59. The peat profile of Rue des Boîteux–Rue d’Argent (BR295), Senne valley, Brussels (Belgium)

IF 0.9 4区 生物学 Q4 PLANT SCIENCES Grana Pub Date : 2022-05-04 DOI:10.1080/00173134.2022.2048886
Elena Marinova, Yannick Devos, L. Speleers, Sylvianne Modrie
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Abstract

The site of Rue des Boîteux–Rue d’Argent (BR295) (coordinates 50° 51’ N; 4° 21’ E, 17 m above sea level [a.s.l.]) is situated in the actual town centre of Brussels, at the foot of a steep slope leading from the alluvial plain of the Senne River to the Brabantian plateau.Mean annual temperature in Brussels is 10.4 °C. Mean temperature is 3.2 °C for January and 18.4 °C for July. Mean precipitation reaches 848 mm (KMI s.d.). The actual soil moisture regime of the region is Udic (soil moisture is sufficient throughout the year to meet plant requirements [USDA 1999: 97]). The soil temperature regime is Mesic. This implies that the mean annual soil temperature is 8 °C or higher and lower than 15 °C, and the difference between mean summer and mean winter soil temperatures is more than 6 °C (USDA 1999: 112). During a rescue excavation in 2014, a thick peat deposit was discovered. The top of the peat was affected by human activity and gradually transformed into an urban Dark Earth. Locally, modern construction works truncated the peat deposit. The peat deposit with total thickness of c. 2 m was sampled at three profiles by overlapping monolith blocks. The blocks were correlated stratigraphically based on their lithology (Table I) and the chronology was subsequently confirmed with absolute dates (Table II) so that a composite profile was obtained. Samples for pollen analysis (with volume 3 cm2) were taken at each 2.5 cm. Dating
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59. 比利时布鲁塞尔塞纳河谷,borue - teux - Rue d 'Argent (BR295)泥炭剖面
Bo街-阿金特街(BR295)(坐标:北纬50°51';东经4°21',海拔17m)位于布鲁塞尔市中心,位于从塞纳河冲积平原通往布拉班蒂高原的陡坡脚下。布鲁塞尔的年平均气温为10.4°C。一月平均气温为3.2°C,七月平均气温为18.4°C。平均降水量达到848毫米(KMI s.d.)。该地区的实际土壤水分状况为Udic(全年土壤水分足以满足植物需求【美国农业部1999:97】)。土壤温度状况为Mesic。这意味着年平均土壤温度为8°C或更高且低于15°C,夏季和冬季平均土壤温度之间的差异超过6°C(美国农业部1999:112)。在2014年的一次救援挖掘中,发现了一个厚厚的泥炭矿床。泥炭的顶部受到人类活动的影响,逐渐转变为城市的黑暗地球。在当地,现代建筑工程截断了泥炭矿床。总厚度约为2m的泥炭矿床通过重叠的单片块体在三个剖面上取样。根据岩性对区块进行了地层对比(表I),随后用绝对日期确认了年代(表II),从而获得了复合剖面。花粉分析样品(体积3cm2)每2.5厘米取样一次
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来源期刊
Grana
Grana 生物-植物科学
CiteScore
2.10
自引率
11.10%
发文量
23
审稿时长
>12 weeks
期刊介绍: Grana is an international journal of palynology and aerobiology. It is published under the auspices of the Scandinavian Palynological Collegium (CPS) in affiliation with the International Association for Aerobiology (IAA). Grana publishes original papers, mainly on ontogony (morphology, and ultrastructure of pollen grains and spores of Eucaryota and their importance for plant taxonomy, ecology, phytogeography, paleobotany, etc.) and aerobiology. All submitted manuscripts are subject to initial appraisal by the Editors, and, if found suitable for further consideration, to peer review by independent, anonymous expert referees. All peer review is single blind and submission is online via ScholarOne Manuscripts.
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