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Soil conditions under cormorant colonies favor for mites excepting Oribatida

Oszust, Mateusz 1 and Klimaszyk, Piotr 2

1✉ Zakład Dydaktyki, Wielkopolska Akademia Społeczno-Ekonomiczna w Środzie Wlkp.- Akademia Nauk Stosowanych, Środa Wielkopolska, Poland.
2Department of Water Protection, Faculty of Biology, Adam Mickiewicz University, Poznań, Poland.

2022 - Volume: 62 Issue: 4 pages: 974-988

https://doi.org/10.24349/u9ke-eqk9

Original research

Keywords

fertilization island soil mites soil microvertebrate

Abstract

Over the last few decades, the population of the great cormorant (Phalacrocorax carbo L., 1758) in Europe has been rising. The formation of large nesting and roosting colonies in relatively small areas, their rapid metabolism and the excretion of significant amounts of guano can have a marked environmental impact. This study aimed to investigate how cormorants affect the biodiversity and density of soil mites under breeding colonies. Soil samples from three cormorant colonies located on lake islands were compared to samples from adjacent areas unaffected by birds. Soil from colonies was characterised by a higher concentration of nitrogen, phosphorus and organic matter as well as the abundance of mites (except Oribatida). The abundance and diversity of adult Oribatida in soil under the colonies were lower than in their control sites.


Introduction

The great cormorant (Phalacrocorax carbo L., 1758) is a seabird with a global distribution. It is an apex predator with a diet almost exclusively based on fish. The growth of the European population of these birds has raised concerns due to their impact on the land and water environment. Cormorants breed and rest on land but forage on water and can, therefore, represent a very important intermediate link in ecosystems and food webs. Their fish-based diet and behaviour result in the transport of nutrients and other chemical elements between terrestrial and aquatic environments (Marion et al. 1994; Klimaszyk and Rzymski 2016). They deposit large amounts of guano (20–50 g per day), mainly beneath their roosts and nests, leading to acidification of the soil and accumulations of N and P loads to extreme levels. These changes in the chemical properties of the soil can decrease plant biodiversity and promote the growth of nitrophilous species. Cormorants also have a significant impact on the trees in their colonies, as these usually become defoliated because the birds break off twigs to build their nests, thus making the trees more susceptible to a pest invasion (Klimaszyk and Rzymski 2016).

The high allochthonous input and changes in soil chemistry and plant vitality, diversity and density also have a significant impact on food webs and the diversity of other groups of organisms. Previous studies found that the abundance, density or species richness of Collembola, Coleoptera (herbivores), Thysanoptera and litter spiders in breeding colonies of cormorants were lower than in reference sites (Kolb et al. 2010, 2012, 2015). Breeding colonies of cormorant are also characterised by a higher abundance and density of Astigmata (Acari), bacteriophage nematodes, some herbivores (Aphidoidae and Lepidoptera larvae) and their natural enemies, such as Hymenoptera, Neuroptera and Coccinellidae (Kolb et al. 2010, 2012, 2015; Pen-Mouratov and Dayan 2019).

This study aimed to determine how the transformations of habitat by cormorants affect the populations of soil mites, mainly Oribatida, which are one of the most common soil arthropods. Their abundance can reach up to 200 000 ind./m2. Most Oribatida are saprophagic, feeding mainly on dead plant material and fungi, but some species also eat, among other things, algae, lichen, mosses, and even nematodes. They digest dead organic material, which returns it into the circulation of nutrients (Magilton et al. 2019). Also, some species belonging to Nothroidea or Ptyctima, due to their sensitivity to soil disturbance, may serve as potential bioindicators of soil conditions (Gulvik 2007).

Additionally, the study collected data on the abundance of other soil mites (without distinguishing between species), which have different ecologies and functions. Mesostigmata are mostly predators, Astigmata are saprophagous, fungivorous, or graminivorous, while Prostigmata have a broad range of feeding habits, e.g. being predators, fungivores-microbivores, parasites, or omnivores (Potapov et al. 2022). These taxa are also considered to be potential bioindicators of soil conditions. For example, previous studies showed that disturbing the soil causes a decrease in the densities or percentage abundance of Oribatida, as well as an increase of Prostigmata (Gulvik 2007). These changes were due to the difference in life strategies of these mites. Most Oribatida use the K-strategy, while most Prostigmata use the r-strategy. Thus, the latter can colonise new habitats faster and react to change faster (Gulvik 2007).

Knowledge of the impact of cormorants on soil mites (Oribatida, among others) is still limited. Kolb et al. (2015) found a higher abundance of Astigmata and a lower abundance of moss mites in breeding colonies, but individuals were not identified to the species level. There are few publications on the impact of European cormorants on soil mites. Many works do not include Oribatida (e.g. Kolb et al. 2012) or focus on other bird species (e.g. Zmudczynska-Skarbek et al. 2017), which have different diets, nesting behaviours, or habitat preferences.

In summary, a hypothesis was formulated that the change in the soil habitat caused by cormorants results in a decrease in the abundance and diversity of Oribatida (adults and juveniles), and an increase in the abundance of Astigmata.

Material and methods

Study sites

The samples were collected on three sites (Fig.1):

Figure 1. Map of sampling sites.

Lake Chrzypsko

Samples were collected in July 2018 from the following sites:

  • Col. I - The cormorant colony (52°36′57″N, 16°13′23″E) has existed since the beginning of the 21st century. Cormorants occupy the most northward island of the lake, with an area of 0.9 ha. The island is slightly elevated above the lake level. It is overgrown mainly with alder (Alnus glutinosa (L.) Gaertn., 1791) and willow (Salix cinerea L., 1753). In sites where nests are concentrated, the herbaceous vegetation is very poor or represented by nitrophilous species like the nettle (Urtica dioica L., 1753) or elderberry shrubs (Sambucus nigra L., 1753). The forest canopy is bald and many of the trees are dead. In recent years, over 160 pairs of cormorants have been nested on the island.
  • Con. I - Control island (52°36′44″N, 16°13′24″E) is located about 400 m South of the cormorant colony. The island elevation is insignificant, and its area is about 1.4 ha. The island is unaffected by cormorants and is overgrown with dense alder, willow and ash (Fraxinus excelsior L., 1753) forest.

Lake Załom

Samples were collected in May 2019 from the following sites:

  • Col. II - The cormorant colony (53°04′58″N, 16°03′35″E) is located on the eastern island with an area of 0,6 ha. Inhabited by cormorants since the second decade of the 21st century. Overgrown with alders, oaks, birches and willows. In areas with cormorant nests, the tree canopy is sparse, herbaceous vegetation is absent and forest litter is accumulated. During the surveys over 200 nests were occupied by cormorants.
  • Con. II - Control island (53°04′59″N, 16°03′49″E) is unaffected by cormorants, it is about 150 m West of the colony. It is similar to the colony island regarding morphology. Vegetation showed no symptoms of cormorant impact.

Lake Drawskie

The colony and control sites were located on Bielawa Island. The island surface is about 8 ha and is mainly covered by forest. Samples were collected in June 2019.

  • Col. III – The cormorant colony (53°36′11″N, 16°09′44″E) was established in the first decade of the 21st century on the western part of the island. Today, almost 800 pairs of cormorants are nesting there. The area of the colony is overgrown with alder, willow and elderberry shrubs. Herbaceous vegetation is sparse.
  • Con. III - control site (53°36′05″N, 16°10′24″E) is located 500 m from the colony in an alder forest unaffected by cormorants.

Sampling

Sampling of soil for chemical analyses

Soil samples for chemical analyses were taken simultaneously and from the same sites as the soil fauna samples. The collected soil samples were air-dried and sieved using a 2-mm sieve to separate gravel (particle size \textgreater2 mm) and non-soil components and were stored in a freezer at -20 °C prior to analysis.

Sampling of soil for studying mite communities

In total, 25 soil samples were collected from random sites in the central part of each island using a metal core (10 cm in depth, 4 cm in diameter). Samples were collected from under nests in breeding colonies of cormorants. Invertebrates were extracted with a Tullgren funnel and preserved in 75% ethanol. Soil mites were divided into the following groups: Astigmata, Mesostigmata, Prostigmata, and adult and juvenile Oribatida.

Chemical analyses of soil

The total amount of nitrogen (NtK) in soils was determined using the Kjeldahl method (van Reeuwijk 1995), constituting the sum of Norg and N-NH4. Contents of N-NO3- and N-NH4+ were determined after extraction in CH3COOH (0.03 mol L-1) using the Nessler method, whereas N-NO2- was analysed using a method with phenoldisulphonic acid (Prince 1955). TP content in soils was determined at 850 nm using a Shimadzu UV-1610 spectrophotometer (molybdate method) after burning the samples at 550 °C and mineralized in suprapure HNO3 (14 mol L) and H2SO4 (18 mol L) (Sobczyński and Joniak 2009). The amount of organic matter in soil samples was measured as a percentage weight loss through the combustion at 550 °C for 3 h following drying at 50 °C for 24 h (Wang et al. 2011).

Identification of soil mites

To classify individuals, adult Oribatida mites were macereted with 80% lactic acid. Subsequently, they were placed on a microscope cavity slide and covered by a coverslip. A drop of lactic acid was also used as the medium. The following keys were used for the identification: Olszanowski (1996), Weigmann (2006), Niedbała (2008), and Krantz and Walter (2009). The abundance, constancy, density, and dominance were estimated for each species. Up-to-date taxon names were used according to Subías (2004, updated 2021).

Data analysis

Diversity and abundance of mites

To compare study sites, the following indices were used according to Krebs (2011), Carmo et al. (2013), Pen-Mouratov and Dayan (2019):

  • Abundance: number of individuals per sample
  • Density: number of individuals per m2
  • Dominance: DOM=(i/t)*100, where i = abundance of taxa and t = total abundance of all taxa
  • Constancy: CON=(p × 100)/N, where p = number of samples in which the taxa is present; N = total number of samples
  • Species richness: SR=[(S-1)/ln(N)], where S is the number of species and N is the number of individuals identified
  • Shannon-Wiener diversity index: H′=[−ΣPi (lnPi)], where Pi is the proportion of individuals in the taxon
  • Species evenness: J′=H′/Hmax, where Hmax = lnS
  • Modified Simpson's dominance index: D = 1-(ΣPi2)

Additionally, we used a modified ratio of the dominance index of Oribatida and Prostigmata, which is based on the ratio of the relative abundance of Oribatida and Prostigmata (Gulvik 2007). To avoid dividing by zero (many samples lacked Prostigmata), 1 was added to the dominance values of both groups.

O+1/P+1, where O = dominance value of Oribatida, P = dominance value of Prostigmata.

Statistical analysis

Data about soil chemistry and mites were assessed with the Shapiro–Wilk tests. Due to the lack of normality of the distributions in most cases and unsuccessful attempts at transformation, Mann–Whitney U test was applied on the untransformed data.

A canonical correspondence analysis (CCA) was conducted to identify species and site arrangements in relation to environmental factors. The analyses used untransformed data for average soil chemistry (pH, organic material content, and nitrogen content in mineral and organic form), the number of cormorant pairs, and mean abundance of species whose dominance after rounding up was ≥5% on at least one island. Data about each species of Oribatida were transformed using: log(x+1), where x is the mean abundance.

Statistical software

Statistical analyses about soil chemistry were performed with the program Statistica (StatSoft Inc. 2007). The significance of any difference in the data for soil mites was calculated with the base and stats R packages (R Core Team 2020). A graphical interface was also used (RStudio Team 2020). The CCA was run using the PAST software package (Hammer et al. 2001).

Results

Soil chemistry

Table 1. Content of nutrients and pH in (±SD) under cormorant colonies (Col) and control sites unaffected by birds (Con). Asterisk signifying p-value of Mann–Whitney U test for given pairs of islands: * p<0.05, ** p<0.001, *** p<0.001.

Cormorants exerted a significant influence on the chemistry of the soils under their colonies. Very high concentrations of nitrogen, phosphorus, and potassium were recorded, as well as soil acidification. Among nitrogen forms, organic nitrogen predominated in all colonies, accounting for between 60% and 70% of the total pool of accumulated nitrogen. Regardless of the colony, compared to control sites, which were not exposed to bird impact, soils under colonies were characterised by 4 to more than 10 times higher nitrogen concentrations. The differences between colonies and control sites were even greater for total phosphorus concentrations. Soils under the colonies were characterized by 20 times (Lake Załom) to almost 90 times (Lake Chrzypskie) higher concentrations of this element than the control sites. The differences for potassium were not as high, but like nitrogen and phosphorus, the soils under the colonies were characterised by statistically significantly higher concentrations of potassium (Table 1). The soil reaction at the control sites was neutral or slightly alkaline, while the soil under the colonies was strongly acidic (Table 1). Moreover, the content of organic matter in the soil under the cormorant colonies was statistically higher compared to the control sites (Figure 2).

Figure 2. Organic matter comparisons between studied islands. Asterisk signifying p-value of Mann-Whitney U test for given pairs of islands: * p<0.05, ** p<0.001, *** p<0.001.

The abundance of soil mites

In total, 3 191 individuals of adult Oribatida were found. The highest abundance of Oribatida was in control site II (Con. II), where 1679 specimens were found (Table 2). The lowest abundance was detected in colony site III (Col. III). The abundance of juveniles was lower than that of adults. In all cormorant colonies, fewer Oribatida (both adults and juveniles) were recorded than in the corresponding control sites. This difference is statistically significant for Oribatida from the islands in Lake Drawskie and the population of adult mites in Lake Załomie (Table 2).

Table 2. Abundance (A), mean density (D) and constancy (C) of Oribatida (adult and juvenile) with standard error (SE). Asterisk signifying p-value of Mann–Whitney U test for given pairs of islands: * p<0.05, ** p<0.001, *** p<0.001.

Figure 3. Comparison of abundance of mite groups in soil under cormorant colonies and control sites. Asterisk signifying p-value of Mann–Whitney U test for given pairs of islands: * p<0.05, ** p<0.001, *** p<0.001. box – mean, whisker – SE.

Among other soil mite groups (Table 3), the most numerous were Mesostigmata (955 individuals), while the least abundant were Prostigmata (209 individuals). Mesostigmata were identified in most samples from all sites. Their constancy was ≥80%. Astigmata and Mesotigmata were mostly significantly more abundant in colonies than at reference sites (Figure 3). The only exception was an island in Lake Załomie. Populations of Prostigmata were also greater in areas occupied by cormorants but only the difference between Col. II and Con. II was statistically significant. The ratio of Oribatida and Prostigmata dominance was significantly lower in all colonies (Table 4).

Table 3. Abundance (A), mean density (D) and constancy (C) of other mites (Astigmata, Mesostigmata and Prostigmata) with standard error (SE). Asterisk signifying p-value of Mann–Whitney U test for given pairs of islands: * p<0.05, ** p<0.001, *** p<0.001.

Table 4. Number of species, mean species richness (SR), Shannon-Werner index (H′) evenness(J′) and Simpson index (D) of samples, mean dominance ratio of Oribatida and Prostigmata (O/P) with standard error (SE). Next to the value of colonies indices are asterisk signifying p-value of Mann–Whitney U test for given pairs of islands: * p<0.05, ** p<0.001, *** p<0.001, ns – non-significant.

Species diversity of Oribatida

In total, 78 species from 32 families were recorded (Table Supplement). The richest number of species was found at the control site on the island in the Lake Drawskie, where 39 species were found (Table 4). In all cormorant colonies, fewer species were recorded than at control sites. Furthermore, most samples from colonies had lower values for species richness, evenness, Shannon-Werner index and Simpson index. In most cases, these differences were statistically significant. Exceptions were the islands in Lake Chrzypsko where no difference was significant (except Simpson index). Among control sites, the highest values of all indicators (except J′) were found in Con. II.

In Cols. II and III, the dominant species were Rhinoppia nasuta (Moritz, 1965) and Acrogalumna longipluma (Berlese, 1904). Their dominance values ranged from 3.60% to 55.43% and from 4.50% to 21.70%, respectively (Table Supplement). Both species also occurred in Col. I (constancy values 8% and 12%), but the most common species was Scheloribates laevigatus (Koch, 1835), which was absent in other colonies of cormorants. The dominance and constancy of this species were 61.26% and 80%. For comparison, in reference sites (Cons.I, II, III) Atropacarus striculus (Koch, 1835), Oppiella nova propinqua Mahunka & Mahunka-Papp, 2000; Oppiella nova (Oudemans, 1902) and Suctobelbella baloghi (Forsslund, 1950) were the most common species. Oppiella nova also occurred frequently in colonies of cormorants, and three individuals of A. striculus were found in Col.II. The dominance of A. striculus at control sites ranged from 11.37% to 34.36%, while its constancy range was from 48% to 96%. No specimens of R. nasuta were recorded at the reference sites.

CCA was used to analyse the Oribatida communities in relation to habitat type (Figure 4). The first eigenvalue axis is about 0.71 and explains 46.63% of the variance. The permutation test shows that the eigenvalue of the first axis is significant (p= 0.035; N= 999). It is positively correlated with the pH, while organic material (Om), number of cormorants pairs (Cor), and mineral and organic nitrogen (N min and N org) were negatively correlated with this axis. Cor and N org had the strongest correlation with the axis (the smallest angles between the axis and the vector). For the second axis, the eigenvalue is 0.59 and explains 38.64% of the variance. CCA divided the studied sites into three groups of points. Along the first axis, Cols. II and lII are separated from their reference sites. These colonies are positively correlated with Cor and all soil parameters apart from pH and have the highest abundances of S. pallidulus, S. latipes, H. rufulus, A. longipluma and R. nasuta.

Figure 4. CCA with scaling type 2 of the relationship between site fauna and chemical parameters of soil: Cor – number of cormorants pairs, Om – soil organic matter, N min. – mineral nitrogen, N org – organic nitrogen, pH – value of pH, H.r – Hypochthonius rufulus, A.s – Atropacarus striculus, P.c – Phthiracarus clavatus, M.m – Malaconothrus monodactylus, R.n – Rhinoppia nasuta, O.n – Oppiella nova, O.p – Oppiella nova propinqua, Q.h – Quadroppia hammerae, S.b – Suctobelbella baloghi, S.f – Suctobelbella forsslundi, T.t – Tectocepheus velatus sarekensis, O.t – Oribatula tibialis, C.s – Chamobates subglobulus, S.p – Scheloribates pallidulus, S.lv –Scheloribates laevigatus, S.l – Scheloribates pallidulus latipes, A.l – Acrogalumna longipluma.

The next group of points are reference sites, which are positively correlated with the pH and characterised by the highest abundance of A. striculus, P. clavatus, M. monodactylus, O. nova, O. nova propinqua, Q. hammerae, S. baloghi, S. forsslundi, and T. velatus sarekensis. Colony I stands out the most among the islands. This site is characterised by the highest abundance of S. laevigatus and is the only site where C. subglobulus and O. tibialis were found. O. nova is close to the central portion of the triplot. These species occur in nearly all sites; however, it was more abundant at the reference sites.

Discussion

This study demonstrated that cormorants cause significant alterations in biotopes and biocenoses under their colonies. The soil under all the surveyed colonies contained significantly higher loads of nitrogen (both the organic and mineral form), phosphorus and potassium compared to the control sites. Fertilisation of areas under cormorant colonies and roosts results mainly from the deposition of nutrient-rich guano (Marion et al. 1994; Ligęza and Smal 2003; Klimaszyk 2012). The faeces-originating nitrogen occurs primarily in the form of uric acid (Mizutani and Wanda 1988; Mulder and Keall 2001) which acidifies soils under the colonies (Kameda et al. 2000; Breuning-Madsen et al. 2008). In the case of the surveyed colonies, strong soil acidification was also noted. Moreover, additional loads of chemical substances are deposited under colonies with cormorants' pellets, which contain fish remains, along with the bird-induced accumulation of plant debris (Hobara et al. 2001; Osono 2006a). In dense colonies, cormorants may be responsible for the accumulation of as much as 2000 kg ha-1 of forest litter per month (Klimaszyk and Rzymski 2016). This usually results in the topsoil horizon becoming enriched with organic matter (Osono et al. 2006a; Breuning-Madsen et al. 2008; Klimaszyk 2012), which was also reported in the studied colonies.

In addition to their chemical properties, soils beneath the colonies differed from the control sites with respect to the diversity and abundance of mites. Similar to Kolb et al. (2015), we found that the abundance of oribatid mites was lower in soil under cormorant colonies, but Astigmata were more frequent in the areas than at the control sites unaffected by birds. However, contrary to the above-mentioned work, Mesostigmata mites were significantly more abundant in soils under cormorant pressure. Most Mesostigmata are predators, thus an increase in their abundance might be caused by the higher availability of prey, such as bacteriophage nematodes, which are also more abundant in these habitats (Pen-Mouratov and Dayan 2019) or other invertebrates. Isotopic studies in the Westland petrels (Procellaria westlandica Falla, 1946) colony showed that one mesostigmatid species likely feeds on guano decomposers or their eggs (Hawke et al. 2013).

Astigmata, which include species associated with carrion, guano and nests as well as parasites of birds, likely filled appropriate microhabitats in cormorants colonies (Krantz and Walter 2009). Previous studies also show a correlation between the density of Astigmata and the concentration of N, for which the source could be guano (Kolb et al. 2015).

For all the studied colonies, the dominance ratios of Oribatida and Prostigmata were lower than at their control sites. This is in accordance with previous studies, which showed that a change in the ecosystem (e.g. the transformation of woodland into an arable field) leads to a decrease of Oribatida and an increase in Prostigmata abundance (Gulvik 2007). Prostigmata were more abundant in the colonies in this study, but statistical significance was achieved only in the samples from islands on Lake Załomie. Most individuals likely belonged to Heterostigmata (e.g. Scutacaridae), which are among other things fungivorous, phytophagous and algophagous mites (Krantz and Walter 2009). However, Kolb et al. (2015) did not demonstrate any statistically significant differences in the density of Prostigmata between colonies and their reference sites.

Zmudczynska-Skarbek et al. (2017) also revealed the significant negative effect of a colony of planktivorous little auks (Alle alle (L., 1758)), on decomposers' diversity (oribatid mites and springtails) and a positive one on the density of predator (mesostigmatid mites and one spider species) and the number of invertebrate species. However, other studied birds, such as the predatory glaucous gull (Larus hyperboreus Gunnerus, 1767) and great skua (Stercorarius skua (Brünnich, 1764)), did not have any significant impact on invertebrates populations. Contrary to the above-mentioned works and present results, the studies of Orwin et al. (2015), showed a positive effect of seabirds' burrow density on the abundance of oribatid and mesostigmatid mites. Similarly, Ilieva-Makulec et al. (2015) also found a higher abundance of mites (the authors did not separate the mites into groups) from soil under corvid roosts.

The results obtained indicate that cormorants have a significant effect on the biodiversity of Oribatida. In all colonies, the abundance, numbers of species and values of diversity indices were lower than those at control islands unaffected by birds. In the case of Lake Chrzypsko, no diversity indices were statistically significant (except Simpson's dominance index), although the difference in the number of species between the colony and control islands was the highest. However, in Con. I most species had constancy lower than 25%, thus the diversity indices values were low. The lowest abundance, constancy and diversity indices of Oribatida were for Col. III, which could have been caused by the substantial impact of cormorants because that island was occupied by the highest number of bird pairs during the study.

Species composition also differed among the studied islands. Many species (e.g. Galumna obvia (Berlese, 1915) were found only at the control sites. This is similar to the findings of previous studies that showed this taxon is sensitive to a high dose of organic fertilisation (Wasińska-Graczyk et al. 2009). Suctobelbidae, Phthiracaridae (e.g. A. striculus) and Nothrina (Malaconothridae, Crotoniidae, Nothridae), as well as others, turned out to be the groups most sensitive to guano fertilisation. In the control sites, they are the most abundant and diverse soil mites, while in colonies, they were found sporadically. A similar result was obtained by Lebedeva et al. (2006), as no species from Suctobelbidae or Phthiracaridae were found in soil from the breeding sites of the Arctic tern (Sterna paradisaea Pontoppidan, 1763) and snow bunting (Plectrophenax nivalis (L., 1758)). Nothrina and Phthiracaridae are known for their sensitivity to soil disturbance and are considered potential bioindicators of soil quality (Gulvik 2007). Moreover, in some studies, Suctobelbella sp. reacted by decreasing in abundance due to soil fertilisation (Lindberg and Persson 2004; Cao et al. 2011).

The reason for the decrease in Oribatida diversity is not known; however, it is most likely to be the result of combination of several factors, interacting with individual species in different intensities. The first potential factor is the harmful effect of guano's compounds, including ammonia, which is toxic to most animals (Weihrauch et al. 2012). However, the effect of the cormorant colony could be less direct. The low abundance of A. striculus might be due to decreased plant cover and diversity because the abundance of this species is correlated with these factors (Skubała and Maślak 2010). Guano also has a significant impact on the abundance and species composition of bacteria, lichen and fungi, which are sources of food for oribatid mites (Osono et al. 2002, 2006a,b; Kutorga et al. 2013; Magilton et al. 2019; Motiejūnaitė et al. 2014; Pen-Mouratov and Dayan 2019). Thus, faecal fertilisation may decrease the availability of the food preferred by mites. For example, high concentrations of phosphorus inhibit the development of mycorrhizal hyphae, while excess nitrogen interferes with the activity of the lignin-degrading enzymes of ligninolytic fungi (Osono et al. 2002, 2006b; Cao et al. 2011). Kolb et al. (2015) also noticed a negative correlation between the density of Oribatida and soil P concentration in cormorant colonies. According to Lemanski and Scheu (2004), fertilisation of the soil weakens the trophic links between microorganisms and microbial grazers and leads to changes in the diet of soil invertebrates. Most Oribatida are characterised by high trophic plasticity; however, the type of food affects their fertility and mortality. Thus, the reduced availability of food might limit the abundance of some species (Seniczak et al. 2017; Maraun et al. 2020). The enrichment of potassium in colonies was not huge; thus its effect on mites is likely masked by the influence of phosphorus and nitrogen.

Although cormorants create hostile habitats for most Oribatida species, some tolerate or maybe prefer such an environment. Among the taxa recorded in the colonies were for examples, Punctoribates punctum (Koch, 1839) and Scheloribates laevigatus which according to Seniczak et al. (2006) and Wasińska-Graczyk et al. (2009) showed a significant tolerance or even increased abundance in the presence of ammonia water and high dose of liquid pig manure (for second species small and medium dose caused opposite effect). Another example is O. pectinate, which are mites associated mostly with nests of for examples, birds (Rajski 1968; Skubała and Kalinka 2006).

The presence of cormorants can create optimal conditions for scavengers due to the availability of dead plant and animal remains. Also, a higher density of nematodes in topsoil may be beneficial mites that feed on nematodes (Pen-Mouratov and Dayan 2019). An example of a scavenger mite is H. rufulus, which is one of the most common species in colonies (Magilton et al. 2019). Acrogalumna longipluma is considered a secondary decomposer or fungivore. However, Melguizo-Ruiz et al. (2017) suggest that this species may function in part, as a predator, scavenger or omnivore. Oppiidae (e.g. O. nova) are also known for feeding on nematodes. According to Eissfeller et al. (2013), the densities of both groups are correlated.

Rhinopia nasuta occurred only in cormorant colonies and was the dominant species in Cols. II and III. This is a rare species. In Poland, it has been found only in one cave (without bats and guano) according to Maślak and Barczyk (2011). Rhinopia nasuta is known mostly from beech forests and soil with low pH and high C/N ratio and humus mass (Weigmann and Kratz 1981; Arabuli 2007; Eissfeller et al. 2013). Thus the fertilisation and acidification of soil by cormorant guano may create optimal conditions for R. nasuta populations. The density of R. nasuta is also associated with the density of nematodes. Thus like other Oppidae, this species may be predatory (Eissfeller et al. 2013).

Although R. nasuta occurred in all the colonies, its abundance on each island was different. This species was the most common mite, in Cols. II and III. However, its constancy was low in Col. III (8%) because most samples were free of Oribatida. The colony on Lake Drawskie was the biggest (800 pairs); thus, its impact may be too strong for most Oribatida. Rhinopia nasuta was also identified in Col. I, although only four specimens were found. A more common species was S. laevigatus. This could be because of the specificity of the island. In contrast to Col. II, the colony on Chrzypsko has very poor herbaceous vegetation, the forest canopy was bald and many of the trees were dead (the conditions on Col.III were intermediate between the mentioned colonies). These factors might lead to better insolation of soil and thus, to a change in soil temperature and moisture (Kunkel et al. 2016). This could explain the dominance of S. laevigatus, as this species is common in similar habitats such as meadows (Rajski 1967). On the other hand, it could create less optimal conditions for R. nasuta due to for example the lower humidity of the soil. Progressive deforestation in the colonies may lead to the replacement of R. nasuta by S. laevigatus. If this hypothesis is true, these mites could be used as bioindicators of cormorant activity and the development stage of a colony.

Another species common in the islands studied is A. longipluma, which was found in all colonies. One individual was found in Con. II. According to Rajski (1968), this is a rather rare species, being known from various microhabitats, like tree hollows, mosses, lichen or ant nests. They are also found in tree hollows with bird guano (Żbikowska-Zdun et al. 2006; Seniczak et al. 2012). A decrease in the abundance of some Oribatida due to the transformation of soil by cormorants may make accessible niches for A. longipluma and other more resistant species, which would explain, why they became the dominant species.

The influence of ornithogenic input on oribatid mite diversity has been poorly studied and the results do not display clear dependencies. Zmudczynska-Skarbek et al. (2017) found T. velatus in sites occupied by auks and gulls. Of the colonies studied only one individual of T. velatus sarekensis was found. It was from Col. III Oribatula tibialis, which was found in Col. I has also been recorded in soil from a colony of gulls and skuas. However, in both colonies, this species occurred in only one plot (Zmudczynska-Skarbek et al. 2017). Oribatula tibialis has also been found in ornithogenic soils from the breeding sites of the Svalbard Arctic tern (Sterna paradisaea) and snow bunting (Plectrophenax nivalis).

In summary, the transformation of soil by cormorants leads to a drastic change in the abundance of soil mites, Oribatida diversity and species compositions. Since the samples from each pair of islands (colony and reference site) were collected on the same day, thus we could exclude any seasonal variation. However, this does not apply overall, as the soil samples Załomie and Drawskie were collected in different months (May and June). Moreover, the fieldwork in Chrzypsko was in different years. Oribatida may display seasonal fluctuations of abundance (e.g. Seniczak et al. 2006). Thus, the sampling date may be an important factor. Additionally, cormorants are migratory birds. They leave colonies at the end of summer and come back in spring; thus, the impact of these birds is not constant over the year. For example, cormorants generally have a negative impact on trees; however, Molina-Montenegro et al. (2013) noticed the increased growth of trees on an island abandoned by these birds due to, among other things, the accumulation of organic material. This leads to the hypothesis that some species of Oribatida may recolonise islands during the cormorants' absence (between autumn and spring) and that their abundance gradually decrease, when new colonies form. This hypothesis could be verified in further studies, such as on the relation between seasonal dynamics of Oribatida and cormorants.

According to our results, the best potential indicators of the impact of cormorants on soil would be R. nasuta and members of Scherloribates, Suctobelbidae, Phthiracaridae and Nothrina. However, this work should be treated as a pilot study due to the small number of samples and because each island was sampled on only one day. More seasons and samples should be included in further research to confirm the observations of this study.

Acknowledgements

The authors would like to commemorate professor Ziemowit Olszanowski, appreciating his advice and assistance in research. The authors would also like to thank Aleksandra Jagiełło for help in field and laboratory analyses, as well as Elaheh Daghighi from Center for Environmental Research and Sustainable Technology for her help in calculation.



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References

  1. Arabuli T. 2007. The oribatid mites (Acari, Oribatida) of Gombori. Ecology, 5(1):23-28.
  2. Breuning-Madsen H., Ehlers B.C., Borggaard O.K. 2008. The impact of perennial cormorant colonies on soil phosphorus status. Geoderma, 148:51-54. https://doi.org/10.1016/j.geoderma.2008.09.002
  3. Cao Z., Han X., Hu C., Chen J., Zhang D., Steinberger Y. 2011. Changes in the abundance and structure of a soil mite (Acari) community under long-term organic and chemical fertilizer treatments. Appl. Soil. Ecol., 49:131-138. https://doi.org/10.1016/j.apsoil.2011.06.003
  4. Carmo R.F.R., Amorim H.P., Vasconcelos S.D. 2013. Scorpion diversity in two types of seasonally dry tropical forest in the semi-arid region of Northeastern Brazil. Biota Neotrop., 13(2):340-344. https://doi.org/10.1590/S1676-06032013000200037
  5. Eissfeller V., Langenbruch C., Jacob A., Maraun M., Scheu S. 2013. Tree identity surpasses tree diversity in affecting the community structure of oribatid mites (Oribatida) of deciduous temperate forests. Soil Biol. Biochem., 63:154-162. https://doi.org/10.1016/j.soilbio.2013.03.024
  6. Gulvik M. 2007. Mites (Acari) as indicators of soil biodiversity and land use monitoring: a review. Pol. J. Ecol., 55(3):415.
  7. Hammer Ø., Harper D.A.T., Ryan P.D. 2001. PAST: Paleontological statistics software package for education and data analysis. Palaeontol. Electron., 4:1-9.
  8. Hawke D.J., Clark. J.M., Vallance J.R. 2013. Breeding Westland petrels as providers of detrital carbon and nitrogen for soil arthropods: a stable isotope study. J. R. Soc. N. Z., 43(1), 58-65. https://doi.org/10.1080/03036758.2011.616211
  9. Hobara S., Osono T., Koba K., Tokuchi N., Fujiwara S., Kameda K. 2001. Forest floor quality and N transformations in a temperate forest affected by avian-derived N deposition. Wat. Air and Soil Poll. 130(1):679-684. https://doi.org/10.1023/A:1013869115132
  10. Ilieva-Makulec K., Kozacki D., Makulec G. 2015. The impact of roosting birds on the abundance of two groups of soil mesofauna. Stud. Ecol. Bioeth., 13(4), 117-133. https://doi.org/10.21697/seb.2015.13.4.05
  11. Kameda K., Koba K., Yosimizu C., Fujiwara S., Hobara L., Koyama L., Tokuchi N., Takayanagi A. 2000. Nutrient flux from aquatic to terrestrial ecosystem maintained by the great cormorant. Sylvia, 36:54-55.
  12. Klimaszyk P. 2012. May a cormorant colony be a source of coliform and chemical pollution in a lake? Oceanol. Hydrobiol. Stud., 41:67-73. https://doi.org/10.2144/btn-2019-0084
  13. Klimaszyk P., Rzymski P. 2016. The complexity of ecological impacts induced by great cormorants. Hydrobiologia, 771(1):13-30. https://doi.org/10.1007/s10750-015-2618-1
  14. Kolb G.S., Jerling L., Hambäck P.A. 2010. The impact of cormorants on plant-arthropod food webs on their nesting islands. Ecosystems, 13(3):353-366. https://doi.org/10.1007/s10021-010-9323-8
  15. Kolb G.S., Jerling L., Essenberg C., Palmborg C., Hambäck P.A. 2012. The impact of nesting cormorants on plant and arthropod diversity. Ecography, 35(8):726-740. https://doi.org/10.1111/j.1600-0587.2011.06808.x
  16. Kolb G.S., Palmborg C., Taylor AR., Bååth E., Hambäck P.A. 2015. Effects of nesting cormorants (Phalacrocorax carbo) on soil chemistry, microbial communities and soil fauna. Ecosystems, 18(4):643-657. https://doi.org/10.1007/s10021-015-9853-1
  17. Krantz G.W., Walter D.E. 2009. A manual of acarology. Texas Tech University Press.
  18. Krebs CJ. 2011. Ekologia [Ecology]. Wyd. Nauk. PWN. Warsaw. p. 573-574. In Polish.
  19. Kunkel V., Wells T., Hancock G.R. 2016. Soil temperature dynamics at the catchment scale. Geoderma, 273: 32-44. https://doi.org/10.1016/j.geoderma.2016.03.011
  20. Kutorga E., Irsenaite R., Iznova T., Kasparavicius J., Markovskaja S., Motiejunaite J. 2013. Species diversity and composition of fungal communities in a Scots pine forest affected by the great cormorant colony. Acta Mycol., 48(2):173-188 https://doi.org/10.5586/am.2013.019
  21. Lebedeva N.V., Lebedev V.D., Melekhina E.N. 2006. New data on the oribatid mite (Oribatei) fauna of Svalbard. Dokl. Biol. Sci., 407(1):182-186. https://doi.org/10.1134/S0012496606020207
  22. Lemanski K., Scheu S. 2014. Fertilizer addition lessens the flux of microbial carbon to higher trophic levels in soil food webs of grassland. Oecologia, 176(2):487-496. https://doi.org/10.1007/s00442-014-3037-0
  23. Ligęza S., Smal H. 2003. Accumulation of nutrients in soils affected by perennial colonies of piscivorous birds with reference to biogeochemical cycles of elements. Chemosphere, 52:595-602. https://doi.org/10.1016/S0045-6535(03)00241-8
  24. Lindberg N., Persson T. 2004. Effects of long-term nutrient fertilisation and irrigation on the microarthropod community in a boreal Norway spruce stand. For. Ecol. Manage., 188(1-3):125-135. https://doi.org/10.1016/j.foreco.2003.07.012
  25. Magilton M., Maraun M., Emmerson M., Caruso T. 2019. Oribatid mites reveal that competition for resources and trophic structure combine to regulate the assembly of diverse soil animal communities. Ecol. Evol., 9(14):8320-8330. https://doi.org/10.1002/ece3.5409
  26. Maraun M., Augustin D., Pollierer MM., Scheu S. 2020. Variation in trophic niches of oribatid mites in temperate forest ecosystems as indicated by neutral lipid fatty acid patterns. Exp. Appl. Acarol., 81(1):103-115. https://doi.org/10.1007/s10493-020-00494-2
  27. Marion L., Clergeau P., Brient L., Bertru G. 1994. The importance of avian-contributed nitrogen (N) and phosphorus (P) to Lake Grand-Lieu, France. In: Kerekes JJ, editor Aquatic Birds in the Trophic Web of Lakes. Developments in Hydrobiology. Springer. Dordrecht. 96:133-147. https://doi.org/10.1007/978-94-011-1128-7_13
  28. Maślak M., Barczyk G. 2011. Oribatid mites (Acari, Oribatida) in selected caves of the Krakow-Wielun Upland (southern Poland). Biol. Lett., 48(1):107-116. https://doi.org/10.2478/v10120-011-0011-y
  29. Melguizo-Ruiz N., Jiménez-Navarro G., Zieger S.L., Maraun M., Scheu S., Moya-Laraño J. 2017. Complex effects of precipitation and basal resources on the trophic ecology of soil oribatid mites: Implications for stable isotope analysis. Eur. J. Soil Biol, 82:98-107. https://doi.org/10.1016/j.ejsobi.2017.08.008
  30. Mizutani H., Wanda E. 1988. Nitrogen and carbon isotope ratios in seabird rookeries and their ecological implication. Ecology, 69:340-349. https://doi.org/10.2307/1940432
  31. Molina-Montenegro M.A., Torres-Díaz C., Gallardo-Cerda J., Leppe M., Gianoli E. 2013. Seabirds modify El Niño effects on tree growth in a southern Pacific island. Ecology, 94(11): 2415-2425. https://doi.org/10.1890/12-1054.1
  32. Motiejūnaitė J., Iršėnaitė R., Adamonytė G., Dagys M., Taraškevičius R., Matulevičiūtė D., Koreivienė J. 2014. Pine forest lichens under eutrophication generated by a great cormorant colony. The Lichenologist, 46(2):213-228. https://doi.org/10.1017/S0024282913000820
  33. Mulder CPH., Keall SN. 2001. Burrowing seabirds and reptiles: impact on seeds and soils in an island forest in New Zealand. Oecologia., 127:350-360. https://doi.org/10.1007/s004420000600
  34. Niedbała W. 2008. Ptyctimous mites (Acari, Oribatida) of Poland. Museum and Institute of Zoology at the Polish Academy of Science.
  35. Olszanowski Z. 1996. A monograph of the Nothridae and Camisiidae of Poland [Acari: Oribatida: Crotonioidea]. Genus Int. J. Invertebr. Taxon. Supplement.
  36. Orwin K.H., Wardle D.A., Towns D.R. 2015. Burrowing seabird effects on invertebrate communities in soil and litter are dominated by ecosystem engineering rather than nutrient addition. Oecologia, 180, 217-230 https://doi.org/10.1007/s00442-015-3437-9
  37. Osono T., Hobara S., Fujiwara S., Koba K., Kameda K. 2002. Abundance, diversity, and species composition of fungal communities in a temperate forest affected by excreta of the Great Cormorant Phalacrocorax carbo. Soil Biol. Biochem., 34(11):1537-1547. https://doi.org/10.1016/S0038-0717(02)00123-2
  38. Osono T., Hobara S., Koba K., Kameda K., Takeda H. 2006a. Immobilization of avian derived nutrients and reduced lignin decomposition in needle and twig litter in a temperate coniferous forest. Soil Biol. Biochem., 38:517-525. https://doi.org/10.1016/j.soilbio.2005.05.022
  39. Osono T., Hobara S., Koba K., Kameda K. 2006b. Reduction of fungal growth and lignin decomposition in needle litter by avian excreta. Soil Biol. Biochem., 38(7):1623-1630. https://doi.org/10.1016/j.soilbio.2005.12.001
  40. Potapov A.M., Beaulieu F., Birkhofer K., Bluhm S.L., Degtyarev M.I., Devetter M., Goncharov A.A, Gongalsky K.B., Klarner B., Korobushkin D.I., Liebke D.F., Maraun M., Mc Donnell R.J., Pollierer M.M., Schaefer I., Shrubovych J., Semenyuk I.I., Sendra A., Tuma J., Tůmová M., Vassilieva A.B., Chen T.W., Geisen S., Schmidt O., Tiunov A.V., Scheu S. 2022. Feeding habits and multifunctional classification of soil‐associated consumers from protists to vertebrates. Biological Reviews, 97: 1057-1117. https://doi.org/10.1111/brv.12832
  41. Pen-Mouratov S., Dayan T. 2019. Effect of piscivorous and omnivorous colonial birds' activity on structure, abundance and diversity of soil free-living nematodes. Preliminary results from a study of the impact of avifauna on soil biota in Israel's Mediterranean Coastal Plain. Ecol. Indic., 107. 105211. https://doi.org/10.1016/j.ecolind.2019.02.053
  42. Prince AL. 1995. Appendix–Methods in soil analysis, In Bear, F.E. (ed), Chemistry of Soil. ACS Monograph 126, Reinhold Publishing Corporation. New York. 328-362.
  43. Rajski A. 1967. Autecological-zoogeographical analysis of moss mites (Acari, Oribatei) on the basis of fauna in the Poznan environ. Part I. Pol. Pismo Entomol. 37:69 -166. https://doi.org/10.3161/00159301FF1968.14.12.277
  44. Rajski A. 1968. Autecological-zoogeographical analysis of moss mites (Acari, Oribatei) on the basis of fauna in the Poznan environ. Part II. - Fragm. Faun., 14:277-405. https://doi.org/10.3161/00159301FF1968.14.12.277
  45. R Core Team (2020). R: A language and environment for statistical computing. R Foundation for Statistical Computing, Vienna, Austria. URL https://www.R-project.org/.
  46. RStudio Team (2020). RStudio: Integrated Development for R. RStudio, PBC, Boston, MA URL http://www.rstudio.com/.
  47. Seniczak S., Chachaj B., Wasinska B., Graczyk R. 2006. Effect of ammonia water on seasonal dynamics of the density of Oribatida [Acari] in a lowland meadow. Biol. Lett., 43(2).
  48. Seniczak A., Seniczak S., Słowikowska M., Paluszak Z. 2017. The effect of different diet on life history parameters and growth of Oppia denticulata (Acari: Oribatida: Oppiidae). Syst. Appl. Acarol., 22(5):749-758. https://doi.org/10.11158//saa.22.5.12
  49. Skubała P., Kalinka R. 2006. Oribatid mite fauna (Acari: Oribatida) in selected biotopes of the Silesian Botanical Park at Mikołów. In: Gabryś G, Ignatowicz S. editors. Advances in Polish Acarology. Publishing house SGGW. Warszawa. p.356-366.
  50. Skubała P., Maślak M. 2010. Succession of oribatid fauna (Acari, Oribatida) in fallen spruce trees: Deadwood promotes species and functional diversity. In: Sabelis M., Bruin J., editors. Trends in Acarology. Proceedings of the 12th International Congress. Springer. Dordrecht. 123-128. https://doi.org/10.1007/978-90-481-9837-5_19
  51. Sobczyński T., Joniak T. 2009. Vertical changeability of physical-chemical features of bottom sediments in three lakes, in aspect type of water mixis and intensity of human impact. Pol. J. Environ. Stud. 18(6): 1093-1099.
  52. StatSoft, Inc. 2011. STATISTICA (Data Analysis Software System), Version 10. http://www.statsoft.com
  53. Subías LS. 2004., updated 2021. Listado sistemático, sinonímico y biogeográfico de los ácaros oribátidos (Acariformes: Oribatida) del mundo (Excepto fósiles)(16ª actualización) [Systematic, synonymic and biogeographic list of the oribatid mites (Acariformes: Oribatida) of the world (Except fossils) (16th update)]. Graellsia. 60:1-532. https://doi.org/10.3989/graellsia.2004.v60.iExtra.218
  54. Van Reeuwijk LP. 2002. Procedures of soil analysis. ISRIC. Wageningen.
  55. Wang Q., Li Y., Wang Y. 2011. Optimizing the weight loss-on-ignition methodology to quantify organic and carbonate carbon of sediments from diverse sources. Environ. Monit. Assess., 174(1): 241-57. https://doi.org/10.1007/s10661-010-1454-z
  56. Wasinska-Graczyk B., Seniczak S., Graczyk R. 2009. Effects of liquid pig manure fertilization on the density and species structure of Oribatida (Acari) and green forage yield in a lowland meadow in Poland. Biol. Lett., 46(2):57-62. https://doi.org/10.2478/v10120-009-0001-5
  57. Weigmann G., Kratz WR. 1981. Die deutschen Hornmilbenarten und ihre ökologische Charakteristik [The German beetle mite species and their ecological characteristics]. Zool Beitr. 27:459-489. In German.
  58. Weigmann G. 2006. Hornmilben (Oribatida). Die Tierwelt Deutschlands. 76. Teil. Goecke & Evers.Keltern. pp. 520.
  59. Weihrauch D., Donini A., O'Donnell MJ. 2012. Ammonia transport by terrestrial and aquatic insects. J. Insect Physiol., 58(4):473-487. https://doi.org/10.1016/j.jinsphys.2011.11.005
  60. Żbikowska-Zdun K., Piksa K., Watrak I. 2006. Diversity of mites (Acari: Oribatida) in selected microhabitats of the bug river protected landscape area. Biol. Lett., 43(2):277-286.
  61. Zmudczyńska-Skarbek K., Barcikowski M., Drobniak S.M., Gwiazdowicz D.J., Richard P., Skubała P., Stempniewicz L. 2017. Transfer of ornithogenic influence through different trophic levels of the Arctic terrestrial ecosystem of Bjørnøya (Bear Island), Svalbard. Soil Biol. Biochem., 115: 475-489. https://doi.org/10.1016/j.soilbio.2017.09.008


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Date received:
2022-05-26
Date accepted:
2022-09-20
Date published:
2022-09-26

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Baumann, Julia

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2022 Oszust, Mateusz and Klimaszyk, Piotr
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