| Literature DB >> 30176793 |
Mingbo Yin1, Xiaoyu Wang2, Xiaolin Ma2, Sabine Gießler3, Adam Petrusek4, Johanna Griebel5, Wei Hu2, Justyna Wolinska5,6.
Abstract
BACKGROUND: The zooplanktonic cladocerans Daphnia, present in a wide range of water bodies, are an important component of freshwater ecosystems. In contrast to their high dispersal capacity through diapausing eggs carried by waterfowl, Daphnia often exhibit strong population genetic differentiation. Here, to test for common patterns in the population genetic structure of a widespread Holarctic species, D. galeata, we genotyped two sets of populations collected from geographically distant areas: across 13 lakes in Eastern China and 14 lakes in Central Europe. The majority of these populations were genotyped at two types of markers: a mitochondrial gene (for 12S rRNA) and 15 nuclear microsatellite loci.Entities:
Keywords: 12S rRNA; Cladocera; Cyclical parthenogenesis; Genetic variation; Microsatellites; Population structure
Mesh:
Substances:
Year: 2018 PMID: 30176793 PMCID: PMC6122193 DOI: 10.1186/s12862-018-1256-4
Source DB: PubMed Journal: BMC Evol Biol ISSN: 1471-2148 Impact factor: 3.260
Fig. 1Location of D. galeata samples from Eastern China (red dots) and Central Europe (green dots)
Genetic diversity of Daphnia galeata populations from Eastern China and Central Europe, based on 15 microsatellite loci and a mitochondrial gene (for 12S rRNA)
| Locality (abbreviation), habitat type, country | Sampling period | Latitude, longitude | Microsatellites | 12S | |||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Nmic | NMLG | MLG | R |
| Nseq | Nhapl |
|
| haplotypes (Nident) | ||||
| Europe | Ammersee (AMME)a, natural lake, DE | Autumn 2008 | 48°02′, 11°42′ | 12 | 12 | 11 | 0.91 | 2.57 | n.a. | ||||
| Böhmerweiher (BOHM)c, small flooded gravel pit, DE | Spring 2008 | 48°10′, 11°22′ | n.a. | 13 | 3 | 0.29 | 0.00067 | CES (11), BOHMa (1), BOHMb (1) | |||||
| Fasanariesee (FASA), small flooded gravel pit, DE | Spring 2011 | 48°12′, 11°31′ | 43 | 41 | 17 | 0.40 | 2.30 | 10 | 1 | 0 | 0 | CES (10) | |
| Feldmochinger See (FELD), small flooded gravel pit, DE | Spring 2009 | 48°07′, 11°18′ | 46 | 44 | 33 | 0.74 | 2.29 | 10 | 1 | 0 | 0 | CES (10) | |
| Feringasee (FERI)a,c, small flooded gravel pit, DE | Spring 2009 | 48°07′, 11°24′ | 32 | 31 | 31 | 1 | 2.80 | 19 | 3 | 0.20 | 0.00071 | ESa (17), FERIa (1), FERIb (1) | |
| Greifensee (GREI), natural lake, CH | Spring 2002 | 47°20′, 08°40′ | 36 | 35 | 21 | 0.59 | 3.49 | 10 | 2 | 0.53 | 0.00232 | CES (6), ESb (4) | |
| Goslawskie (GOSL), natural lake, PL | Spring 2014 | 52°18′, 18°15′ | 43 | 36 | 31 | 0.86 | 4.25 | 10 | 2 | 0.36 | 0.00232 | ESb (2), GOSLa (8) | |
| Heimstettener See (HEIM)a, small flooded gravel pit, DE | Spring 2008 | 48°06′, 11°26′ | 46 | 43 | 43 | 1 | 3.06 | n.a. | |||||
| Lerchenauer See (LERC), small flooded gravel pit, DE | Spring 2011 | 48°12′, 11°32′ | 45 | 44 | 31 | 0.70 | 3.07 | 10 | 1 | 0 | 0 | CES (10) | |
| Lußsee (LUSS), small flooded gravel pit, DE | Spring 2008 | 49°12′, 11°25′ | n.a. | 12 | 2 | 0.17 | 0.00037 | CES (11), LUSSa (1) | |||||
| Mueggelsee (MUEG), natural lake, DE | Spring 2016 | 52°26′, 13°38′ | 46 | 46 | 32 | 0.69 | 3.74 | 10 | 3 | 0.51 | 0.00385 | ESa (7), ESb (2), MUGGa (1) | |
| Římov (RIM), man-made reservoir, CZ | Autumn 2009 | 48°50′, 14°30′ | 46 | 46 | 31 | 0.67 | 3.40 | n.a. | |||||
| Vír (VIR), man-made reservoir, CZ | Autumn 2009 | 49°34′, 16°19′ | 46 | 16 | 15 | 0.93 | 3.71 | 10 | 3 | 0.38 | 0.00174 | CES (8), ESa (1), ESb (1) | |
| Želivka (ZEL), man-made reservoir, CZ | Summer 2009 | 49°43′, 15°06′ | 42 | 35 | 31 | 0.88 | 4.11 | 10 | 3 | 0.51 | 0.00358 | CES (1), ESa (2), ESb (7) | |
| China | Baoying Hu (BYH)b,d, natural lake | Spring 2012 | 33°06′, 119°08′ | 39 | 34 | 34 | 1 | 3.75 | 10 | 2 | 0.20 | 0.00218 | HS1 (9), CES (1) |
| Hewangba Reservoir (HWB)b, man-made reservoir | Spring 2013 | 32°32′, 118°50′ | 40 | 35 | 17 | 0.47 | 2.37 | 10 | 3 | 0.51 | 0.00121 | HS1 (7), HWBa (2), HWBb (1) | |
| Hung-tse Lake (HZH)b,d, natural lake | Spring 2012 | 33°13′, 118°18′ | 44 | 40 | 29 | 0.72 | 3.08 | 10 | 1 | 0 | 0 | HS1 (10) | |
| Jinniushan Reservoir (JNS)b, man-made reservoir | Spring 2013 | 32°28′, 118°57′ | 42 | 37 | 18 | 0.47 | 2.24 | 10 | 2 | 0.53 | 0.00116 | HS1 (4), HS4 (6) | |
| Luoma Hu (LMH)b,d, natural lake | Autumn 2012 | 34°07′, 118°11′ | 43 | 33 | 33 | 1 | 3.17 | 10 | 2 | 0.53 | 0.00116 | HS1 (6), HS4 (4) | |
| Shanhu Reservoir (SHR)b, man-made reservoir | Spring 2013 | 32°26′, 118°47′ | 22 | 17 | 17 | 1 | 2.50 | 10 | 1 | 0 | 0 | HS1 (10) | |
| Zaolin Reservoir (ZLR)b, man-made reservoir | Spring 2013 | 32°20′, 119°04′ | 42 | 34 | 31 | 0.91 | 2.50 | 10 | 1 | 0 | 0 | HS1 (10) | |
| Zhongshan Reservoir (ZSR)b,d, man-made reservoir | Autumn 2012 | 31°37′, 119°04′ | 41 | 34 | 22 | 0.64 | 2.30 | 10 | 1 | 0 | 0 | HS1 (10) | |
| Li Hu (LIH), natural lake | Spring 2012 | 31°19′, 120°09′ | 40 | 34 | 34 | 1 | 3.73 | 10 | 5 | 0.84 | 0.00741 | HS1 (3), CES (3), LIHa (1), LIHb (1), LIHc (2) | |
| Qinyun Hu (QYH)d, man-made reservoir | Spring 2012 | 35°54′, 117°48′ | 37 | 33 | 25 | 0.75 | 2.65 | 10 | 2 | 0.36 | 0.00387 | HS1 (2), CES (8) | |
| Jingdong Reservoir (JDR)d, man-made reservoir | Spring 2012 | 35°57′, 117°48′ | 45 | 24 | 11 | 0.43 | 2.20 | 10 | 1 | 0 | 0 | HS1 (10) | |
| Ying Hu (YIH)d, man-made reservoir | Autumn 2012 | 32°37′, 108°54′ | 44 | 26 | 21 | 0.80 | 3.06 | 10 | 3 | 0.62 | 0.00465 | HS1 (6), HS4 (2), CES (2) | |
| Dongzhang Reservoir (DZR), man-made reservoir | Spring 2013 | 25°42′, 119°16′ | 42 | 22 | 13 | 0.57 | 1.34 | 10 | 1 | 0 | 0 | HS1 (10) | |
Microsatellite data published in: a [24], b [19]. 12S data published in: c [42], d [15]. N number of genotyped individuals, N number of genotyped individuals with a complete multilocus genotype (MLG), MLG number of detected multilocus genotypes, R relative clonal richness, A allele richness, n.a. data not available, N number of sequenced individuals, N number of haplotypes per lake, h haplotype diversity per lake, π nucleotide diversity per lake, N a number in brackets indicates number of individuals possessing the identical sequence. Haplotype ID: CES: haplotype shared by China and Europe; ES: haplotypes shared among European populations; HS: haplotypes shared among Chinese populations (IDs are consistent with [15]). Countries are indicated by two-letter ISO codes in the second column
Fig. 2Results of the Factorial Correspondence Analysis (FCA) based on allelic variation at up to 15 microsatellite loci. a Species assignment of Daphnia individuals from Eastern China and Central Europe. Reference genotypes representing three species of the D. longispina complex and their interspecific hybrids (indicated by crosses) are included (for a list of all reference genotypes, see [20]). b Genetic similarities among pure D. galeata individuals sampled from Eastern China and Central Europe. For lake abbreviations see Table 1. Note that analyses in (a) and (b) are independent, and thus the axes are not comparable
Fig. 3Results from a Bayesian assignment analysis (STRUCTURE) of microsatellite data for: a all 25 D. galeata populations, b 12 European populations, and c 13 Chinese populations. The best K is equal to a 2, b 8 and c 2, according to the method reported in [33]. The assignment of each individual to the respective groups is given. For lake abbreviations see Table 1
Hierarchical analysis of molecular variance (AMOVA) for D. galeata populations, based on microsatellites and mtDNA, respectively. Between-region (i.e. Eastern China and Central Europe) variation is estimated in relation to within-region and within-population components
| Marker type | Source of variation | DF | Explained variation (%) |
|
|---|---|---|---|---|
| Microsatellites | Between regions | 1 | 32.80 | < 0.001 |
| Among populations (within region) | 23 | 18.91 | < 0.001 | |
| Among individuals (within population) | 1983 | 48.29 | < 0.001 | |
| mtDNA | Between regions | 1 | 71.67 | < 0.005 |
| Among populations (within region) | 22 | 12.62 | < 0.001 | |
| Among individuals (within population) | 230 | 15.71 | < 0.001 |
Fig. 4Scatterplot of pairwise geographical distance (kilometres) versus genetic distance (F based on up to 15 microsatellite loci) among D. galeata populations from a Eastern China and b Central Europe
Fig. 5a Bayesian phylogenetic tree and b haplotype network of D. galeata, based on the variation of the mitochondrial 12S rRNA gene (430 bp). Codes of Daphnia individuals are provided in Table 1; for origin of reference sequences see Additional file 1: Table S1. Less than 70% support of nodes is not shown. Daphnia hrbaceki was used as an outgroup. Each circle in b represents a unique haplotype, and its size reflects the number of individuals carrying that particular haplotype. Segment sizes within circles correlate with the distribution of haplotypes among different populations. Colour codes allow easy discrimination between European populations (purple to red) and Chinese ones (blue, green, grey) in the network. For lake abbreviations see Table 1