000331675 001__ 331675 000331675 005__ 20210406110634.0 000331675 037__ $$aPUBDB-2017-08001 000331675 041__ $$aEnglish 000331675 1001_ $$0P:(DE-H253)PIP1008646$$aHammel, Joerg$$b0$$eCorresponding author 000331675 1112_ $$aInvited talk by the Division Morphology at 108. Jahresversammlung der Deutschen Zoologischen Gesellschaft$$cGraz$$d2015-09-09 - 2015-09-12$$wAustria 000331675 245__ $$aMoving fluids for live – a sponge perspective 000331675 260__ $$c2015 000331675 3367_ $$033$$2EndNote$$aConference Paper 000331675 3367_ $$2DataCite$$aOther 000331675 3367_ $$2BibTeX$$aINPROCEEDINGS 000331675 3367_ $$2DRIVER$$aconferenceObject 000331675 3367_ $$2ORCID$$aLECTURE_SPEECH 000331675 3367_ $$0PUB:(DE-HGF)6$$2PUB:(DE-HGF)$$aConference Presentation$$bconf$$mconf$$s1501239638_12622$$xInvited 000331675 520__ $$aSessile filter feeding animals, including sponges (Porifera), rely on efficient fluid transport systems tokeep energy expenditure for water processing low. As a consequence of the sponge canal systemcomplexity only limited data on flow velocities and transport rates are available. This restricts ourunderstanding of this central anatomical structure and related physiological processes, functionalmorophological principles and ecology. Obtaining experimental measurements from internal parts ofthe canal system is almost impossible for most species. Therefore data are mainly based ontheoretical assumptions. This is linked to the limited availability of detailed morphometric andquantitative data on canal system architecture. Here I discuss experimental and in silico results onflow studies in marine and fresh water sponges. Canal system models based on SR-µCT data allowedfor the setup of finite element models to study flow inside the aquiferous system and the influence ofspecific canal system elements (bypasses and cellular structures). In order to calibrate the model andverify results flow velocity measurements by particle tracking velocimetry have been performed.Observed flow velocities in canal segments of diverse hierarchical orders differ from predictions basedon the classical hierarchical model of flow for sponges which reported much higher and fasterincreasing flow velocities towards the osculum. This is a consequence of the aquiferous systemarchitecture which displays a compensating increase in available canal volume. With the ability toactively change canal diameters and aperture openings in the canal system sponges are most likelyable to fine tune internal flow velocities and perfusion rates of specific areas of their body. 000331675 536__ $$0G:(DE-HGF)POF3-6G3$$a6G3 - PETRA III (POF3-622)$$cPOF3-622$$fPOF III$$x0 000331675 536__ $$0G:(DE-H253)I-20100327$$aFS-Proposal: I-20100327 (I-20100327)$$cI-20100327$$x1 000331675 536__ $$0G:(DE-H253)I-20110915$$aFS-Proposal: I-20110915 (I-20110915)$$cI-20110915$$x2 000331675 536__ $$0G:(DE-H253)I-20120218$$aFS-Proposal: I-20120218 (I-20120218)$$cI-20120218$$x3 000331675 693__ $$0EXP:(DE-H253)P-P05-20150101$$1EXP:(DE-H253)PETRAIII-20150101$$6EXP:(DE-H253)P-P05-20150101$$aPETRA III$$fPETRA Beamline P05$$x0 000331675 8564_ $$uhttp://www.dzg-ev.de/de/jahrestagung/2015_graz108/dzg2015_abstracts_final.pdf 000331675 909CO $$ooai:bib-pubdb1.desy.de:331675$$pVDB 000331675 9101_ $$0I:(DE-HGF)0$$6P:(DE-H253)PIP1008646$$aExternes Institut$$b0$$kExtern 000331675 9131_ $$0G:(DE-HGF)POF3-622$$1G:(DE-HGF)POF3-620$$2G:(DE-HGF)POF3-600$$3G:(DE-HGF)POF3$$4G:(DE-HGF)POF$$9G:(DE-HGF)POF3-6G3$$aDE-HGF$$bForschungsbereich Materie$$lVon Materie zu Materialien und Leben$$vFacility topic: Research on Matter with Brilliant Light Sources$$x0 000331675 9201_ $$0I:(DE-H253)HZG-20120731$$kHZG$$lZentrum für Material- und Küstenforschung$$x0 000331675 980__ $$aconf 000331675 980__ $$aVDB 000331675 980__ $$aI:(DE-H253)HZG-20120731 000331675 980__ $$aUNRESTRICTED