| Literature DB >> 31294213 |
Inês Barros1,2, Hugo Froufe3, George Marnellos4, Conceição Egas3, Jennifer Delaney4, Michele Clamp5, Ricardo Serrão Santos1,2,6, Raul Bettencourt1,2,6.
Abstract
BACKGROUND: The deep-sea mussels Bathymodiolus azoricus (Bivalvia: Mytilidae) are the dominant macrofauna subsisting at the hydrothermal vents site Menez Gwen in the Mid-Atlantic Ridge (MAR). Their adaptive success in such challenging environments is largely due to their gill symbiotic association with chemosynthetic bacteria. We examined the response of vent mussels as they adapt to sea-level environmental conditions, through an assessment of the relative abundance of host-symbiont related RNA transcripts to better understand how the gill microbiome may drive host-symbiont interactions in vent mussels during hypothetical venting inactivity.Entities:
Keywords: Bathymodiolus azoricus; RNA-seq; host-microbe interactions; hydrothermal vent; long term acclimatization; metatranscriptome; symbionts
Year: 2018 PMID: 31294213 PMCID: PMC6604929 DOI: 10.3934/microbiol.2018.2.240
Source DB: PubMed Journal: AIMS Microbiol ISSN: 2471-1888
Figure 1.Workflow diagram representing data processing pipeline for metatranscriptome analysis and annotation of B. azoricus gill holobiome.
HiSeq Illumina data set from B. azoricus gill tissues.
| Time points | Raw data | Duplicates | Dup% | rRNA LSU | rRNA LSU% | rRNA SSU | rRNA SSU% | Putative mRNA | Putative mRNA% | mRNA pair1/pair2 |
| 0 h | 16 277 124 | 8 964 678 | 55.08% | 4 159 716 | 25.56% | 1 803 216 | 11.08% | 1 349 514 | 8.29% | 25784/26323 |
| 12 h | 16 799 796 | 8 753 076 | 52.1% | 4 804 896 | 28.6% | 2 258 626 | 13.44% | 983 198 | 5.85% | 17029/17580 |
| 24 h | 15 582 702 | 8 678 798 | 55.7% | 4 204 320 | 26.98% | 2 120 264 | 13.61% | 579 320 | 3.72% | 18511/19512 |
| 36 h | 18 844 606 | 9 950 220 | 52.8% | 5 472 662 | 29.04% | 2 454 942 | 13.03% | 966 782 | 5.13% | 18511/19512 |
| 48 h | 16 505 724 | 9 049 980 | 54.83% | 4 714 292 | 28.56% | 2 111 882 | 12.79% | 629 570 | 3.81% | 8395/9076 |
| 72 h | 18 342 152 | 9 779 684 | 53.32% | 5 276 664 | 28.77% | 2 185 178 | 11.91% | 1 100 626 | 6,00% | 14898/15301 |
| 1 w | 16 086 918 | 9 229 370 | 57.37% | 4 265 494 | 26.52% | 1 791 380 | 11.14% | 800 674 | 4.98% | 16671/16827 |
| 2 w | 11 755 104 | 7 012 148 | 59.65% | 3 197 050 | 27.2% | 1 157 994 | 9.85% | 387 912 | 3.3% | 5079/5555 |
| 3 w | 17 237 480 | 10 939 364 | 63.46% | 4 232 038 | 24.55% | 1 623 300 | 9.42% | 442 778 | 2.57% | 8959/9350 |
| 4 w | 18 929 698 | 12 350 284 | 65.24% | 4 469 100 | 23.61% | 1 653 418 | 8.73% | 456 896 | 2.41% | 8026/8486 |
| 5 w | 15 623 958 | 9 989 130 | 63.93% | 3 848 086 | 24.63% | 1 394 758 | 8.93% | 391 984 | 2.51% | 5694/6312 |
Figure 2.Taxonomy summary plots. 16S and 18S OTUs taxonomical assignments are shown as a bar chart. Abundance of 16S and 18S reads assigned to each taxon reflects the height of the bar. Main Gammaproteobacteria representatives are shown as Oceanospirillales Thiotrichales and Methylococcales.
Figure 3.Functional summary plots. A: Functionally important transcript categories of B. azoricus-endosymbiont transcriptome according to KEGG database assignment. B: Time-dependent transcript expression trends during experimental acclimatization at atmospheric pressure.
Alpha diversity estimators from 16S rRNA and 18S rRNA.
| Time points | Observed species | Chao1 | Shannon index | Equitability | Good's coverage |
| 0 h | 1003 | 1593.5 | 4.209 | 0.4222 | 0.9995 |
| 12 h | 894 | 1565.1 | 4.135 | 0.4218 | 0.9996 |
| 24 h | 793 | 1352.6 | 3.970 | 0.4122 | 0.9997 |
| 36 h | 842 | 1439.4 | 4.113 | 0.4233 | 0.9997 |
| 48 h | 1060 | 2027.4 | 4.300 | 0.4279 | 0.9995 |
| 72 h | 1138 | 1993.8 | 4.143 | 0.4081 | 0.9995 |
| 1 w | 1727 | 2786.9 | 4.219 | 0.3923 | 0.9993 |
| 2 w | 1199 | 2103.1 | 3.415 | 0.3339 | 0.9991 |
| 3 w | 2096 | 3029.8 | 3.995 | 0.3621 | 0.9991 |
| 4 w | 2320 | 3789.1 | 3.874 | 0.3465 | 0.9990 |
| 5 w | 1342 | 2298.2 | 3.045 | 0.2931 | 0.9992 |
Figure 4.Rarefaction curves of Chao1 diversity.