European charophyte evolution across the Cretaceous–Paleogene boundary

Vicente, Alba; Csiki-Sava, Zoltán; Martı́n-Closas, Carles

doi:10.1016/j.palaeo.2019.109244

Cited by 18 publications

(16 citation statements)

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“…Modern charophytes are typical inhabitants of freshwater (non‐marine) environments, but a few can tolerate some salinity, though they are not suited to grow in an open marine environment (Schubert, Marquardt, Schories, & Blindow, 2015; Vicente et al, 2019; Vicente, Expósito, et al, 2016; Vicente, Villalba‐Breva, et al, 2016; Villalba‐Breva & Martín‐Closas, 2011, 2013). They flourish in almost all inland waters, particularly in slow‐flowing rivers and streams, and lake and pond bottoms (temporary and permanent), and are able to live in sand and silt substrates, and marl‐rich lacustrine environments (Barbosa, Lefler, Berthold, & Laughinghouse, 2021).…”

Section: Discussionmentioning

confidence: 99%

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Charophytes from theCretaceous–Palaeogenetransition in the Jhilmili intertrappean beds of Central India

et al. 2022

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The Jhilmili intertrappean beds (Chhindwara District, Madhya Pradesh) of Central India are studied from a palaeoenvironmental, palaeoecological, and palaeobiogeographical perspective using fossil charophytes. These beds have yielded a diverse charophyte assemblage, consisting of Platychara perlata, Platychara raoi, Platychara sahnii, Peckichara cf. varians, Nemegtichara cf. grambasti, and Chara sp. 1. These charophytes were recovered from a 60 cm thick clayey and nodular limestone unit that is underlain by claystone and overlain by laminated claystones deposited on fluvial floodplains. This charophyte assemblage suggests a Late Cretaceous-Early Danian age, which agrees with the previous dating carried out using freshwater to brackish water ostracods and planktic foraminifera found in the same beds, together with dasycladalean and halimedacean chlorophytes. The Jhilmili intertrappean charophyte assemblage resembles those found in other infra-and intertrappean sections of western, central, and southern India. The charophyte assemblage indicates that during the Cretaceous-Palaeogene timespan the Indian subcontinent mainly experienced interchange with Laurasia (China, Europe, and North America) but also with Gondwana (North Africa and South America). In the opposite sense, Laurasian species might have dispersed to India by means of a sweepstakes route across the Kohistan-Dras volcanic arcs.

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Section: Discussionmentioning

confidence: 99%

“…The Characeae family largely dominated the Late Cretaceous charophyte flora while clavatoraceans and porocharaceans become extinct close to the K-Pg boundary (Feist, Grambast-Fessard, et al, 2005;Feist, Liu, & Tafforeau, 2005;Grambast, 1974;Vicente et al, 2019).…”

Section: Palaeobiogeographical Implicationsmentioning

confidence: 99%

Charophytes from theCretaceous–Palaeogenetransition in the Jhilmili intertrappean beds of Central India

et al. 2022

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“…Despite the growing interest in the history of Lychnothamnus (Soulié‐Märsche, 1989; Musacchio, 2010; Vicente, Csiki‐Sava & Martín‐Closas, 2019), its fossil record is known only from a few sites covering parts of the Holocene period. For instance, Lychnothamnus gyrogonites were found in palaeolacustrine sediments in the central Sahara (Petit‐Maire & Riser, 1981), the Ganga Plain (India) sediments (Bhatia, 2006), and Lake Shkodra (Albania), where the disappearance of L. barbatus occurred approximately 1,300 cal.…”

Section: Discussionmentioning

confidence: 99%

“…Soulié-Märsche, 1989;Musacchio, 2010;Vicente, Csiki-Sava & Martín-Closas, 2019), its fossil record is known only from a few sites covering parts of the Holocene period. For instance, Lychnothamnus gyrogonites were found in palaeolacustrine sediments in the central Sahara(Petit-Maire & Riser, 1981), the…”

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confidence: 99%

Preliminary evidence of an endangered species benefiting from moderate climate warming: A palaeolimnological study of the charophyte Lychnothamnus barbatus

Brzozowski

Kowalewski

Szczuciński

et al. 2021

Aquatic Conservation

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In a time of rapid environmental changes, identification of the effects of climate warming on charophytes (Characeae, Charophyta) will enable the optimization of conservation measures, especially for extremely rare species. Lychnothamnus barbatus is one of the rarest charophytes worldwide, which has decreased in the number of occupied sites over the last century. However, the recolonization of former sites has been observed in recent years (e.g. Lake Kuźnickie, Poland). The study aimed to analyse the effects of climatic changes and human pressure on the L. barbatus population. Three 30 cm sediment cores were collected from minimum, average, and maximum depths of L. barbatus occurrence to determine the past vegetation composition. Sediment cores were dated using the radioisotopes lead‐210, caesium‐137, and carbon‐14. A spatial analysis of the lake catchment changes during the last 120 years was also conducted. The study demonstrated L. barbatus presence in Lake Kuźnickie at the beginning of the 16th century. However, a sharp increase in the proportion of this species in the vegetation community occurred in the 19th century and during climate warming at the end of the Little Ice Age. Factors that significantly influenced the present occurrence of the L. barbatus population included improvement in water quality and the oospore bank deposited in the bottom sediments. This study is the first palaeoreconstruction in a modern lake dominated by L. barbatus. Based on the history of L. barbatus in Lake Kuźnickie after the end of the Little Ice Age, the positive effect of climate warming on the contemporary recovery of this charophyte is postulated. The reaction of L. barbatus to climate warming appears to differ from commonly accepted scenarios for aquatic macrophytes because its recovery in the past and at present coincided with increases in air temperature. This research indicated the appropriate management and conservation practices for lakes with L. barbatus populations.

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“…9B, C), from the lower La Scoaba level; LPB (FGGUB) M.1699, incomplete left p4, anterior crown fragment, from the upper La Scoaba level. The M2 was found associated only with gastropod shell fragments and indeterminate bone chips, whereas the p4 is part of a richer microfossil assemblage, including characeans (Vicente et al, 2019), as well as gastropods, ostracods, and isolated amphibian remains (anurans, albanerpetontids), an assemblage that is still largely under study (see Csiki-Sava et al, 2016). The overall fossiliferous content of the La Scoaba succession was reviewed by Csiki-Sava et al (2016).…”

Section: Site Sp3mentioning

confidence: 99%

Spatial and Temporal Distribution of the Island-Dwelling Kogaionidae (Mammalia, Multituberculata) in the Uppermost Cretaceous of Transylvania (Western Romania)

Csiki-Sava

Vremir²,

Meng

et al. 2022

Bulletin of the American Museum of Natural History

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CONTENTS FADSUTACTS Fat ech) ode Baa ee tes 4 hehe AIRY Rye torte Ny sands ARLE bes Gumbtae tare RT NS se eaa seniors 3 INtFOGUICH ONS. soe Pet eocdeks Baer eh T rains DEN D deze tee Ore Rm ke a cis Ee oRralon Poa Meas arerop Peers 3 The,Manimals-of the dtateos islands), tesut ts crc tvs, yy sede ates Paras hing ane aedaetegetd cesccee Weg, a ae 4 ADDICViAtlONS ee. oy site cheeses one tates Saleen sehen te ait re gine hereetinte aan clay ure ghee ee acy eee 7 Geological Setting and Mammalian Fossiliferous Content of the Continental Uppermost Cretacecus-ol: Transylvalilaers .ccr 5m) Rages fdas eh wal seh MLAS ELA het LI eS sae RR 8 Kogaionidae in-Phyloseny, Space; and Time 37. psec. aac sau Pete orate oq ae se dndde exe sues 9 The Current Fossil Record of the Latest Cretaceous Transylvanian Kogaionids .............. Kosaionid Occorrentessitp thie Hates, Basin! eee 2 ok. ieee enya eb ns ote cecede ns gree tee Se I SINISE FOLMIACIGIT oye scteres hy te RR ew crete t s NV Re A bE CS AY ces eA REO ANY cra ance Peal Nee Rail Mare Bods suman id. ge tanya ace ah T dpe Pic deena eee pet ate et seth ate kaa AUT Beer ¢ CRs Rae DUO Cae ec Me ry LOC a Lae MO NERY oe CUS wig Ucar SLO EM Rg, Ree aaa Eren Denises Ci ealaM Por mati, 15 >see sate tds Bin Seals Me pee OT a te ee PIR Re WNT at Malta Kogaionid Occurrences in the Rusca Montana. Basin 24 oes aon epteee leeee pe Kogaionid Occurrences im the Transyivanian Basins: phan con Pera ite sont wre dork ES Spatiotemporal Distribution Patterns of the Latest Cretaceous Transylvanian Kogaionids..... 7 Chronostratierapiic Distribatione. ¢ osc tutes eets asus § tee eas ae ohn ae dig ghetemrtattns eke aise a BOGVASI Ze DTSCE HOUT OUT 12 ate vets tee ones ots aun Fe ngtnee Dh tel ob te ee tata oy xe al BY hE at Sedimentary Facies Dependence and Preservation Style .......... 0... cc eee ee eee eee CoOneliding SUMMA. sta 5 oe Gar wtades ol o wage Paes Maw ae Ga aide age osetia Acknowledoments nthe. els tonsa aagradtas file Ser 2a hate thats Ble ton. d-> aerate ale fer ahd FRETSECIICES. asp Aesehyits Nat, Atay le ayes Ween Behe SNE, le Soa Masti ln Linke, beatae tle yale: Wieden Bah tle, Me genta anes, ®

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European charophyte evolution across the Cretaceous–Paleogene boundary

Cited by 18 publications

References 45 publications

Charophytes from theCretaceous–Palaeogenetransition in the Jhilmili intertrappean beds of Central India

Charophytes from theCretaceous–Palaeogenetransition in the Jhilmili intertrappean beds of Central India

Preliminary evidence of an endangered species benefiting from moderate climate warming: A palaeolimnological study of the charophyte Lychnothamnus barbatus

Spatial and Temporal Distribution of the Island-Dwelling Kogaionidae (Mammalia, Multituberculata) in the Uppermost Cretaceous of Transylvania (Western Romania)

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