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Kohärenz gesetzlicher Rahmenbedingungen für eine sozial-ökologische Transformation des Naturschutzes

Als sozial-ökologische Transformation wird der Prozess bezeichnet, der unser Handeln und Wirtschaften wieder in die Bahnen der planetaren Belastungsgrenzen zurückführen will, ohne die sich dabei stellenden sozialen und wirtschaftlichen Fragen zu ignorieren. Ein wichtiges Handlungsfeld einer sozial-ökologischen Transformation sind der Naturschutz und die Erhaltung der Biodiversität. Längst ist klar, dass es dafür nicht nur eines leistungsfähigen Naturschutzfachrechts bedarf, sondern darüber hinaus der Integration des Biodiversitätsschutzanliegens in verschiedene Landnutzungssektoren, wie die Land- und Forstwirtschaft, das Siedlungswesen und die Wasserbewirtschaftung. Auch mit Blick auf den Klimaschutz ist mittlerweile anerkannt, dass er nicht nur Energie und Verkehr betrifft, sondern als sog. "natürlicher Klimaschutz" auch eine landnutzungsbezogene Dimension hat. Der Beitrag untersucht, inwieweit die geltenden rechtlichen Rahmenbedingungen den Weg für eine sozial-ökologische Transformation des Naturschutzes bereiten. Dabei werden insbesondere die im Juni 2024 beschlossene EU-Verordnung über die Wiederherstellung der Natur und die Rahmenbedingungen des natürlichen Klimaschutzes analysiert. Am Beispiel der Wiedervernässung landwirtschaftlich genutzter Moorböden wird danach gefragt, ob die bestehenden Rechts- und Politikinstrumente ausreichend darauf abgestimmt sind, komplexe Renaturierungsziele erreichen zu können.

Hydrochemistry at time series station Helgoland Roads, North Sea, in 2013

In 2013, the hydrochemistry of surface water was monitored at Helgoland Roads station on every workday, typically before 9 a.m. Temperature was measured on board immediately after sampling. Visibility was measured on board using a Secchi Disk. Salinity, dissolved inorganic nutrients, pH and oxygen were measured from a bucket sample in the laboratory.

Hydrochemistry at time series station Helgoland Roads, North Sea, in 2012

In 2012, the hydrochemistry of surface water was monitored at Helgoland Roads station on every workday, typically before 9 a.m. Temperature was measured on board immediately after sampling. Visibility was measured on board using a Secchi Disk. Salinity, dissolved inorganic nutrients, pH and oxygen were measured from a bucket sample in the laboratory.

Hydrochemistry at time series station Helgoland Roads, North Sea, in 2011

In 2011, the hydrochemistry of surface water was monitored at Helgoland Roads station on every workday, typically before 9 a.m. Temperature was measured on board immediately after sampling. Visibility was measured on board using a Secchi Disk. Salinity, dissolved inorganic nutrients, pH and oxygen were measured from a bucket sample in the laboratory.

Hydrochemistry at time series station Helgoland Roads, North Sea, in 2005

In 2005, the hydrochemistry of surface water was monitored at Helgoland Roads station on every workday, typically before 9 a.m. Temperature was measured on board immediately after sampling. Visibility was measured on board using a Secchi Disk. Salinity and dissolved inorganic nutrients were measured from a bucket sample in the laboratory.

Hydrochemistry at time series station Helgoland Roads, North Sea, in 2010

In 2010, the hydrochemistry of surface water was monitored at Helgoland Roads station on every workday, typically before 9 a.m. Temperature was measured on board immediately after sampling. Visibility was measured on board using a Secchi Disk. Salinity and dissolved inorganic nutrients were measured from a bucket sample in the laboratory.

Hydrochemistry at time series station Helgoland Roads, North Sea, in 2008

In 2008, the hydrochemistry of surface water was monitored at Helgoland Roads station on every workday, typically before 9 a.m. Temperature was measured on board immediately after sampling. Visibility was measured on board using a Secchi Disk. Salinity and dissolved inorganic nutrients were measured from a bucket sample in the laboratory.

Hydrochemistry at time series station Helgoland Roads, North Sea, in 2007

In 2007, the hydrochemistry of surface water was monitored at Helgoland Roads station on every workday, typically before 9 a.m. Temperature was measured on board immediately after sampling. Visibility was measured on board using a Secchi Disk. Salinity and dissolved inorganic nutrients were measured from a bucket sample in the laboratory.

Hydrochemistry at time series station Helgoland Roads, North Sea, in 2006

In 2006, the hydrochemistry of surface water was monitored at Helgoland Roads station on every workday, typically before 9 a.m. Temperature was measured on board immediately after sampling. Visibility was measured on board using a Secchi Disk. Salinity and dissolved inorganic nutrients were measured from a bucket sample in the laboratory.

Hydrochemistry at time series station Helgoland Roads, North Sea, in 2004

In 2004, the hydrochemistry of surface water was monitored at Helgoland Roads station on every workday, typically before 9 a.m. Temperature was measured on board immediately after sampling. Visibility was measured on board using a Secchi Disk. Salinity and dissolved inorganic nutrients were measured from a bucket sample in the laboratory.

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