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Did mangrove communities exist in the Late Cretaceous of the Kristianstad Basin, Sweden?
Naturhistoriska riksmuseet, Enheten för paleobiologi.ORCID-id: 0000-0001-6723-239X
Centre for Energy Geoscience, School of Earth Sciences, The University of Western Australia, Perth 6009, Australia.
Department of Earth and Planetary Sciences, Western Australian Museum, Welshpool, WA 6106, Australia.
Department of Geology, Lund University, S-223 62 Lund, Sweden.
2018 (Engelska)Ingår i: Palaeogeography, Palaeoclimatology, Palaeoecology, ISSN 0031-0182, E-ISSN 1872-616X, Vol. 498, s. 99-114Artikel i tidskrift (Refereegranskat) Published
Abstract [en]

Previous inferences of oyster-dominated communities occupying mangrove-like depositional settings in the Kristianstad Basin, Sweden, during the late early Campanian are reassessed. A significant percentage of oysters (Acutostrea incurva) from the Belemnellocamax mammillatus zone in Bed 3 at Åsen bear indentations on their left valves indicating attachment to plant axes. Many of these axes bear morphological features characteristic of the distal subaerial portions of woody plant branches and appear to have been rafted into the marine environment rather than representing in situ mangrove stems and roots. Foraminiferal assemblages recovered from sediment within the oyster body cavities differ from modern mangrove-community associations by the absence of siliceous agglutinated Foraminifera, the presence of diverse and relatively abundant Lagenida, relatively common triserial Buliminida, and a notable percentage of planktonic taxa. Chondrichthyan teeth assemblages from the same beds are similarly incompatible with the interpretation of a mangrove depositional environment based on comparisons with the distribution of related extant taxa. Apart from oyster shells and belemnite rostra, these beds are notably depauperate in diversity and abundance of macroinvertebrate remains compared with coeval carbonate shoal and rocky shoreline assemblages from the same basin. The collective palaeontological and sedimentological evidence favours an inner neritic sandy-substrate setting, but not nearshore or mangrove-like depositional environment for the oyster-rich Bed 3 at Åsen. The absence of mangrove-like assemblages at Åsen is consistent with the development of modern mangrove ecosystems much later (during the Maastrichtian and Cenozoic) based on the global palynological record.

Ort, förlag, år, upplaga, sidor
Amsterdam: Elsevier, 2018. Vol. 498, s. 99-114
Nyckelord [en]
Campanian, oysters, conifers, Foraminifera, sharks, mangroves, Sweden
Nationell ämneskategori
Annan geovetenskap och miljövetenskap
Forskningsämne
Den föränderliga jorden
Identifikatorer
URN: urn:nbn:se:nrm:diva-2906DOI: 10.1016/j.palaeo.2018.03.007OAI: oai:DiVA.org:nrm-2906DiVA, id: diva2:1258006
Forskningsfinansiär
Vetenskapsrådet, 2014-5234
Anmärkning

Additional funding from:

National Science Foundation (project #1636625).

Excavations at Åsen in 2010–2012 were supported by grants from the Royal Physiographical Society of Lund

Tillgänglig från: 2018-10-23 Skapad: 2018-10-23Bibliografiskt granskad

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