-
Global assessment of arbuscular mycorrhizal fungus diversity reveals very low...
The global biogeography of microorganisms remains largely unknown in contrast to the well-studied diversity patterns of macroorganisms. We used arbuscular mycorrhizal (AM)... -
Summary pollen percentages for Marine Isotope Stages (MIS) 42-43 at IODP Site...
This dataset has no description
-
Summary pollen percentages for Marine Isotope Stages (MIS) 34-35 at IODP Sit...
This dataset has no description
-
Pollen records of sediment core HL4 (Hoher List infilled maar), Eifel, Germany
Pollen were analyzed in a total of 560 lake sediment samples from four Eifel maars (lake Holzmaar, Jungferweiher infilled maar, Dehner infilled maar, Hoher List infilled maar).... -
Pollen records of sediment core DE2 (Dehner infilled maar), Eifel, Germany
Pollen were analyzed in a total of 560 lake sediment samples from four Eifel maars (lake Holzmaar, Jungferweiher infilled maar, Dehner infilled maar, Hoher List infilled maar).... -
Pollen records of sediment core JW3 (Jungferweiher infilled maar), Eifel, Ger...
Pollen were analyzed in a total of 560 lake sediment samples from four Eifel maars (lake Holzmaar, Jungferweiher infilled maar, Dehner infilled maar, Hoher List infilled maar).... -
Pollen records of sediment core HM4 from lake Holzmaar, Eifel, Germany
Pollen were analyzed in a total of 560 lake sediment samples from four Eifel maars (lake Holzmaar, Jungferweiher infilled maar, Dehner infilled maar, Hoher List infilled maar).... -
A combination of 11 ELSA-pollen cores from six Eifel maars, Germany
Pollen were analyzed in a total of 560 lake sediment samples from four Eifel maars (lake Holzmaar, Jungferweiher infilled maar, Dehner infilled maar, Hoher List infilled maar).... -
Percentages of pollen data from late MIS 6 to MIS 1 from Füramoos, Southern G...
High-resolution palynological data (taxa and groups) from the Füramoos peat bog. The data span from the latest Rissian glaciation (MIS 6) to the present (MIS 1) at an average... -
Zunehmende Trockenphasen und Waldbrände an der südlichen Taigagrenze und in d...
Die borealen Wälder Sibiriens werden generell nach Süden hin zu den zentralasiatischen Trockengebieten durch die Abnahme der Niederschläge begrenzt. Im...