Abstract The continued investigation of the middle Miocene palynoflora from the Lavanttal Basin reveals numerous additional angiosperm taxa. The Myrtales to Ericales pollen record documented here comprises 46 different taxa belonging to Onagraceae (Ludwigia), Ericaceae (Craigia, Reevesia, Tilia), Anacardiaceae (Pistacia), Rutaceae (Zanthoxylum), Sapindaceae (Acer), Santalaceae (Arceuthobium), Amaranthaceae, Caryophyllaceae, Polygonaceae (Persicaria, Rumex), Cornaceae (Alangium, Cornus, Nyssa), Ebenaceae (Diospyros), Ericaceae (Andromeda, Arbutus, Empetrum, Erica), Sapotaceae (Pouteria, Sideroxylon), Styracaceae (Rehderodendron) and Symplocaceae (Symplocos). Köppen signatures of potential modern analogues of the additional fossil woody elements confirm the hypothesis of a subtropical (Cfa, Cwa) climate at lower elevations and subsequent transition into a temperate climate with altitudinal succession (Cfa → Cfb/Dfa → Dfb; Cwa → Cwb → Dwb-climate). The fossil plants represent different vegetation units, from wetland lowlands to well-drained montane forests. Many of the fossil taxa have potential modern analogues that can be classified as nemoral and/or meridio-nemoral and/or semihumid-meridional vegetation elements. New is the recognition of oreotropical elements, which are direct indicators for a substantial altitudinal gradient.

中文翻译：

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奥地利拉万塔尔盆地中期中新世（萨尔马提亚）孢粉植物群的 LM 和 SEM 联合研究：第五部分：木兰植物 3 – 桃金娘目到杜鹃花目

摘要 对拉万塔尔盆地中新世中期孢粉植物群的持续研究揭示了许多额外的被子植物类群。这里记录的桃金娘目到杜鹃花目花粉记录包括 46 个不同的分类群，分别属于 Onagraceae (Ludwigia)、Ericaceae (Craigia、Reevesia、Tilia)、Anacardiaceae (Pistacia)、Rutaceae (Zanthoxylum)、Sapindaceae (Acer)、Santalacaceae (Arceuthobium)、Amaranthaceae、石竹科、蓼科（Persicaria、Rumex）、山茱萸科（Alangium、Cornus、Nyssa）、山茱萸科（Diospyros）、杜鹃花科（仙女座、杨梅、Empetrum、Erica）、山楂科（Pouteria、Sideroxylon）、丁香科（Rehderodendron）和山矾科（Symplocos） 。其他化石木本元素的潜在现代类似物的柯本特征证实了低海拔亚热带（Cfa，Cwa）气候以及随后随着海拔演替过渡到温带气候的假设（Cfa → Cfb/Dfa → Dfb；Cwa → Cwb → DWB-气候）。这些植物化石代表了不同的植被单元，从湿地低地到排水良好的山地森林。许多化石类群具有潜在的现代类似物，可以归类为向阳和/或子午-向阳和/或半湿润-子午植被元素。新的是对逆向性元素的识别，它们是显着海拔梯度的直接指标。