1. Introduction
Mineral supplements for horses (
Equus caballus) usually include both, macro as well as trace elements. However, forage-based diets, which are common in horse feeding, already contain adequate levels of macro minerals, especially sufficient levels of calcium. According to the recommendation by the Committee for Requirement Standards of the Society of Nutrition Physiology (GfE) from 2014 [
1], the calcium requirement of a warmblood horse (bodyweight 600 kg, 25 to 36 months old) is 25.8 g per day. This amount is already covered by about 5.5 kg of hay, with an average calcium content in grass hay of 4.8 g per kg dry matter (variations from 1.6–19.4 g/kg DM were observed in hay samples from the years 2014 to 2019 in Germany) [
2]. In other types of hay, for example, clover or alfalfa hay, the calcium contents are even higher than those found in grass hay and reach mean concentrations of 15.7 g/kg DM [
3].
Reducing the macro-mineral supply might improve the utilisation of specific minerals, as high levels of calcium in the diet were reported to cause a secondary deficiency of trace elements [
4]. In horses, high dietary calcium negatively affected copper digestibility, whereas zinc digestibility was not influenced [
5]. In pigs (
Sus scrofa domesticus), carnivores and small ruminants, on the other hand, a secondary zinc deficiency due to high dietary calcium levels was observed [
3]. In addition, reduced serum magnesium concentrations were found in horses with increased calcium and phosphorus levels in the diet [
6]. In terms of the physiological calcium metabolism, horses differ from other mammalian species, as a dietary calcium excess is not only excreted with faeces but also via urine [
7]. This bears the risk of urinary stones with increased calcium levels in the feed [
8].
Basically, the supply level of minerals is reflected in the serum of horses, so blood tests provide a simple yet reliable criterion for assessment [
9]. However, the assessment of calcium supply via a blood test is only of limited value, since calcium levels in the blood are strictly regulated by endocrine mechanisms. In terms of insufficient calcium supply, parathyroid hormone (PTH) which is secreted by the parathyroid glands causes the release of calcium from the skeleton by stimulating osteoclastic bone resorption and leads to increased tubular reabsorption of calcium in the kidney. Furthermore, PTH stimulates the activation of vitamin D into its biologically active form calcitriol (1,25-dihydroxycholecalciferol), which in turn causes an increased intestinal calcium absorption [
10]. By means of balance studies, an exact determination of the intestinally absorbed calcium amount, as well as the renal calcium excretion, is possible. However, performing balance studies means enormous restrictions on the animals’ welfare. Nevertheless, to investigate the effects of different dietary calcium levels in more detail, bone markers can be used in order to monitor bone metabolism, which might be of interest, especially in growing animals. For this purpose, plasma levels of osteocalcin (OC) can provide information about bone formation as it is a synthesis product of osteoblasts and is produced during matrix formation [
11,
12]. In contrast, levels of C-terminal telopeptide (CTX-I) can give information about degradation processes [
13]. CTX-I fragments are released into the blood as degradation products of type I collagen during osteoclast-mediated bone resorption [
14].
The effects of different calcium contents in the diet of warmblood horses in the late growth phase (25- to 36-months-old) have been hardly researched. Our hypothesis is that high calcium excess might impair the utilisation of trace elements. To prove this theory, the effects on serum mineral status and bone metabolism in young stallions fed a hay- and oat-based diet were evaluated under conditions of either high or moderate calcium excess.
4. Discussion
As it is common practice to use mineral supplements in horse feeding, the aim of this study was to investigate the effects of different dietary calcium levels in young warmblood stallions under practical conditions. The investigations focused on whether reducing calcium supply offers an advantage over conventional feeding regimes in terms of trace element utilisation and, furthermore, whether bone metabolism might be affected due to either dietary treatment. Conventional feeding regimes can be understood as roughage (and oat) based rations, which are supplemented with calcium-rich complementary feeds in amounts of about 1 kg per day and animal. In the present study, this feeding regime was represented by the ration of Ca-High during phase 2. In phase 1, the supplementation of (macro) and trace elements as well as vitamins was carried out on the basis of mineral feeds which require amounts of about 0.1 kg per day per animal. During both phases, calcium supply in group Ca-Moderate was reduced in comparison to Ca-High. In general, mineral feeds are particularly suitable for horses in maintenance, as their energy requirement is covered (or even exceeded) by ad libitum feeding of hay [
16], but can also be fed as a supplement to hay and concentrates in the case of increased energy requirements. However, complementary feeds replace part of the concentrates and supply horses not only with minerals and vitamins but also with a certain amount of energy and protein. The resulting larger dosage offers a degree of protection against a (potentially dangerous) over-supply of trace elements and vitamins, as dosage inaccuracies are relatively less significant.
Considering mineral intake from 8 kg hay as fed in the present study displayed and compared to requirements according to GfE [
1] in
Table S4, the horses in the present study were already sufficiently supplied with macro minerals (except for sodium) by the hay. In addition, an uptake of straw (approx. 2 kg DM per animal and day) from the bedding material can also be assumed. This resulted in an additional supply of 4.4–4.8 g calcium, 3.0–3.7 g phosphorus, 18.8–20.2 g potassium, and 4.0–8.2 g chloride considering the chemical composition of the straw used in this study (
Table S2), whereas an additional supply of magnesium and sodium was negligible. With regard to trace elements, this study revealed clear deficits in the supply of copper, selenium and zinc, when hay (and straw) was the only source for minerals. In the literature, the macro element contents in hay are quantified similarly high. An accredited service laboratory in Germany (Landwirtschaftliche Untersuchungs- und Forschungsanstalt, LUFA Nord-West, Oldenburg, Germany) found in hay samples from 2014 to 2019 mean concentrations (and ranges of variations) of 4.7–4.9 g (1.6–19.4 g) Ca/kg DM, 2.2–2.6 g (0.6–4.9 g) P/kg DM, 0.2–1.4 g (< 0.2–11.1 g) Na/kg DM, 1.7–1.9 g (0.6–5.6 g) Mg/kg DM and 17.7–19.4 g (4.2–37.8 g) K/kg DM, respectively [
2]. Concentrations of trace elements were also comparable to those of the present study with 4.9–5.9 mg (2.1–11.2 mg) Cu/kg DM and 25–32 (10–111) mg Zn/kg DM [
2], so it can be assumed that the mineral concentrations in hay measured in this study are in line with the average and do not represent an outlier.
Warmblood horses comprise a large part of the horse population in Europe. However, there is hardly any data on the effects of different calcium contents in the diet of warmblood horses on mineral household and bone metabolism. Within the population of warmblood horses, the animals from the present study represent a homogenous group as only stallions of the same age belonging to one breed were used. While in mares, there are differences in the mineral status in dependence of reproductive status, mineral metabolism in stallions is subject to less fluctuations due to reproduction [
19].
Since blood calcium levels are tightly regulated by endocrine mechanisms, blood calcium levels in the present study did barely differ in dependence on dietary calcium supply and all measured values were within the reference of 9.6–13.6 mg/dL [
10,
16]. When comparing the serum phosphorus concentrations on the dependence of high and moderate calcium supply, it was noticeable that in Ca-Moderate, the phosphorus levels were numerically higher during the trial and significantly higher at the end of the trial in spite of slightly lower dietary phosphorus intake. The same observation could already be made in a balance study with adult ponies, where the effects of low compared to high calcium contents in the diet were likewise investigated [
20]. It can be assumed that calcium and phosphorus form complexes in the intestinal content, which reduces the bioavailability of phosphorus, especially in the presence of high dietary calcium levels [
21]. Furthermore, calcium carbonate, which was used in CF
1, works as a buffer and can increase intestinal pH. As phosphorus absorption is decreased with increasing intestinal pH, this might have further reduced the phosphorus availability in Ca-High [
21]. Nevertheless, all phosphorus serum levels were within the reference value [
16].
The labour of the horses (30 min/day), which according to Coenen and Vervuert [
16] can be classified as “light”, results in an additional requirement for macro elements, which is mainly due to electrolyte losses via sweat. However, the additional requirement for calcium, phosphorus and magnesium is already covered by the increased feed intake necessary to meet the energy requirement [
1]. The most abundant minerals in horse sweat are sodium (3.1 g/L), chloride (5.5 g/L), and potassium (1.6 g/L) [
22]. Since the sweat production of the horses was not monitored, it was not possible to quantify the amount of losses through sweat. Next to sweat production during work, basal sweat production should also be taken into account. According to Coenen and Vervuert [
16], basal sweat production is about 0.04l/kg BW
0.75 resulting in 4.5l of sweat per day and animal for the stallions in the present study. Basal sweat losses already occur within the thermoneutral zone (5–25 °C) of horses and increase at temperatures above 25 °C [
23]. In terms of sodium and chloride, intake through the salt-lick-stones is also an unknown variable, so that the sodium contents in the diet given in
Table 2 do not represent the total intake. However, the measured sodium concentrations were frequently below the reference range of 303–336 mg/dL [
16] in both groups, even though daily sodium intake exceeded recommendations of the GfE [
1]. These results support the assumption by Coenen and Vervuert [
16] that voluntary sodium intake via a salt-lick-stone might be not sufficient to meet the performance requirement for sodium that can reach amounts of 60 g sodium per day in hard-working warmblood horses (600 kg BW). For horses that sweat regularly, offering loose salt together with the concentrates should therefore be considered [
16]. Furthermore, in line with the low sodium serum levels measured in this study and against the background of basal sweat production according to Coenen and Vervuert [
16], the recommendation of the GfE on the maintenance requirement of sodium of 3.4 g per day for a warmblood horse [
1] could be reconsidered. The statements made for sodium also apply in principle to chloride. Serum chloride was several times below the reference of 351–386 mg/dL [
16], although chloride requirements were already fulfilled due to hay [
1]. Potassium concentrations were independent of the treatment mostly within the reference range of 10.9–18.8 mg/dL [
16]. All 13 exceptions were below 10.9 mg/dL. Similar to sodium and chloride serum levels, losses via sweat could be the cause. However, studies on the influence of sweating on the potassium concentrations in the blood provide contradictory results. While Soliman and Nadim [
24] found a decrease in serum potassium after exercise, Assenza et al. [
25] reported increasing potassium levels in the serum after three days of intensive training which was assumed to result due to losses from muscle fibres.
To evaluate the dietary supply of macro elements, blood tests provide a rapid and easy way of assessment. However, as already mentioned for calcium levels, limitations must be made with regard to the reliability of the results due to endocrine regulatory mechanisms [
26]. Furthermore, variations can occur as a consequence of circadian, prandial or genetic variations [
26], which, however, were excluded as best as possible in the present study.
In phase 1, the copper supply of Ca-High was 87.7 mg/d which is about 30% below the recommendations of the GfE from 2014 [
1]. This was caused mainly by the very low copper content of the hay (3.03 mg/kg DM) in the first phase of the trial, while in Ca-Moderate the copper requirement was met due to slightly higher copper concentrations in MF
2 than in MF
1. In phase 2, the copper supply for both groups was in the range of requirement. However, all serum copper levels were within the reference range of 50–250 µg/dL [
16]. Nevertheless, it should be considered that copper storage in the liver can be depleted in terms of insufficient supply [
27]. A 14-day feeding trial in mares revealed that mane hair might be a useful tool to evaluate dietary copper supply and therefore was recommended by the authors to use instead of blood sampling [
28]. The zinc supply of Ca-High in phase 1 met the requirement (525 mg/d) while it was in phase 2 and in Ca-Moderate during both phases slightly above the requirement [
1]. However, despite the slightly lower zinc supply in Ca-High, the high calcium excess had no effect on zinc levels in the serum in comparison to Ca-Moderate. In both groups, zinc levels were partly too low [
16]. Among the complementary feeds used, zinc was added in the form of inorganic zinc (zinc oxide and zinc sulphate). When evaluating the zinc supply, the zinc source should be taken into account, as inorganic zinc sources are associated with a lower bioavailability than organic zinc compounds [
29]. In addition, there is an interaction between dietary zinc and iron. It has been shown for several animal species that high levels of iron (as in the rations used in this study, presented in
Table 2) can impair zinc utilisation [
30]. The high iron concentrations in the serum, which partly exceeded the reference level according to Coenen and Vervuert [
16] of 70–200 mg/dL, could also be explained by the high iron contents in the diet which exceeded the requirements [
1] by 280%. However, when using the reference range of 70–300 mg/dL according to Geor et al. [
31], all values were within the norm. Considering the entirety of measured trace element concentrations in serum, the hypothesis of an influence of high calcium excess on serum trace element concentrations cannot be confirmed. Therefore, it can be assumed that serum levels of trace elements are subject to a variety of influences and do not always reflect the level of supply.
As calcium together with phosphorus is the most abundant mineral in the bone, playing an important role for bone formation especially during growth, a further focus of the study was bone metabolism. Osteocalcin (OC), as well as C-terminal telopeptide (CTX-I), are reliable markers in the blood to reflect bone formation (OC) and degradation (CTX-I) processes [
12,
13]. In the present study, marker concentrations were determined at the beginning of the trial, before the change of MF
1 to CF
1 and MF
2 to CF
2, respectively, in week 10, and at the end of the trial. In terms of OC, concentrations were already significantly higher in Ca-High at the first measurement (Ca-High: 10.2
a ± 3.26; Ca-Moderate: 7.75
b ± 3.05 ng/mL). As this finding cannot be attributed to the dietary treatment, it was checked whether other factors could have caused the difference. According to Lepage et al. [
12], OC concentrations fall with age. However, the mean days of the age of both groups were identical (Ca-High: 965 ± 19.1; Ca-Moderate: 964 ± 28.9 d). Bodyweight cannot be accountable for the difference either, as this did not differ between the groups during the entire experimental period. Overall, the values in this study were comparatively low. In Lusitano horses of different age groups, OC concentrations in blood were 35.4 ± 5.0 ng/mL (24 months old) and 26.2 ± 5.7 ng/mL (36 months old), respectively [
32]. Similar results were obtained by Jackson et al. [
33] who found OC concentrations of 37.0 ng/mL in two-year-old and 29.9 ng/mL in three-year-old thoroughbreds. The varying levels could be due to the use of different testing methods. While OC concentrations in the present study were analysed by means of an ELISA (IDS Immunodiagnostic Systems GmbH, Frankfurt am Main, Germany), OC levels in the study by Fradinho et al. [
32] and Jackson et al. [
33] were determined by means of a competitive immunoassay (QUIDEL Corporation, San Diego, CA, USA). However, our results are in agreement with Porr et al. [
34], who also could not demonstrate differences in serum OC concentrations due to either low- or high-calcium diets in adult Arabian horses. With respect to CTX-I concentrations, there were no differences between the groups throughout the trial. Concentrations in both groups were significantly lower at week 10 than at the beginning of the trial but reached the initial level again at the end of the trial. Fluctuations in CTX-I concentrations were demonstrated in dependence on workload and movement [
35]. Before the start of the trial, horses were kept in groups in playpens. After horses were brought to the stallion station where they were kept in individual boxes, the duration of movement was reduced. Therefore, CTX-I concentrations might have decreased. However, during the second half of the trial intensity of movement was increased as the horses have been broken in. This might explain the rise in CTX-I concentrations. Nevertheless, CTX-I concentrations in this study are consistent with values in two-year-old (0.46 ng/mL) and three-year-old (0.38 ng/mL) thoroughbreds [
33].