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Novel reference transcriptomes for the sponges Carteriospongia foliascens and Cliona orientalis and associated algal symbiont Gerakladium endoclionum

  • Brian W. Strehlow*
  • , Mari Carmen Pineda
  • , Carly D. Kenkel
  • , Patrick Laffy
  • , Alan Duckworth
  • , Michael Renton
  • , Peta L. Clode
  • , Nicole S. Webster
  • *Kontaktforfatter
  • Australian Institute of Marine Science
  • Western Australian Marine Science Institution
  • University of Southern California
  • The University of Western Australia
  • The University of Queensland

Publikation: Bidrag til tidsskriftKommentar/debatForskningpeer review

Abstract

Sponge transcriptomes are important resources for studying the stress responses of these ecologically important filter feeders, the interactions between sponges and their symbionts, and the evolutionary history of metazoans. Here, we generated reference transcriptomes for two common and cosmopolitan Indo-Pacific sponge species: Carteriospongia foliascens and Cliona orientalis. We also created a reference transcriptome for the primary symbiont of C. orientalis—Gerakladium endoclionum. Assemblies for C. foliascens, C. orientalis, and G. endoclionum contained 67,304, 82,895, and 28,670 contigs, respectively. Contigs represented 15,248–37,344 isogroups (~ genes) per assembly, and N50s ranged from 1672–4355 bp. Sponge transcriptomes were high in completeness and quality, with an average of 93% of core EuKaryotic Orthologous Groups (KOGs) and 98% of single-copy metazoan core gene orthologs identified. The G. endoclionum assembly was partial with 56% of core KOGs and 32% of single-copy eukaryotic core gene orthologs identified. These reference transcriptomes provide a valuable resource for future research assessing sponge stress responses.

OriginalsprogEngelsk
TidsskriftCoral Reefs
Vol/bind40
Udgave nummer1
Sider (fra-til)9-13
ISSN0722-4028
DOI
StatusUdgivet - feb. 2021

Finansiering

This research was funded by the Western Australian Marine Science Institution (WAMSI) as part of the WAMSI Dredging Science Node and made possible through investment from Chevron Australia, Woodside Energy Limited, BHP Billiton as environmental offsets and by co-investment from the WAMSI Joint Venture partners. The views expressed herein are those of the authors and not necessarily those of WAMSI. Brian W. Strehlow was supported by a University of Western Australia (UWA) Scholarship for International Research Fees, University International Stipend, and UWA Safety-Net Top-Up Scholarships. Brian W. Strehlow was further supported by the Villum Investigator Grant awarded to Don Canfield (No. 16518). The funders had no role in study design, data collection, and analysis, decision to publish, or preparation of the manuscript. The authors are grateful to E. Botté and G. Millar for their assistance with computing issues. They also thank the staff at the AIMS National Sea Simulator for their expertise and assistance in the tank-based experiments. The authors acknowledge the Manburra People, as the Traditional Owners of the sea country where this work took place. We pay our respects to their elders’ past, present and emerging, and we acknowledge their continuing spiritual connection to their sea country.

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