Xianyu Huang
Biographic Data
| ID | 3637069 |
|---|---|
| NAME | Xianyu Huang |
| GIVEN NAMES | Xianyu |
| FAMILY NAME | Huang |
| SIGNATURE | HUANG X |
| AFFILIATIONS | China University of Geosciences |
| ORCID | 0000-0001-6175-9158 |
| VERIFIED | Yes |
| TOTAL WORKS | 5 |
| TOTAL CITATIONS | 3 |
| WORKS AS AUTHOR | 5 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2012 |
| LATEST PUBLICATION YEAR | 2024 |
| H-INDEX | 1 |
Divergent sensitivity of primary producers and benthic invertebrates to hydrological alteration in floodplain lakes
Effects of climate change on a subtropical montane peatland over the last two centuries
Climate variability can induce rapid changes in peatland ecosystems, affecting both carbon cycling and vegetation succession. Diatoms are an important group of ubiquitous and diverse algae in peatlands. Until now, the responses of diatom communities to climate variability have rarely been explored in peatlands, especially in subtropical regions. In this study, monitoring and paleolimnological datasets were combined to decipher environmental chang…
Paleohydrological changes over the last 4000 years in the middle and lower reaches of the Yangtze River
We have reconstructed the history of late-Holocene paleohydrological changes in the middle and lower reaches of the Yangtze River using grain size and n-alkane data from a sediment core retrieved from Longgan Lake. We employ changes in the grain size distribution to reflect the water level in the floodplain lake, with a higher percentage of the finer fraction indicating higher water level and vice versa. The n-alkane molecular distribution, avera…
Paleotemperature variability in central China during the last 13 ka recorded by a novel microbial lipid proxy in the Dajiuhu peat deposit
The Asian summer monsoon is a very important climatic component affecting the land ecosystem on the eastern Asian continent. Here we assess microbe-derived lipid biomarker evidence from a well-dated peat core from Dajiuhu to reconstruct paleotemperature changes in central China through the last 13 ka. The branched fatty alcohol ratio BNA 15 , which is defined as the relative contribution of branched C15 fatty alcohols over their straight-chain ho…
Moisture conditions during the Younger Dryas and the early Holocene in the middle reaches of the Yangtze River, central China
The last glacial–interglacial climate transition in East Asia was characterized by an intensified monsoon, but knowledge about hydrological responses at a regional scale during this transitional period is limited. Here we provide a novel lipid-based paleohydrological record for this period from the Dajiuhu peat deposit, central China. High water levels and persistent wet conditions during the Younger Dryas (12.5–11.6 ka) and the early Holocene (1…
Paleotemperature variability in central China during the last 13 ka recorded by a novel microbial lipid proxy in the Dajiuhu peat deposit
The Asian summer monsoon is a very important climatic component affecting the land ecosystem on the eastern Asian continent. Here we assess microbe-derived lipid biomarker evidence from a well-dated peat core from Dajiuhu to reconstruct paleotemperature changes in central China through the last 13 ka. The branched fatty alcohol ratio BNA 15 , which is defined as the relative contribution of branched C15 fatty alcohols over their straight-chain ho…
Moisture conditions during the Younger Dryas and the early Holocene in the middle reaches of the Yangtze River, central China
The last glacial–interglacial climate transition in East Asia was characterized by an intensified monsoon, but knowledge about hydrological responses at a regional scale during this transitional period is limited. Here we provide a novel lipid-based paleohydrological record for this period from the Dajiuhu peat deposit, central China. High water levels and persistent wet conditions during the Younger Dryas (12.5–11.6 ka) and the early Holocene (1…
Paleotemperature variability in central China during the last 13 ka recorded by a novel microbial lipid proxy in the Dajiuhu peat deposit
The Asian summer monsoon is a very important climatic component affecting the land ecosystem on the eastern Asian continent. Here we assess microbe-derived lipid biomarker evidence from a well-dated peat core from Dajiuhu to reconstruct paleotemperature changes in central China through the last 13 ka. The branched fatty alcohol ratio BNA 15 , which is defined as the relative contribution of branched C15 fatty alcohols over their straight-chain ho…
Paleohydrological changes over the last 4000 years in the middle and lower reaches of the Yangtze River
We have reconstructed the history of late-Holocene paleohydrological changes in the middle and lower reaches of the Yangtze River using grain size and n-alkane data from a sediment core retrieved from Longgan Lake. We employ changes in the grain size distribution to reflect the water level in the floodplain lake, with a higher percentage of the finer fraction indicating higher water level and vice versa. The n-alkane molecular distribution, avera…
Effects of climate change on a subtropical montane peatland over the last two centuries
Climate variability can induce rapid changes in peatland ecosystems, affecting both carbon cycling and vegetation succession. Diatoms are an important group of ubiquitous and diverse algae in peatlands. Until now, the responses of diatom communities to climate variability have rarely been explored in peatlands, especially in subtropical regions. In this study, monitoring and paleolimnological datasets were combined to decipher environmental chang…
Divergent sensitivity of primary producers and benthic invertebrates to hydrological alteration in floodplain lakes
Climate change (4 works) · Environmental Science (4 works) · Geology (4 works) · Geology and Paleoclimatology Research (4 works) · Oceanography (4 works) · Physical geography (4 works) · Biology (3 works) · Climatology (3 works) · Ecology (3 works) · Geography (3 works)