Pollen morphology of the Polish species of the family Caprifoliaceae. Part 2

Maciejewska, Iwona

doi:10.5586/asbp.1997.018

Cited by 6 publications

(6 citation statements)

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“…Remarks: Viburnum sp. corresponds in its morphological characters (tricolporate apertures, reticulate tectum, reticulum condensed in aperture areas, lumina with freestanding columellae) to the extant pollen of this genus (Maciejewska 1997), with closest similarities to pollen "class A" of Donoghue (1985), which is commonly found in this genus. Family Caprifoliaceae Juss., 1789 Subfamily Dipsacoideae Eaton Genus Dipsacus L., 1753/Cephalaria Schrad.…”

Section: Subfamily Cichorioideae Chevall 1828mentioning

confidence: 73%

The middle Miocene palynofloras of the Salihpaşalar lignite mine (Yatağan Basin, southwest Anatolia): environmental characterisation and comparison with palynofloras from adjacent basins

Bouchal

2018

Palaeobio Palaeoenv

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As the third part of an ongoing investigation of middle Miocene palynofloras in the Yatağan Basin (YB), southwestern Anatolia, the palynofloras of the Salihpaşalar lignite mine in the main YB were studied. Seven types of algal spores, aplanospores/zygospores or cysts, six types of lycophyte and fern spores, 12 types of gymnosperm pollen and 90 types of angiosperm pollen were identified. Of a total of ca. 140 plant taxa described from the YB, over 10% are confined to the Salihpaşalar assemblage. Differences between coeval palynofloras of the Sekköy Member might reflect changing or prograding depositional environments. A number of rare accessorial taxa reflect these local differences: Pilularia, Valeriana, Drosera and Persicaria aff. amphibia only occur at Salihpaşalar and are typical of shallow water or temporary ponds associated with a lake shore. Apart from this, all the palynofloras, originating from the lignite seams and overlying limnic limestones (uppermost Turgut and Sekköy Member), of the YB are strongly indicative of extensive woody vegetation with a dominance of diverse Fagaceae and Pinaceae. In addition, a list comparing the well-documented YB palynomorphs to morphologically similar palynomorphs of published late early to middle Miocene plant assemblages of western Anatolian was compiled. Such a comparison reveals that in many instances different taxon names have been used to denote the same taxa. Hence, resolving these synonymies is a prerequisite of any meaningful comparison of palynofloras in the region. Keywords Neogene. Western Anatolia. Dispersed pollen. Scanning electron microscopy. Botanical nomenclature. Artificial nomenclature This article is a contribution to the special issue "Taking the Orient Express? The role of Anatolia in mediterranean Neogene palaeobiogeography".

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Section: Subfamily Cichorioideae Chevall 1828mentioning

confidence: 73%

The middle Miocene palynofloras of the Salihpaşalar lignite mine (Yatağan Basin, southwest Anatolia): environmental characterisation and comparison with palynofloras from adjacent basins

Bouchal

2018

Palaeobio Palaeoenv

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“…Remarks : Morphologically similar pollen is found in Linnaeoideae (Chia‐Chi & Chao‐Xin, ; Maciejewska, ; Li et al ., ; Miyoshi et al ., ).…”

Section: Systematic Palynologymentioning

confidence: 66%

The middle Miocene palynoflora and palaeoenvironments of Eskihisar (Yatağan basin, south-western Anatolia): a combined LM and SEM investigation

et al. 2016

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We investigated a palynological section from middle Miocene sediments at Eskihisar (south‐western Anatolia) to establish biogeographic links of the palynoflora and to infer the palaeoenvironment. Four algal palynomorphs, nine spore taxa, eight gymnosperms, three monocots and 67 dicot pollen types were encountered and investigated using the ‘single grain method’ that combines light microscopy and scanning electron microscopy. Two pollen zones reflect different phases of basin development. Zonal vegetation remained fairly stable across the section and reflects heterogeneous environments including broad‐leaved deciduous forest, subtropical forest and sclerophyllous and semi‐evergreen oak forest. Conifers were accessory elements in the broad‐leaved deciduous forest communities and replaced these at higher elevations. Some herbaceous taxa (Plumbaginaceae) indicate scattered occurrences of sandy and/or rocky soils. Biogeographic affinities are general Northern Hemisphere, North American and East Asian, as also suggested by the macrofossil record. Only two taxa provide potential biogeographic links with the African flora. This suggests that biome shifts of plant taxa between African subtropical/tropical biomes and Anatolian (western Eurasian) temperate forests and shrublands may have been rare in the middle Miocene.

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“…[BACKLUND, DONOGHUE, 1996;BACKLUND, BREMER, 1997;DONOGHUE et al, 1992DONOGHUE et al, , 2001APG III, 2009] Для вирішення розглянутих вище спірних питань необхідне подальше вивчення морфологічних особливостей L. borealis, зокрема, важливо провести детальне дослідження будови генеративних органів рослин (у тому числі на мікроморфологічному рівні) і виявити ознаки, важливі для діагностики таксонів. У літературних джерелах представлені деякі відомості щодо морфологічних особливостей пилкових зерен, квітки, суцвіття та плодів L. borealis [BARBARYCH, 1961;KHOKHRIAKOV, MAZURENKO, 1968;MORRE, 1976;POIARKOVA, 1978;DONOGHUE, 1985;DONOGHUE et al, 2003;ZAITSEVA, 2006;YANG, LANDREIN, 2011;LANDREIN, PRENNER, 2016;KUPRIYANOVA, ALESHINA, 1972;ARTYUSHENKO, ROMANOVA, 1984;MACIEJEWSKA, 1997], проте вони потребують уточнення та більшої деталізації. Отже, метою роботи є уточнення особливості будови квітки, пилкових зерен і плодів на підставі критичного перегляду відомих морфологічних ознак генеративних органів Linnaea borealis, надання детальної характеристики та виявлення додаткових ознак для використання їх у вирішенні спірних питань таксономії.…”

Section: морфологічні особливості генеративних органівunclassified