry mass with lower additions, effects being much stronger for Microberlinia than Tetraberlinia (Fig. 4), but later inevitably some other factor would be limiting growth when Mg came into luxury supply. Increasing K addition had little further influence for either species' change in Mg concentration. Very differently, however, at this Mg level leading to the maximum seedling mass, increasing K addition had barely any effect on K leaf concentrations for Microberlinia, whilst for Tetraberlinia increasing it did increase K concentrations (Fig. 4). One interpretation might be that Microberlinia is not K‐limited when Mg is sufficiently or optimally available, whilst Tetraberlinia is apparently moderately Mg‐limited when K is sufficiently or optimally available. This emphasizes a basic set of reciprocal responses by the two species, to additions of Mg and K, as a complex and interesting nonlinear asymmetrical form of interaction. Moreover, there is no strong evidence in this experiment for ionic antagonism between K and Mg as demonstrated by Sun and Payn (1999) for Pinus radiata and Ding et al. (2006) for Oryza sativa. This was probably because there was no strong deficiency in either element, and this was shown too by the relative changes in their plant parts concentrations, as the other factor was increasingly applied, being very similar.
For Ca, N, and P, percentage change values of <100 showed that the fast growth induced by Mg addition used up and diluted the concentrations of these other elements. Such dilution effects also occurred as K addition was increased, although less strongly. This may also point to their limiting growth at the optimal level of Mg application, which was again stronger for Microberlinia than Tetraberlinia. Addition of small amounts of Ca, N, and P together with Mg at level 3 would be expected to further improve the growth response of Microberlinia, but not necessarily that of Tetraberlinia. For the present experiment, based on the intraleaf concentration (negative) correlations in Table 3, the sequences Mg ‐> N ‐> P for Microberlinia, and K ‐> Mg ‐> Ca for Tetraberlinia suggest the ordering of relevant limiting factors. The results here concur with Rubio et al. (2003) that trying to decide between a ‘law of the minimum’ sensu Liebig and a multiple limitation hypothesis is not too useful, and each element or factor should be examined individually for its effects and interactions with others, e. g., the complex interactions between Mg and K (then P).
Interactions with other elements
Although leaf P concentrations varied little across treatments in this K‐ and Mg‐addition experiment, they were lower for Microberlinia and Tetraberlinia, at 0.91 and 0.69 μg/g, respectively, than controls in the previous nursery and P‐addition trial (Green and Newbery 2001a; Newbery et al. 2002) and averages of the two out‐planting studies (Newbery et al. 2000; Green and Newbery 2001b) involving both species at Korup): four‐studies means of 1.66 μg/g (range 1.31–2.28 μg/g) and 1.20 μg/g (range 1.10–1.27 μg/g), respectively, that is, 55 and 58% the earlier values. Leaf N concentrations were also lower but less so: in the present experiment 19.4 and 14.9 μg/g for the two species, respectively, compared with four‐studies means of 24.2 (19.5–28.3) μg/g and 19.5 (15.6–22.4) μg/g; correspondingly 80% and 76%. This would suggest that P availability in the experiment was suboptimal and partially limiting to all plants, making the implied increase in uptake of P by increased additions of K for Microberlinia and Tetraberlinia (Table 4) especially interesting. Any P‐limitation was being partly mitigated by added K. Nevertheless, the two previous experiments that tested for P‐limitation directly (i.e., by adding P) found no evidence for it (Green and Newbery 2001a; Newbery et al. 2002).
Magnesium may have a different, possibly more important, effect on plant growth from being just a required nutrient. One adaptive mechanism to Al toxicity in acid soils is the release of organic acid anions from roots, and for this Mg is required (Yang et al. 2007; Bose et al. 2011; Brunner and Sperisen 2013). Organic acid anions chelate Al cations by forming nonphytotoxic Al‐organic acid complexes (Marschner 1995; Miyasaka et al. 2007). The tropical soils of Korup are sandy, leached, and acid (pH 4.0‐5.8; Gartlan et al. 1986) and almost certainly (although not, unfortunately, so far confirmed by measurement) high in Al (see Hawkins and Brunt 1965 for the region in general). The element Al competes more actively with Mg at root uptake sites and in metabolic processes than with K (and Ca), because the first two elements have much more similar radii than the others (Miyasaka et al. 2007). This means that interactions are more likely between Al and Mg, not between Al and K. So not only does Al lead to reduced uptake of Mg into plants and interferes with metabolism where Mg is involved, and some exudation of organic acids is induced by the Al alone as a tolerance mechanism by many species, the addition of Mg will raise organic acid production further, thereby ameliorating the toxicity and allowing sufficient uptake and utilization of Mg with the exclusion of Al in the soil. For Pinus radiata in New Zealand, Mitchell et al. (1999) not only showed that adding Mg fertilizer reduced canopy Mg‐deficiency symptoms but also lowered exchangeable soil Al concentrations. For tropical tree seedlings, Burslem et al. (1996) seem to have been the first to hint at a link between Mg and Al in acid soils, albeit for an Al‐accumulating species, Antidesma cuspidatum.
This subtle interplay between Al and Mg concentrations at the root surface may in part explain why the two species, Microberlinia especially, continued to grow well above Mg addition level 1 (L2), which would have removed its limitation as such. The high tissue concentrations of Mg with higher Mg additions were probably a reflection of the beneficial effects of removing the putative Al toxicity. It would suggest, as a competing hypothesis to Microberlinia being more Mg‐limited than Tetraberlinia, that Microberlinia is much more sensitive to Al toxicity than Tetraberlinia, and hence Mg availability both supplies and ameliorates. There is some evidence that ectomycorrhizas can aid Mg uptake by trees (Jentschke et al. 2000, 2001; for Picea abies) but whether they can ameliorate Al toxicity remains still inconclusive (Marschner 1995; Miyasaka et al. 2007). Ahonen‐Jonnarth et al. (2000) and Tahara et al. (2005) showed, however, that increased Al concentrations around roots (of Pinus sylvestris and P. densiflora) led to greater exudation of organic acids when seedlings were ectomycorrhizal as opposed to nonectomycorrhizal. In the present experiment, it appears that ectomycorrhizas, at least for Microberlinia, had a relatively small influence on treatment effects, and probably for Tetraberlinia too.
Ecological aspects: recruitment
As a plant‐growth study, nursery conditions allowed control of many other interacting factors that would occur in the forest (e.g., light level was fixed and the same across all treatments). More importantly, the influence of the ectomycorrhizal mat was excluded. Knowing the intrinsic physiological responses of the two tree species allows an assessment of processes that might be exacerbating or alleviating nutrient limitation in the field (e.g., soil leaching vs. mat retention and nutrient supply to seedlings, G. A. Neba, unpublished data). The experiment reveals only in part, but clearly reflects, the regeneration niches of the two species. Certainly, other factors will define their full niches in the field.
Microberlinia and Tetraberlinia responded quite differently to additions of K and Mg, suggesting that the former is relatively more Mg‐demanding and the latter more K‐demanding. Importantly, both were grown at moderately high light intensities in the Mana nursery, not the more common shady understorey conditions of the forest. A further caveat is that seedlings were already well established (>6 months old) when the treatments were first applied: possibly differences in response might have been larger had they been first treated earlier. Microberlinia is a very shade‐intolerant and strongly light‐responding species, whilst Tetraberlinia is shade‐tolerant and moderately light‐responding (Green and Newbery 2001a,b). Their differences in demands and responses may be simply a reflection of the basic physiologies, with Mg being primarily involved in photosynthesis in the light, K in storage and translocation in the shade. A more complex interpretation does not seem warranted at this stage. Whether both species are low‐K tolerant given their low tissue concentrations, the weak response to added K, and (besides being low‐P) the low K availability in the soil at Korup (Gartlan et al. 1986; Newbery et al. 1988, 1997), remains an open question.
If the K‐Mg availability ratio were to vary spatially in the forest, then a low value, coincident on a lighted area, would presumably be needed to enhance the chances of Microberlinia recruiting better than Tetraberlinia; or, conversely, if soil Mg concentrations can be shown to be very low around adult Microberlinia trees due to a high demand (Chuyong et al. 2000, 2002) for the element internally (to detoxify Al externally), then this limitation might in part explain the poor recruitment of Microberlinia seedlings in the Korup groves. Because Mg and K are both recycled via the mineralization of litterfall and canopy throughfall (Chuyong et al. 2002, 2004), species' growth responses to K and Mg need to be more closely linked in further studies to the relative nutrient inputs and availabilities in the soil. The reported experiment also demonstrates that, whilst it is difficult to completely understand how the causal nexus of interacting elemental concentrations affects tree seedling growth in the field, simplification under the more controlled conditions of a nursery does give valuable insights and new testable hypotheses about the mechanisms involved.
Data Accessibility
Data are available from the Dryad Digital Repository: http://dx.doi.org/10.5061/dryad.k7729.
Conflict of Interest
None declared.
Supporting information
Acknowledgments
We thank the Ministries of Forestry and Wildlife (MINFOF) and Scientific Research and Innovation (MINRESI) in Cameroon for research permission (to DMN), Conservators of Korup National Park, P. Ndongmo and F. Fotendong, for access permission; Pamol Plantations Plc for use of the Mana nursery site and long‐term cooperation over the Ndian meteorological station; Yara Cameroon for supplying the kieserite fertilizer gratis, R. Kometa for field and logistic support, S. Njibile and C. Ohka for assistance in the nursery, M. Zimmerman for nutrient analyses in Bern, J. M. Norghauer for commenting on an earlier manuscript draft, and three anonymous reviewers for their useful comments.
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Data Availability Statement
Data are available from the Dryad Digital Repository: http://dx.doi.org/10.5061/dryad.k7729.