Declining insect abundance and diversity in Germany 2008-2017

Insect abundance and diversity Germany 2008-2017 Nature — (a) Insect diversity (total number of species across all grassland or forest sites) (b), biomass, (c) abundance and (d) number of species (d) in 30 forest and 150 grassland sites across Germany

In this article insect abundance data collected from 150 grassland and 140 forest sites in 3 regions of Germany from 2008 to 2017 was analyzed. A total of about 2,700 species were identified. ), from standardized inventories taken between 2008 and 2017 at 150 grassland and 140 forest sites in 3 regions of Germany. Insect abundance, total biomass of insects, number of species and diversity were calculated for wach year. It was found that diversity in grasslands and forests decreased over time, indicating loss of species across sites and regions. In annually sampled grasslands, biomass, abundance and number of species declined by 67%, 78% and 34%, respectively. In 30 forest sites with annual inventories, biomass and number of species, but not abundance, decreased by 41% and 36%, respectively.

Seibold, S., Gossner, M.M., Simons, N.K. et al. Arthropod decline in grasslands and forests is associated with landscape-level drivers. Nature 574, 671–674 (2019) doi:10.1038/s41586-019-1684-3

From Our Files

Global deep ocean temperature 60 million years ago to present

New evidence that CO2 may have driven cooling 50-30 million years ago

New evidence from analyzing fossil plankton shells has revealed that CO2 concentration in the Earth’s atmosphere was about triple current levels around 52 million years ago. It then declined to levels close to current atmospheric CO2 concentration 34 million years ago when Antarctica began to glaciate.

Southern Ocean warming preceded rising CO2 during the last deglaciation

Marine cores collected in the western tropical Pacific were used to compare the chronology of Southern Ocean warming near Antarctica and rising CO2 during the last deglaciation. The results provide evidence that the Southern Ocean off Antarctica warmed by ~2°C between 19,000 and 17,000 years before the present, about 1,000 years before the rise in atmospheric CO2.

Temperature and atmospheric CO2 from Dome C for 800 000 years

Observed coupling between surface temperature and atmospheric CO2 extended to 1.5 million years ago

Evidence from Antarctic ice cores have revealed a close correlation between surface temperature and atmospheric carbon dioxide concentration for the past 800,000 years (excluding the immediate present.) A recent analysis of Antarctic blue ice has found that the close correlation between temperature CO2 extends to 1.5 million years ago during the time when the glacial/interglacial period was 40,000 years.

Southern Ocean outgassing initial source of rising CO2 during the last deglaciation

During the first pulse of increasing atmospheric CO2 at the beginning of the last deglaciation the carbon-13 ratio dropped precipitously indicating that a source of the CO2 was a large pool of carbon of organic origin. Comparison with other data including the atmospheric carbon-14 record point at outgassing from Southern Ocean deep water as the source of the CO2 increase in this early period of the deglaciation.