FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2000596981> ?p ?o ?g. }

• W2000596981 endingPage "91" @default.
• W2000596981 startingPage "75" @default.
• W2000596981 abstract "Paleoecological responses to coupled geomorphic and hydrological changes have rarely been studied using a multiproxy approach in freshwater floodplain wetlands of semiarid Australia. The Macquarie Marshes are a large, multi-channelled and morphodynamic floodplain wetland system in the lowland interior of the Murray-Darling Basin, southeastern Australia. Evidence from historical maps, aerial photographs, geomorphology and sedimentology indicate that avulsion in the southern Macquarie Marshes caused the formation of a major new channel (Monkeygar Creek) and the abandonment of a reach of the Macquarie River in the last 200 years. Paleobiological samples from near-uniform sediment cores were studied to determine the environmental changes related to this avulsion, as well as associated floodplain evolution and hydrological changes in the adjoining flood-reliant wetlands. Fifteen macrophyte taxa, seven charophyte taxa, 28 diatom taxa and 18 aquatic invertebrate taxa were identified in sediments from the terminal reach of the Macquarie River and the active lower reach of Monkeygar Creek. Paleoecological reconstruction indicates that the slowly accreting marsh (ca 0.032 to 0.037 cm a−1) around the Macquarie River (Terminus Marsh) was more frequently and deeply inundated in the past (presence of limnetic zooplankton before ca 1626 cal. years BP) than during the penultimate pre-avulsion phase (absence of limnetic zooplankton and more diverse terrestrial and aquatic vegetation from ca 540 cal. years BP). In contrast, the floodplain near lower Monkeygar Creek was only periodically inundated prior to avulsion (high diversity of charophytes and low diversity of diatoms and invertebrates before ca 149 years BP), before experiencing disturbance, rapid accretion and ecological succession during the avulsion (paucity of wetland biota in distinct flood facies ca 149 years BP). This part of the floodplain became a substantial wetland, dominated by algae (charophytes and diatoms) and submerged macrophytes, due to a more consistent flood regime following the avulsion. The contemporary marsh on lower Monkeygar Creek has evolved in the last ca 54 years into a shallower, less frequently flooded wetland (new dominance of emergent macrophytes, charophytes and littoral cladocerans), probably due to changes in inundation caused by rapid local floodplain accretion (ca 0.409 to 0.556 cm a−1) and possibly river regulation. This multiproxy approach provides some of the first evidence of significant changes in wetland communities and ecological successions that are directly related to the geomorphic processes of avulsion and floodplain evolution in a semiarid wetland system such as the Macquarie Marshes." @default.
• W2000596981 created "2016-06-24" @default.
• W2000596981 creator A5003880889 @default.
• W2000596981 creator A5024956751 @default.
• W2000596981 creator A5027752274 @default.
• W2000596981 creator A5035099191 @default.
• W2000596981 creator A5035381379 @default.
• W2000596981 creator A5082395580 @default.
• W2000596981 creator A5091483984 @default.
• W2000596981 date "2011-02-01" @default.
• W2000596981 modified "2023-10-06" @default.
• W2000596981 title "Paleoecological responses to avulsion and floodplain evolution in a semiarid Australian freshwater wetland" @default.
• W2000596981 cites W11890670 @default.
• W2000596981 cites W1597179471 @default.
• W2000596981 cites W1967348481 @default.
• W2000596981 cites W1967452773 @default.
• W2000596981 cites W1974123436 @default.
• W2000596981 cites W1977192625 @default.
• W2000596981 cites W1988451080 @default.
• W2000596981 cites W2002804085 @default.
• W2000596981 cites W2007318302 @default.
• W2000596981 cites W2014831772 @default.
• W2000596981 cites W2026388995 @default.
• W2000596981 cites W2043773914 @default.
• W2000596981 cites W2044027953 @default.
• W2000596981 cites W2058638765 @default.
• W2000596981 cites W2065906184 @default.
• W2000596981 cites W2071567586 @default.
• W2000596981 cites W2074413711 @default.
• W2000596981 cites W2074834271 @default.
• W2000596981 cites W2077109512 @default.
• W2000596981 cites W2084137732 @default.
• W2000596981 cites W2092121704 @default.
• W2000596981 cites W2109054304 @default.
• W2000596981 cites W2144262173 @default.
• W2000596981 cites W2152552999 @default.
• W2000596981 cites W2153499444 @default.
• W2000596981 cites W2156358294 @default.
• W2000596981 cites W2544774665 @default.
• W2000596981 cites W4229678515 @default.
• W2000596981 cites W4231824221 @default.
• W2000596981 doi "https://doi.org/10.1080/08120099.2010.534818" @default.
• W2000596981 hasPublicationYear "2011" @default.
• W2000596981 type Work @default.
• W2000596981 sameAs 2000596981 @default.
• W2000596981 citedByCount "27" @default.
• W2000596981 countsByYear W20005969812012 @default.
• W2000596981 countsByYear W20005969812013 @default.
• W2000596981 countsByYear W20005969812014 @default.
• W2000596981 countsByYear W20005969812015 @default.
• W2000596981 countsByYear W20005969812016 @default.
• W2000596981 countsByYear W20005969812017 @default.
• W2000596981 countsByYear W20005969812018 @default.
• W2000596981 countsByYear W20005969812019 @default.
• W2000596981 countsByYear W20005969812020 @default.
• W2000596981 countsByYear W20005969812021 @default.
• W2000596981 countsByYear W20005969812023 @default.
• W2000596981 crossrefType "journal-article" @default.
• W2000596981 hasAuthorship W2000596981A5003880889 @default.
• W2000596981 hasAuthorship W2000596981A5024956751 @default.
• W2000596981 hasAuthorship W2000596981A5027752274 @default.
• W2000596981 hasAuthorship W2000596981A5035099191 @default.
• W2000596981 hasAuthorship W2000596981A5035381379 @default.
• W2000596981 hasAuthorship W2000596981A5082395580 @default.
• W2000596981 hasAuthorship W2000596981A5091483984 @default.
• W2000596981 hasConcept C111201904 @default.
• W2000596981 hasConcept C111368507 @default.
• W2000596981 hasConcept C127313418 @default.
• W2000596981 hasConcept C132000320 @default.
• W2000596981 hasConcept C155681218 @default.
• W2000596981 hasConcept C186632785 @default.
• W2000596981 hasConcept C187320778 @default.
• W2000596981 hasConcept C18903297 @default.
• W2000596981 hasConcept C67268981 @default.
• W2000596981 hasConcept C67715294 @default.
• W2000596981 hasConcept C76886044 @default.
• W2000596981 hasConcept C86803240 @default.
• W2000596981 hasConceptScore W2000596981C111201904 @default.
• W2000596981 hasConceptScore W2000596981C111368507 @default.
• W2000596981 hasConceptScore W2000596981C127313418 @default.
• W2000596981 hasConceptScore W2000596981C132000320 @default.
• W2000596981 hasConceptScore W2000596981C155681218 @default.
• W2000596981 hasConceptScore W2000596981C186632785 @default.
• W2000596981 hasConceptScore W2000596981C187320778 @default.
• W2000596981 hasConceptScore W2000596981C18903297 @default.
• W2000596981 hasConceptScore W2000596981C67268981 @default.
• W2000596981 hasConceptScore W2000596981C67715294 @default.
• W2000596981 hasConceptScore W2000596981C76886044 @default.
• W2000596981 hasConceptScore W2000596981C86803240 @default.
• W2000596981 hasIssue "1" @default.
• W2000596981 hasLocation W20005969811 @default.
• W2000596981 hasOpenAccess W2000596981 @default.
• W2000596981 hasPrimaryLocation W20005969811 @default.
• W2000596981 hasRelatedWork W2019463735 @default.
• W2000596981 hasRelatedWork W2046845797 @default.
• W2000596981 hasRelatedWork W2130256892 @default.
• W2000596981 hasRelatedWork W2167604123 @default.
• W2000596981 hasRelatedWork W2246829106 @default.

• next