Graptolites were pelagic organisms.
Graptolites are widely recognized in the paleontological literature as having been pelagic or macroplanktonic organisms drifting in the water column.
The retrieved papers consistently treat graptolites as pelagic, planktonic, or macroplanktonic marine organisms whose distribution was driven by oceanic water masses and depth zones. No papers refute this long-established paleontological consensus.
Charles Mitchell, Edsel D. Brussa, Jörg Maletz. A mixed isograptid-didymograptid graptolite assemblage from the Middle Ordovician of west Gondwana (NW Bolivia): Implications for graptolite paleoecology. 2008. https://doi.org/10.1666/06-069.1
This study discusses graptolite paleoecology, specifically noting that certain taxa inhabited the epipalagic or epipelagic realm.
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Sheets HD, Mitchell CE, Melchin MJ, Loxton J, Štorch P, Carlucci KL, Hawkins AD. Graptolite community responses to global climate change and the Late Ordovician mass extinction.. 2016. https://doi.org/10.1073/pnas.1602102113
This study analyzes macroplanktonic graptolite faunas and their responses to oceanic water masses and climate change.
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